■i*^^';'*rf'''?.;:' Cornell University Library The original of this book is in the Cornell University Library. There are no known copyright restrictions in the United States on the use of the text. http://www.archive.org/details/cu31924054701614 3 1924 054 701 614 THE THEORY AND PEACTICE OF HORTICULTUEE ; OR, AN ATTEMPT TO EXPLAIN THE CHIEF OPEEATIONS OF GARDENING UPON PHYSIOLOGICAL GEOUNDS. BEINQ THE SECOND EDITION OF THE THEOEY OF HOETICIJLTUEE, MUCH ENLARGED. By JOHN LINDLEY, Ph.D. F.R.S. Correspondingr Member of the Institute, Vice-Secretary of the Horticultural Society, Professor of Botany in University College, Ltjndon, &c. &c. &c. " Thougli I am very sensible tliat it is from long experience chiefly that we are to expect the m.ost certain rules of practice, yet it is withal to he remembered that the likeliest method to enable us to make the most judicious observations, and to put us upon the most probable means of improving any art, is to get the best insight we can into the nature and properties of those things which we are desirous to cultivate and improve." Hales's Vegetable Staiicks, I 376. LONDON: LONGMAN, BROWN, GREEN, AND LONGMANS. 1855. LONDON : BRADBtTRY AND EVANS, PR1NTEE3, WI-TITEFIITA"BS, EIGHT HONOTJEABLE THOMAS FEANCIS KENNEDY, Lately one of Her Majesty's Commissioners of Woods, Forests, and Land Revenues, B!S{)0 ffinSeafaanteU to i&datm A PUBLIC DEPAETMEMT IN WHICH UNSKILFUL MANAGEMENT HAS BEEN MOST DI3ASTB0UB, THIS EDITION OS A WORK ON THE PEINCIPLES 0! CULTIVATION, JEs Eiwcvibetf AS A MARK OF RESPECT FOR HIGH OFFICIAL CHARACTER AND ILL-REQUITED PUBLIC SERVICES, BT HIS FAITHFUL SBBVANT, THE AUTHOR. PREFACE TO THE FIRST EDITION. (1840.) This book is written in the hope of providing the intelligent gardener, and the scientific amateur, correctly, with' the rationalia of the more important operations of Horticulture ; in the full persuasion that, if the physiological principles on which such operations, of necessity, depend, were correctly appreciated by the great mass of active-minded persons now engaged in gardening in this country, the grounds of their practice would be settled upon a more satisfactory foundation than can at present be said to exist. It is, I confess, sur- prising to me, that the real nature of the vital actions of plants, and of the external forces by which they are regulated, should be so frequently misapprehended even among writers upon Horticulture ; and that ideas relating to such matters, so very incorrect as we frequently find them to be, should obtain among intelligent men, in the present state of what I may be permitted to call horticultural physiology. There must be a great want of sound knowledge of this subject, when we find an author, who has made himself distinguished in the history df English gardening, giving it as his opinion, " that the weali drawn state of forced Asparagus in London is occasioned by the action of the dung immediately upon its roots ! " It does not seem possible to account for this in any other way than by referring it to the want of some short guide to the horticultural application of vegetable physiology, unmixed with vi PREFACE TO THE FIRST EDITION. other things ; and so arranged that the intimate connexion of one branch of practice with another, and of the whole with a few well ascertained facts upon which everything else depends, may be distinctly perceived from a single point of view. The admirable papers of Mr. Knight are scattered through the Horticultwal Transactions ; and the writings of other physi- ologists are dispersed through so many different works, that the labour of finding them, when wanted, is greater than is willingly undertaken even by those who have access to ample libraries. With regard to general works on Horticulture, it is very far from my wish to say one word in disparagement of the many excellent publications upon this subject which have already appeared in this country 5 on the contrary, the improved state of gardening among us may be reasonably ascribed to the influence of some of these valuable works : but it must be admitted that the true principles of physiology are not, in such books, so separated from the details of routine on the one hand, or so applied to them on the other, as to be readily understood by those who want either the skill or the inclination to distiuguish empirical directions from rules which are plainly founded upon the very nature of things. I must also be permitted to observe that, although results are correctly stated in such books, they are not unfrequently referred to wrong causes. In preparing the following pages for the press, my anxious desire has been to strike out all unnecessary matter, even although it may be required to complete the physiological explanation of common facts ; and to introduce little beyond that which every gardener can verify for himself. Vegetable anatomy is no doubt the foundation of all correct views of physiological action ; chemistry is of the first importance, when the general functions of plants are considered in a large and general way ; and electricity probably exercises an important PfiEFACE TO THE FIRST EDITION. vii influence over the vital actions of all living things. But these are the refinements of science, belonging to the philosopher in his laboratory, and not to the worker in gardens; they are indispensable to the correct appreciation of physiological phenomena, but not to the application of those phenomena to the arts of life ; electricity, in particular, appears to me, in the present imperfect state of our knowledge of its relation to vegetable functions, altogether incapable of forming a part of any horticultural theory. What the gardener wants is, not a treatise upon botany, nor a series of speculations upon the possible nature of the influence on plants of all existing forces, nor an elaborate account of chemical agencies inappreciable by his senses and obscurely indicated by their visible results ; but an intelligible explanation, founded upon well ascertained facts which he can judge of by his own means of observation, of the general nature of vegetable actions, and of the causes which, while they control the powers of life in plants, are themselves capable of being regulated by himself. The possession of such knowledge will necessarily teach him how to improve his methods of cultiva- tion, and lead him to the discovery of new and better modes. It is very true that ends of this kind are often brought about by accident, without the smallest design on the part of the gardener ; and there are, doubtless, many men of uncultivated or idle minds, who think waiting upon Providence much better than any attempt to improve their condition by the exertion of their reasoning faculties. For such persons books are not written. I hope that what has now been said will not lead any one to suppose that this sketch is offered to the reader as a complete theory of Horticulture in all its varied branches ; such a work would be alike tedious to the author and the reader, and, I fear, as unprofitable ; for, if a gardener, when once made acquainted viii PREFACE TO THE FIRST EDITION. with the general principles of science, has not the skill to apply them to each particular case, it is to be feared that no disquisi- tion, however elaborate, would enable him to do so. So far has it been from my intention to enter into subordinate details, that I have carefully avoided them, from a fear of complicating the subject, and making that obscure which in itself is suffici- ently clear. All that a physiologist has reaUy to do with Horticulture is, to explain the general nature of the Yital actions of a plant, and the manner in which these are commonly applied to the arts of cultivation ; if he quits this ground, he extends his limits so much that there is no longer a horizon in view. No one, indeed, could advantageously investigate the minor points of cultivation in aU their branches, unless he were both a good physiologist and a practical gardener of the greatest experience, a combination of qualifications which no man has ever yet possessed, and to which I, most assuredly, have not the shadow of pretension. In conclusion, let me, in impressing upon the minds of gar- deners the importance of attending to first principles, also caution them against attempting to apply them, except in a limited manner, and by way of safe experiment, until they fully understand them. The difference between failure and success, in practice, usually depends upon slight circumstances, very easily overlooked, and not to be anticipated beforehand, even by the most skilful ; their importance is often unsuspected till an experiment has failed, and may not be discovered tUl after many unsuccessful attempts, during which more mischief may be done by extensive failures than the result is worth when attained. No man understood this better than the late Mr. Knight, the best horticultural physiologist that the world has seen, whose experiments were conducted with a skiU and knowledge which few can' hope to equal. So fuUy was he aware of the uncertain issue of experimental investigations in Horti- PREFACE TO THE FIRST EDITION. ix culture, that he thought it necessary, in recommending a new mode. of ctiltivating the Pine-apple, and in ohjecting to methods at that time commonly in use, to express himseK in the fol- lowing words : — ■" I beg it to be understood that I condemn the machinery only which our gardeners employ, and that I admit most fully their skill in the application of that machinery to be very superior to that which I myself possess. Nor do I mean, in the slightest degree, to censure them for not having invented better machinery, for it is their duty to put in practice that which they have learned ; and, having to expend the capital of others, they ought to be cautious in trying expensive experiments, of which the results must necessarily be uncertain; and, I believe, a very able and experienced gardener, after having been the inventor of the most perfect machinery, might, in very many instances, have lost both his character and his place before he had made himself sufficiently acquainted with it, and consequently become able to regulate its powers." PREFACE TO THE SECOND EDITION. Aftee a lapse of fifteen years the author has been called upon to prepare for the press a Second Edition of this work. In obeying the call, he gladly avails himself of the only public opportunity that he can have for thanking his foreign editors for the honour they have done him by translating the book into German,* Dutch,t and Eussian.I , He has always felt that the naked principles laid down in the First Edition were less interesting than they would have been if they had received more extensive illustration from examples and frequent reference to practical operations. He has now, therefore, greatly extended the matter, and endeavoured, when- ever it appeared necessary, to support the doctrines of physiology by an appeal to facts which are or should be familiar to culti- vators. In doing this he has to express his sincere gratitude to the numerous intelligent contributors to the Gardeners' Chronicle, who during more than fourteen years have honoured * Theorie der Gartenkunde, &c., uebersetzt mit Anmerkungen von Ludolpli Christiau Treviranus. Erlangen, 1843. Theorie der Gartnerei, &o., aus dem Englisohen iitersetzt von S. G., mit eiaer Vorrede, Amnerkungen, und einem Anhange, versehen von einigen Freimden der Horti- cultur. Wien, 1842. + Gfrondbegiuselen der Horticnltniir (Tuinkunst) naar het Engelsch van John Lindley, &c. ; mit hijlagen door W. H. de Vriese. Amsterdam, 1842. J Teoria Sadovodstva Hi opoit izjasnenia glaTneiahich proizvodstv sadovodstva iz natshal rastitelnoi phisiologii. Edited, with Tarious notes and additions, by J. Sohyehowsky. St. Petersburg, 1845. xii PREFACE TO THE SECOND EDITION. him with their confidence, for avast accumulation of horticultural information upon almost every point that can engage the thoughts of a gardener ; it is they who have put principles to the test of experience, and who have shown how little there is of doubtful or unsound in the Theory of gardening ; and he thinks it due to them to acknowledge that whatever new merit this book may possess is owing greatly to the experience gained by their friendly cooperation. AOTON ©KEEN, April, 1855. ERRATUM. Page 101, for Baroness RoUe read Baroness RoUe. CONTENTS. BOOK I. OP THE PRINCIPAL CIRCUMSTANCES CONNECTED WITH VEGETABLE LIFE WHICH ILLUSTRATE THE OPERATIONS OF GARbENING . . 5 CHAPTER I. Vital Force .... . . CHAPTER II. GEEMINATION. The Nature of a Seed. — Its Duration. — Power of Growth. — Causes of Ger- mination. — Temperature. — Light. — Humidity. — Chemical Changes . 13 CHAPTER III. ftEOWTH BT THE KOOI. Boots lengthen at their Points only. — Absorb at that Part chiefly. — Increase in Diameter lite Stems. — Their Origin. — Are feeding Organs— without much Power of selecting their Pood. Nature of the 'latter. — May be poisoned. — Are constantly in Action. — Have been thought to poison the Soil in which they grow. — Have no Buds — but may generate them . 17 CHAPTER IV. GEOWTH BY THE STEM. Origin of the Stem. — The Growing Point. — Production of Wood, Bark, Pith, Medullary Eays. — Properties of Sap-wood, Heart-wood, Liber, Rind, &c. Nature and Office of Leaf-buds. — Embryo-buds. — Bulbs. — Conveyance of Sap, and its Nature 33 xiv CONTENTS. PAGE CHAPTER V. ACTION OF lEATES. Their Nature, Structure, Veiiis, Epidermis, Stomatea. — Effect of Light. — Digestion or decompositiou of Carbonic Acid. — Insensible Perspiration. Formation of Secretions. — ^Fall of the Lea£ — Formation of Buds by Leaves 54 CHAPTER VI. ACTION OF PIOWEES. Structure of Flowers. — Names of their Parts. — Tendency of the Parts to alter and change into each other, and into Leaves. — Double Flowers.^ Analogy of Flowers to Branches. — Cause of the Production of Flowers. Of Productiveness. — Of Sterility. — Uses of the Parts of a Flower. — Fertilisation. — Hybrids.— Crossbreds ....... 81 CHAPTER VII. OF THE MATTTEATION OF THE FETJIT. Changes it undergoes. — Is fed by Branches upon Organisable Matter fur- nished by Leaves. — ^Physiological use of the Fruit. — Nature of Secre- tions. — The changes they undergo. — Effect of Heat — of Sunlight — of Water. — Seeds. — Source of their Food. — Cause of their Longevity — of their Destruction. — ^Difference in their Vigour 97 CHAPTER VIII, OF TEMPBEATUEE. Limits of Temperature endurable by Plants. — Effects of a too high Tempe- rature — of a too low Temperature. — Frost. — Alternations of Tempera- ture. — Day and Night. — ^Winter and Summer. — Temperature of Earth and Atmosphere 106 BOOK II. OP THE PHYSIOLOGICAL PRINCIPLES UPON WHICH THE OPERATIONS OF HORTICULTURE ESSENTIALLY DEPEND I33 CHAPTER I. Of Bottom Heat • j3^ CHAPTER II. Of the Moisture of the Soil. — Watering jgg CONTENTS. XT CHAPTER III. -'""' Of Atmoepherical Moisture and Temperature I77 CHAPTER IV. Of Ventilation „■.„ CHAPTER V. Of Seed-sowing 227 CHAPTER VI. Of Seed-saving 039 CHAPTER VII. Of Seed-packing and Plant-packing 245 CHAPTER VIII. Of Propagation by Eyes and Knaurs 263 CHAPTER IX. Of Propagation by mere Leaves 271 CHAPTER X. Of Propagation by Cuttings 281 CHAPTER XI. Of Propagation by Layers and Suckers 301 CHAPTER XII, Of Propagation by Budding and Grafting 303 CHAPTER XIII. On Pruning . . 361 CHAPTER XIV. Of Training 421 xTi CONTENTS. PAGE CHAPTER XV. OfPotting ... *^^ CHAPTER XVI. 445 Of Transplanting . • • CHAPTER XVII. Of the Preservation of Races by Seed . . ... • 463 CHAPTER XVIII. Of the Improvement of Races ^°^ CHAPTER XIX. Of Resting ... 507 CHAPTER XX. Of Soil 525 CHAPTER XXI. Of Manure ... 539 Index 581 THE THEORY AND PRACTICE OF HORTICULTURE. HoETicuLTURB is that branch of knowledge which relates to the cultivation, multiplication, and amelioration of the Vege- table Kingdom. It divides into two branches, which, although mutually dependent, are, in fact, essentially distinct : the art and the science. Under the art of horticulture is compre- hended whatever concerns the mere manner of executing the operations connected with cultivation, multiplication, and amelioration ; the science explains the reasons upon which practice is founded. It is to the consideration of the latter subject that the following 'pages are dedicated. It must have been remarked by aU intelligent observers, that in the majority of works upon horticultural subjects, the numerous directions given in any particular ramification into which the art is susceptible of being divided, are held together by no bond of union, and that there is no explanation of their connection with general principles, by which alone the sound- ness of this or that rule of practice may be tested ; the reader is therefore usually obliged to take the excellence of one mode of cultivation, and the badness of another, upon the good faith of gardening authors, without being put into possession of any laws by which they may be judged of beforehand. Horticulture is by these means rendered a complicated subject such as none but practised gardeners can hope to pursue successfully ; and, like all empirical things, it is degraded into a code of peremptory precepts. It will nevertheless be found, if the subject is carefully investigated, that in reality the explanations of horticultural operations are simple, and free from obscurity ; provided they are not encumbered with speculations, which, however inter- esting in theory, are only perplexing in practice in the present state of our knowledge. When, for example, refined chemical disquisitions or minute anatomical details, or references to electrical action, are introduced, a plain subject becomes embarrassed with considerations too learned for the majority of readers of gardening works, and having Kttle obvious applica- tion to practical purposes. Instead, therefore, of introducing points of obscure or doubtful application, or such as are merely speculative and which only tend to complicate the theory of horticulture, it seems better strictly to confine attention to the action of the simplest vital forces ; for the general nature of these has been undoubtedly ascertained, and is easily under- stood by every class of readers. It is certain, for instance, that plants breathe, digest, and perspire ; but it may be a question whether the exact nature of their respiration, digestion, and perspiration is beyond all further explanation ; it is there- fore better to limit our consideration to the naked fact, which is all that it imports the gardener to know, without inquiring too curiously into those phenomena. For it must always be remembered that the object of a work like the present is not to elucidate the laws of vegetable life in all their obscure details, but to teach, to those acquainted with the art of gardening, what the great principles are upon wliich their practice is founded. In order to attain this end it is necessary, in the first place, to explain, however briefly, the nature of those vital actions which have a direct reference to cultivation ; and further to show how those facts bear upon the routine of practice of the horticulturist, by making them explain the reason of the practical methods employed in various branches of the gardener's art. The first part of this work therefore embraces the principal laws and facts in vegetable physiology, as deduced from the investigations of the botanist ; and the second an apphcation of those laws to practices established by the experience of the horticulturist. If the laws comprehended in the first book are correctly explained, and the facts connected with them rightly interpreted, they must necessarily afford, in all cases, the reasons why one kind of cultivation is better than another; and all kinds of practice at variance with those laws must be bad. Seeing that, from the very nature of things, this cannot be otherwise, it follows that, by a careful consideration and due understanding of such laws, the intelligent cultivator will acquire the most certain means of improving his practice. B 2 BOOK I. OF THE PRINCIPAL CIRCUMSTANCES CONNECTED WITH VEGETABLE LIFE WHICH ILLUSTRATE THE OPERATIONS OF GARDENING. A PLANT is a living body composed of an irritable, elastic, hygrometrical matter, called tissue. It is fixed to the earth by roots, and it elevates into the air a stem bearing leaves, flowers, and fruit. It has no power of shifting its place except when it is acted upon by wind or other external forces ; it is therefore peculiarly susceptible of injury or benefit from the accidental circumstances that may surround it ; and, having no free agency, it is above aU other created beings suited to acknow- ledge the power of man. In order to turn this power to account, it is necessary to study the manner of life which is peculiar to the vegetable kingdom, and to ascertain what the laws are by which the numerous actions essential to the existence of a plant are regulated. It is, moreover, requisite that the causes which modify those actions, either by increasrug or diminishing their force, should be understood. The vital actions of plants have so little apparent resem- blance to those of animals, that we are unable to appreciate their nature in even the smallest degree by a reference to our own sensations, or to any knowledge we may possess of animal functions. Nevertheless, when we carefully reflect upon the phenomena of vegetation, we discover certain unquestionable analogies of a general nature, between the animal and vegetable kingdoms. And although it is necessary that plants should be studied by themselves, as an abstract branch of investigation, without attempting to reason as to their habits from what we know of other organised beings ; still it must never be forgotten that they are living things, possessed, like animals, of vitality, that mysterious force which modifies all chemical and mechanical phenomena, and which so essentially distinguishes the organic world from the brute materials of which it is composed. In discussing this subject, it will be most convenient to divide the matter into the heads of, 1. Vital force; 3. Ger- mination; 3. Growth by the Boot; 4. Growth by the Stem; 5. Action of the Leaves ; 6. Action of the Flowers ; and, 7. Maturation of the Fruit. By this means the life of a plant is traced through all its principal changes, and an opporttmity is afforded of introducing under one or other of these heads every point of information that can be interesting to the cultivator ; who will be most likely to seek it in connection with those phenomena he is best acquainted with by their effects. CHAPTER I. VITAL FORCE. Me. Andeew Knight asserted that, in the course of his numerous experiments, he had never been able to trace the existence of anything like sensation or intellect in plants, but that they always appeared to be influenced by the action of surrounding bodies, and not by any degrees of sensation and passion analogous to those of animal Hfe. This seems to have led to the belief that they do not even possess a vital principle, but are mere chemical laboratories. One writer ventures to call a plant a porous system — endowed with no mtality other than the power of forming Cytohlasts," and arranging cellules after a definite type {Gardner in Phil. Mag. xxviii. 432). Even here it is admitted that some vitality exists ; for the arrangement of cells, or in other words the construction of plants, each after its kind, out of cells, implies vitality of a high order, although the writer seems to have meant that a plant is little more than a hag of quaternary compounds, and to have overlooked the fact that a plant when dead is a porous system as much as when alive. Nee dens intersit is however a favourite maxim with a certain class of modern writers, although nee absit would appear to be more consistent with all we know of the living world. But many discoveries have been made since the days of Knight, and a body of facts, showing the existence of high vitality, if not sensation, among plants, has been collected, with which he was wholly unacquainted. So that it is not too much to say, that the vegetable kingdom is now known to stand at least as high in the scale of life as the inferior orders of the animal kingdom. * A Cytoblast is the vital centre round which the cell and all its contents is even- tually formed. 8 PROOFS OF VITAL FORCE. This is shown, a, by the influence exercised over plants by substances such as laudanum and arsenic ; h, by the active and visible motions of the fluid contained within their cells ; c, by the unerring directions taken by the delicate apparatus which ensures reproduction by seed ; and d, by the locomotive power possessed by the reproductive apparatus of the lower classes of plants. M. It was long ago shown by Marcet, that if the common Kidney Bean, the Lilac, and other plants, were exposed to the action of such poisons as destroy animal life, they will perish not only under their influence, but in a manner analogous to what occurs among animals. If an animal is dosed with arsenic, or corrosive sublimate, or any poisonous metallic salt, it perishes by inflammation or corrosion : plants die in a similar way, their leaves turning yeUow and withering, no art sufficing for their recovery. On the other hand, vegetable poisons destroy life by a species of paralysis, leaves bending, and becoming flaccid, and the whole plant rapidly falling into a state resembling stupefaction, and ending in death. Every one knows that if the inner face of the stamens of the common Berberry is touched they suddenly rise upwards and dash their anthers against the stigma ; that after a time they fall back, and then become able again to present the same phenomenon. Macaire showed that when a twig of the Berberry in flower is placed in weak Prussio acid, or a solution of opium, the stamens lose their irritability, and become so flexible that they may be moved backwards and forwards without difficulty. When, however, the Berberry is placed in solutions of arsenic or corrosive sublimate, the stamens equally lose their excitability, but instead of becoming flexible, they are made stiflF, hard, and brittle. Similar efieots are produced upon the Sensitive Plant and other species. Here we have direct proof that the life of a plant is affected by destructive agents in the same manner as animals. The curious effect of ansesthetic substances is the same upon plants as on animals. Dr. Marcet has shown this by means of Chloroform. "If," he says, "a drop or two of pure chloroform be placed on the point of the common petiole of a leaf of the Sensitive Plant, the petiole is soon seen to droop, and directly afterwards the leaflets collapse in succession, pair by pair, beginning with those that are situate at the extremity of each branch. A minute or two afterwards (the time vary- ing with the irritability of the plant), most of the leaves near that on which the chloroform was placed, and situate below it on the same stem,, droop one after the other, and their leaflets collapse, althoun-h not in so decided a manner as those of the leaf to which the chloroform was applied. After a certain time, which vaaies with the condition of VITAL FORCE IN SENSITIVE PLANTS— IN CHARA. 9 the plant, the leaves gradually open ; but when touched they can no longer be irritated so as to ooUapse, as they do in their natural condition. They remain iu this passiye state, benumbed, as it were, for a consider- able time, and generally it is not untU some hours have elapsed that they regain their original sensibility. If, however, while ia this passive state, the leaves be again touched with chloroform, they coUapse as before. It is not till after several doses that they lose their sensibility entirely, or at all events until the next day ; sometimes they wither completely after too many applications of the chloroform. The purer the chloroform and the greater the excitability of the plant, the greater are the effects produced." Similar experiments with rectified ether gave results quite analo- gous. When the author repeated the experiment with chloroform, he found that the leaflets remained paralysed, as it were, and still unable to open after eighteen hours' rest ; they seemed to be dead. This was apparently caused by excess of chloroform, a laiger dose than that em- ployed by Dr. Marcet having been used. It is thus seen that overdoses of chloroform kiU. plants as well as animals, though small doses are inaoouous. b. There grows commonly ia ditches and stagnant water a plant called Chara, in the large cells of which a current of green globules steadily rises up one side and falls by another, presenting an appearance calling to mind the motion of an endless chain. If one of these cells is choked by a Ugaioire, then the motion contiuues exactly as before in each of the two divisions so produced. The singularity of the motion, and the ease with which it may be observed, have rendered this plant a favourite object of examination by young microscopists. Those philosophers who refused to admit this to be a vital motion analogous to that of the blood, imagined that they had found an explanation in electrical action. But Dutrochet, who once held this opinion, when he attempted to establish his hypothesis upon experiment, found that the magnetic force, even when prodigious, exercises no influence whatever upon the circulation of fluid within the cells of Chara, and he was obliged to admit the presence of a vital force, of the nature of which we are whoUy ignorant. Motion of an analogous nature has been now remarked within the cells of so many plants that we cannot doubt it to be a universal phenomenon. It is to be remarked that this kind of movement is whoUy independent of the general motion of the sap. c. When a grain of pollen falls upon a stigma, it protrudes a tube of extreme tenuity. The tube penetrates the stigma, much in the same manner as the root of a seed pierces the earth. Thence it proceeds unerringly to the tiny opening which it is destined to enter, passing by all obstacles, turning to the right or to the left, and now ascending, now curving back again, with the same constant certainty as would attend an act of consciousness. Nor is this all ; in certain cases the 10 MANIFESTED BY POLLEN-TUBES, ETC. entranoe of the pollen- tube into the young seed through its foramen,* is assisted by movements on the part of the seed itself, as in the common garden Thrift ( Armeria) in -which a horizontal strap, interposed between the pollen-tube and the foramen, is spontaneously removed in order to enable the former to enter the latter. These phenomena, varying as the structure of plants itself varies, and destined as they evidently are to ensure that great end, the propagation of species, are wholly inex- plicable upon any other principle than that of high vitality ; so high indeed that they are only less than voluntary actions. d. But perhaps nothing places the presence of a powerful vital force in stronger evidence than the facts which modem botanists have discovered in connection with the propagation of the lower orders of plants. It has been known from the observations of the younger Agardh, that in fresh-water Confervse the seeds (technically called spores) swim about with activity in the interior of the cell which generates them, that they eventually force their way through a thin part of the cell waU, andthenoe darting into the water move about with great activity, the lighter end downwards, and therefore contrary to the force of gravitation. These motions last for several hours. More recently it has been demonstrated that the motion is caused by delicate vibratile cilia or fringes attached to the small and narrow end of the seed (spore). This motion is stopped instantaneously by any poison, such as iodine, being allowed to mingle in the water. Discoveries of a similar nature have been made among other races of plants. Modem research has shown that in the greater part of the lowest forms of vegetable Ufe, and probably in all, minute spiral bodies exist having the power of active locomotion in many cases. These are called Aniheeozoibs in consequence of the bodies or antherids which contain them being regarded as analogous to the anthers of the higher orders of plants. Sea-weeds bear both spores and antherozoids. According to M. Thnret, whose observations are not open to doubt, by placing certain sea- weeds in a damp atmosphere, the spores and antherids are freely expelled, and remain on the surface of the fronds, from which they can be readily collected and transferred to vessels containing sea-water. M. Thuret found that when put iato separate vessels, the antherids placed by themselves immediately emit their antherozoids ; the latter move about with great activity, even for two days successively, but on the third, begin to decompose. Spores, also, when placed in sea-water by themselves, retaiu their vitality for some time, not decomposing in less than a week ; they even make attempts at growth, but abortions are the only consequence, and at last they perish also. It is otherwise when the spores and antherozoids are mingled in the same • The foramen is a mmute passage through the integuments of an ovule or young seed, into which the pollen-tube must enter in order to vivify the latent embryo VEGETABLE IRRITABILITY. H vessel of sea-water. Then ocoviis a series of most curious phenomena. The antherozoids attack the spores, creep, as it were, over their surface, and communicate, by means of their vibratile cilia, a rotatory motion, which is sometimes very rapid. "Nothing," says M. Thuret, "is more curious than the appearance of great brown spores rolling and tumbling about in the midst of a swarm of antherozoids." The result is the fertilisation of the spore, which then begins to grow, and in ten days becomes a little cellular brown oval body, supported by a trans- parent rootlet. Sea- weeds are by no means the only plants in which these most remarkable phenomena have been detected. Most cryptogamic plants have now been observed to possess locomotive organs, analogous to antherozoids and bearing the same name. Liverworts, Mosses, Lycopods and Perns themselves are supplied by nature with parts of the same description. When a Fern-seed vegetates it forms a small, thin, two-lobed green plate or scale lying horizontally on the damp surface of the ground. In this scale, called a protothaU, lodge anthero- zoids and spores. By unknown means the former creep up to the latter, and fertilisation is accomplished. Wherever Fern-seeds have fallen, there a crop of these scaly protothalls springs up, as may be seen on the walls, or pots, or damp earth of any Fern-house. In each protothaU. is lodged an abundance of antherozoids and spores, the former active and capable of moving from place to place, the latter passive and stationary. Nor is there any thing in their structure which enables the observer to say whether the motions are voluntary or involuntary, so much do they resemble what is witnessed in animal life. So far then as the important phenomena of reproduction are con- cerned, we have indications not only of vitality, but of such a force being present in plants in great activity. Evidence of this kind, proving as it does beyond all doubt the presence of a vitality among plants identical with that of animals, though different in its manifestations, is greatly strengthened by the many known cases of what is called vegetable irritability. That of the Sensitive Plant, which shrinks from the touch ; of the OsciUating Saintfoin (Hedysarum gyrans) whose leaves move with as much appearance of spontaneousness as the polype ; the sleep of leaves and flowers which close at night and expand in the day; the violent recoil of the column of Stylidium, or of the lip of Draksea, when touched ; the oscillation of the labellum of many BolbophyUs and Pterostyles ; the snap of the traplike leaf of Dionsea which closes with great force whenever' one of its six bristle-shaped springs is disturbed — phenomena familiar to the naturalist — are all intelligible 12 VITAL PRINCIPLE UNIVERSAL. upon the supposition tliat they are the result of high vitality, inexpU- cahle if referred to the operation of mere material forces. One of the causes which have most embarrassed the progress of cultivation is not perceiving the presence among plants of this vital principle. Because plants neither walk, nor fly, nor crawl ; because they are not endowed with the sense of pain or pleasure ; because they neither struggle nor shriek, we are too apt to forget that they are aUve, and consequently to treat them as if but rods of metal or plates of leather. Once grant that they are living beings, that they breathe although we see no mouths, that they digest although no stomachs are discoverable by common eyes, and above all things, that they feel, however low their sensations may be, and half the modes of cultivation employed by unskilful gardeners will stand con- spicuous as palpable errors. Only show that plants are endowed with a life, identical in its nature with that of animals, and men must necessarily make it their first businesS'to study the history of that life, and to master all which interferes vrith its healthy exercise. Such a step once taken, no cultivator would poison plants by a contaminated atmosphere, or paralyse them by an eternal footbath of cold water, or suffocate them in places where no air can reach them, or starve them by withholding the food without which they cannot exist, or cram them with incessant meals of heavy indigestible matter, which can but reduce them to the condition of an apoplectic glutton. That power which causes the bud to sprout, the leaves to form, the poUen to act, the seed to produce its embryo ; which enables vegetation to breathe, and feed, and grow ; which distinguishes aU organised beings from the brute matter of which they consist, is the same as what gives to man the high attributes of his nature. It is VITALITY ; a word which so-called philosophers in their ignorance, or presumption, may sneer at, but which in truth is the un- known force that controls the energy of matter, and directs it to special ends. It is only when cultivation is conducted with a fuU appreciation of this fundamental truth that Horticulture rises above the level of unreasoning custom, and acquires a solid base upon which the rationaUa of the practices which experience seems to sanction can be permanently secured. CHAPTER II. GERMINATION. THE NATTIRE OF A SEED. — IIS BTTEATION. — POTVES OF GBOWTH. — CAUSES OF GEBMINATION. — TEMPERAITJEE. — LIGHT. — HXTMIDITT. —CHEMICAL CHANGES. A SEED is a living body, separating from its parent, and capable of growing into a new individual of the same species. It is a reproductive fragment, or vital point, containing within itself all the elements of life, which, however, can only be called into action by special circumstances. But while it will with certainty become the same species as that ia which it originated, it does not possess the power of reproducing any peculiarities which may have existed in its parent. For instance, the seed of a Green Gage plum will grow into a new individual of the plum species, but it will not produce the peculiar variety called the Green Gage. This latter property is confined to leaf-buds, and seems to be owing to the seed not being specially organised after the exact plan of the branch on which it grew, but merely possessing the first elements of such an organisation, together with an Lavariable tendency towards a particular kind of development. Under fitting circumstances a seed grows ; that is to say, the embryo which it contains swells, and bursts through its integu- ments ; it then lengthens, first in a direction downwards, next in an upward direction, thus forming a centre or axis round which other parts are ultimately formed. No known power can overcome this tendency, on the part of the embryo, to elevate one portion in the air, and to bury the other in the earth. It is an inherent property with which nature has endowed seeds, in order to insure the young parts, when first' 14 PHaiNOMENA OF GERMINATION. called into life, each finding itself in the situation most suitable to its existence ; that is to say, the root in the earth, the stem in the air. The conditions required to produce germination are, exposure to moisture, and a certain quantity of heat ; in addition, it is necessary that a communication with the atmosphere should he provided, if germination is to be maintained in a healthy state. A seed, when fuUy ripe, contains a larger proportion of carbon than any other living part, and so long as it is thus charged with carbon, it is unable to grow. The only means it possesses of ridding itself of this principle, essential to its preservation, but forming an impediment to its development as a new plant, is by converting the carbon into carbonic acid, for which purpose a supply of oxygen is necessary. It cannot obtain oxygen in sufficient quantity from the air, for it is cut off from free communication with the air by various means, either natural, as being inclosed in a thick layer of pulp, or in a hard shell or stone ; or artificial, as being buried to a considerable depth below the surface of the soil. It is from the water absorbed in germination that the seed procures the requisite supply of oxygen ; fixing hydrogen, the other element of water, in its tissue: and thus it is enabled to form carbonic acid, which it parts with by its respiratory organs, until the propor- tion of fixed carbon is lowered to the amount suited to its growth into a plant. It has been objected that the evidence adduced in support of this explanation is not conclusive ; and that there is nothing to show that the hydrogen of decomposed water enters into new combinations or is fixed ia tissue. But since no hydrogen is evolved during germination, it must necessarily be fixed or recombined after water has been decom- posed. That this last phenomenon occurs is proved by the experiments of Edwards and Colin, as given in the Comptes rendus (vii. 922), and quoted in Lindley's Introduction to Botany (4th edit., II. 261 and 272). But the formation and respiration of carbonic acid takes place most freely, though not exclusively, in darkness; if exposed to light, the seed again parts with some of its oxygen, and again fixes its carbon by the decomposition of its carbonic acid. INFLUENCE OF WATER AND HEAT UPON GERMINATION. 15 In addition to this, the absorption of water causes all the parts to soften and expand; many of the dry, but soluble, parts to become fluid ; sap, or vegetable blood, to be formed ; and a motion of fluids to be established, by means of which a communication is maintained between the more remote parts of the embryo. Heat seems to set the vital principle in action, to expand the air contained in the numerous microscopic cavities of the seed, and to produce a distension of all the organic parts, which thus have their irritability excited, never again to be destroyed except with death. What degree of heat seeds find most conducive to their germination, probably varies in different species. Chickweed (Stellaria media) and Groundsel (Senecio vulgaris) will germinate at a temperature but little above 33° Fahr. It has been imagined that electbicai action also promotes the germination of seeds. Sir H. Davy found that seeds placed in the vicinity of the positive pole of a voltaic pUe, germinated sooner than those near the negative pole ; and judging from the known powers of electricity it was not unreasonable to expect, that, Kke light and heat, it would exert influence on the growth of vegetables. Professor Edward SoUy, however, has shown, experimentally, by an extensive series of trials in the Garden of the Horticultuial Society, that this is not so. Seeds of Barley, Wheat, Rye, Turnip, and Radish, were, in several different experiments, found to germinate with increased rapidity, when exposed,to the influence of a feeble current of electricity of very low tension, and the plants not only came up sooner, but were more healthy than others; but, on the other hand, a number of experiments on other seeds had given quite opposite results, proving either that the germination of some seeds was retarded, whilst that of others was facilitated, by electricity ; or, that the effects, observed in both cases, were merely accidental. Out of a series of ftfty-five experiments on different seeds, twenty appeared in favour of electricity, ten against it, and twenty-five showed no effect whatever; and, on oarefoily counting the whole number of seeds up in the entire series, it was found that twelve hundred and fifty of the electrified, and twelve hundred and fifty-three of the non-electrified seeds had grown. Germination being established, by the absorption and decom- position of water, and by the requisite elevation of temperature, all the parts enlarge, and new parts are created, at the expense 16 INFLUENCE OF WATER AND HEAT UPON GERMINATION. of a mucilaginous saccharine secretion which the germinating seed possesses the power of forming. With the assistance of this substance, the root, technically called the radicle, at first a mere point, or rather rounded cone, extends and pierces the earth in search of food ; the young stem rises and unfolds its cotyledons, or rudimentary leaves, which, if they are exposed to light, decompose carbonic acid, fix the carbon, become green, and, by processes hereafter to be explained, when speaking of leaves, form the matter by which all the pre-existing parts are solidified. And thus a plant is born into the world ; its first act having been to deprive itself of a principle (carbon) which, in superabundance, prevents its growth ; but, in some other proportion, is essential to its existence. CHAPTER III. GEOWTH BY THE ROOT. BOOTS LENGTHEir AX THEIE POnSTTS ONLY. ABSOBB AT THAT PAST CHTEI'LT, — ^INCEEASE ISr DIAMETBE LIKE STEMS. THEIR OEieiN. — ^AEE EEEDDfG OEGANS. — ^WITHOTTT ITTJCH POWES OF SELECTING THBIB. 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As plants have little power of generating heat, like animals, except in particular cases, and very locally,* they are princi- pally dependent upon the media that surround them for the heat which they require. Consideriug the great importance of heat in their economy, it is, for the purposes of gardening, necessary to ascertain what proportion is usually borne to each other, in different countries, by the temperatures of th« earth and atmosphere, the chief media by which plants can be affected. Upon the temperature of the atmosphere there are numerous observations in many countries ; upon that of the earth much fewer. It has been considered that the temperature of springs affords sufficient evidence of the temperature of the, earth ; but, so far as vegetation is concerned, tliis evidence. is .unsatisfactory. Springs, deriving their origin from considerable depths, have a nearly uniform temperature all the year round : but the tempe- rature of the earth's surface varies with the seasons ; is extremely different in summer and winter ; ' and ' is affected by the quality of the soil, in proportion as that is more or less absorbent and retentive of heat. What we want to know, as respects vegetation, is, not the mean temperature of the earth at some distance from its surface, but the temperature imme- diately below the surface ; i. e. of that part of the soil which the roots of plants penetrate, and whence they derive their food. It is also requisite that this should be ascertained monthly, so as to fui'nish the means of comparing the terres- trial temperature with the periodical state of vegetation. Such being the case, the temperature indicated by springs will be too high in winter, and too low in summer, a most material error. I am indebted to Mr. Robert Thompson for the following highly important tables indicating the ascertained temperature of the earth in various parts of the world. * AllusioD is here, of course, made to the extrication of leat during the periods of flowering and gennination, phenomena which have no otvions connexion with cultiva- tion. 118 TEMPERATUKE OF ENGLAND. II. — ^Mean Tempebatubb of the Earth and of the Air at Chiswiok, lat. 51° OH the AVEBAQB of 10 YEARS, 1844 — 1853. Mean TEMPEKAinini OF THE BAKTH. Meak Temp, of Atk. Difference. Months. 1 foot. 2 feet. Mean of land 2 feet. Earth warmer thau air. Earth colder than air. January February March . April . May . June , July . August September October November December • 40-07 39-74 40-96 46-47 63-11 60-02 62-85 61-80 57-54 51-52 46-01 41-13 41-02 40-51 41-57 46-25 52-01 58-47 61-71 61-26 57-89 52-79 47-28 42-83 40-54 40-12 41-26 46-36 52-66 59-24 62-28 61-53 57-71 52-15 46-64 41-98 38-21 38-42 40-49 46-57 53-54 60-45 63-40 61-28 56-14 49-35 42-89 38-14 2-33 1-70 0-77 0-25 1-57 2-80 3-75 3-84 0-21 0-98 1-21 1-12 50-10 50-30 50-20 49-07 1-13 From the above it appears that, in the first three months of the year, the thermometer at the depth of two feet indicates a somewhat higher temperature than that at one foot deep. The latter, from April till August, is higher than the one at two feet. But from September till the end of the year, or in fact till April, the ground at two feet deep is wanner than at one foot. Agaia, it will be seen that in AprU, May, June, and July, the earth at one and two feet deep is on the average nearly a degree colder than the air ; but iu aU the pther months it is warmer. TEMPERATURE OF SWEDEN. 119 III. — Temperature of the Earth and op the Air at Upsai, lat. 59° 52' ; ON the averaoe op 8 tears, 1838 — 1845. (Calculated from data in a M6mowe sw la TempSratwre de la Terre a Upsai, par A. J. Angstirom.) Meak Tempeeattjre of the EAUTm Mean Temp, or THE Air. DlFEEKENCE. Months. 2 ft. deep. 3 ffc. 10| in. deep. 6 ft. 10 in. deep. 9 ft. 9 in. deep. Mean of 2 ft., and 3 ft. lOJ iu. Mean of Earth at 2 ft. and 3 ffc. lOi in. ip ^ m Jairaary 33-55 36-85 41-27 45-38 35-20 23-70 11-50 February 31-43 35*25 37-57 43-36 33-34 19-96 13-37 March. 31-16 34-22 36-32 41-84 32-69 25-65 7-03 April . 34-87 34-85 37-90 40-66 34-86 37-17 2-31 May . 46-44 43-44 39-86 41-15 44-94 49-07 4-13 June . 56-49 60-38 48-53 44-47 53-43 57-61 4-18 July . 60-12 55-10 51-27 48-90 67-61 60-64 3-03 August 60-96 67-79 53-78 52-36 69-37 60-62 1-14 Septembe r 56-11 54-91 53-59 54-22 65-31 52-06 3-44 October . 45-57 48-48 49-81 53-66 47-02 40-30 6-72 Novembe r 38-54 42-63 47-18 61-21 40-59 31-49 9-09 December 35-21 38-65 41-41 48-00 36-93 28-41 8-51 44-26 44-19 44-22 47-11 44-22 40-68 3-64 Notwithstanding the intensity of the Scandinayian winters, it appears that the thermometer at two feet deep falls very little below freezing, although the mean temperature of the air is far below that experienced in this country in the most severe winters. The difference between the temperature of the earth at 2 feet and 3 feet 10 j inches, on the average, and that of the air, is no less than 13-37° in the month of February. This great difference is doubtless owing to radiation of heat from the earth being prevented by a covering of snow. From April till August, the air, as at Chiswick, is warmer than the earth. 120 TEMPEEATUKE OF DENMARK. IV.— Tbmpeeature of the Earth and of the Air at Copenhasen, lat. 55° 41' ; OK the average op 8 TEARS, 1842 — 1849. (Trcmsactions of the Eoyal Society of Demmwrk.) Name, Mean temp, of the earth at 12 feet deep. Mean temp, of air. DiFFEBENCE. Earth warmer than air. Earth colder than air. January , February. March. . April . . May . . June . . July , . August . September October . November December 36-62 34-34 35-25 40-65 50-34 SS-Vl 60-36 61-V7 57-34 50-45 44-24 39-79 31-99 29-60 33-60 43-61 52-98 60-60 62-33 63-12 54-62 48-02 40-06 34-95 4-63 4-74 1-65 2-96 2-64 1-89 1-97 0-35 2-72 2-33 4-18 4-74 47-50 46-39 1-11 Earth warmer than the air in ■winter, early spring and autumn, but colder during the summer, are the results of observations made at Copenhagen by Mr. Weilbach. On the year, the average excess of the ground temperature above that of the air is almost the same as at Chisvdck, the former being 1-11, the latter 1-13. TEMPERATURE OF THE NILGHEKBIBS. 121 V. — ^Mban Tempekahjeb ov the Eakth and ob the Am at Dodabktta, NiLSHBRRT Hills, lat. 11° 23'; elevation 8640 feet above the level OF THE SEA. {Met. Ohs., by T. G. Taylor, Esg^.) Temperature of the Earth, at 1 foot deep. , Temperature OF the Air. DiFFEREKOE. Months. Max. Min Mean. Mix. Min. ■Meta. Ill January . February. Maret, . April . . May . . June . . July . . August ■ September October . November December 62-00 57-70 63-40 62-40 63-60 56-80 56-30 67-80 54-40 58-40 59-30 55-70 54-00 54-00 58-30 68-60 59-60 54-70 53-30 53-80 53-70 64-40 53-80 51-00 58-00 55-85 60-85 60-60 61-60 55-75 54-80 56-80 54-05 56-40 56-55 53-35 68-60 56-70 61-70 61-30 62-40 54-90 54-40 65-10 54-90 55-60 56-60 64-00 44-40 45-90 47-10 61-20 49-90 46-10 47-90 46-80 47-40 48-10 47-20 45-10 61-50 51-30 54-40 66-25 56-15 50-50 61-15 50-96 61-15 61-86 51-40 49-55 6-50 4-55 6-45 4-25 6-45 5-26 3-65 4-86 2-90 4-55 6-10 3-80 58-98 54-93 66-95 67-10 47-26 52-18 4-77 0-0 At this latitude and elevation, the average temperature of the earth at one foot deep is higher throughout the year than that of the air : the average difference being 4-77. The greatest difference occurs in January and March, and the least in September. 122 TEMPEKATUBE OF THE HIMALAYAS,'- VI. — Tempeeatukb op the Earth and op the Aik at Dobjilins, lat. 27° 3' ; ELETATiou 7430 FEET ABOTB THE LETEi OP THE SEA. (From data in Soaker's BvmaXa/yan Jowrnal.) Mean temp. of the earth at 24 ft. to 8 ft. deep. Mean temp, of air. DiFPEKENCE. Earth wanner than air. Earth colder than air. January . February. March. April . . May . , June . . July . . August . September October . November December 46-0 48-0 50-0 58-0 61-0 62'0 62-2 62-0 61-0 60-0 55-0 49-0 40-0 42-1 60-7 55-9 57-6 61-2 61-4 61-7 59-9 58-0 50-0 43-0 6-0 5-9 2-1 3-4 0-8 0-8 0-3 1-1 2-0 5-0 6-0 0-7 56-2 53-5 2-7 Here, as in tbe Nilgberry Hills, tbe temperature of the earth, is ia every month above that of the atmosphere, excepting in March. The desorepancy, as in lower situations and higher latitudes, is in favour of the earth being on the average warmer than the air, but more especially so 'va. winter. They nearly coincide in March and August. VII. — Tempekatuee op the Eakth and op the Am in the Plains op Behsai. At Dacca, lat. 23° 50', and 72 feet above the level of the sea. Dr. Joseph Hooker found the temperature of the earth at the depth. of two feet seven inches was 84°, in the end of May ; and the mean temperature of the air ranged at the same time from 75-3 to 95-5 ; its mean therefore nearly corresponded with that of the earth. At ten stations in these plains, varying from 72 to 131 feet, above the level of the sea, the mean of the indications of the ground thermometer during May was 85-53 ; the approximate mean temperature of the air was 82-30 ; the difference therefore was only 3-23. OP THE PENINSULA OF INDIA, AND AUSTRALIA. 123 VIII. — Temperahtre of the Eabth and Aib, as obseeved by Captain Newbold AT BeLIART, on the CENTRE OF THE TABLE-LAND OF PENINSULAR IhDIA, LAT. 15° 6' N. ; ELEVATION 1600 FEET ABOVE THE LEVEL OF THE SEA. In tie hot month of May, skytmclouded; soil reddish and light in texture, completely sheltered by a thatched roof; depth of thermometer for temperatire of the earth one foot. Barth. Air iu Shade. Two P.M. Earth. Air in Sliade. First Day . Second Day. Third Day . Fourtt Day. 86-5 86-0 85-5 87-0 81-0 78-0 78-5 75-0 ^1-3 89-0 90-0 89-0 96-5 92-0 95-0 92-0 86-0 78-1 89-! 93-9 Mean temperature of the earth one foot deep at sunrise and 2p.m 87-9 Mean temperature of the air at sunrise and 2 p.m. . . . 86'0 Diflference 1-9 From the above it appears that the earth was nearly four degrees warmer at 2 p.m. than at sunrise ; and that on the average it was nearly two degrees warmer than the air. IX. — Variations of Tempebatttkb in New Holland, aocordino to Sir Thomas Mitohell's Observations. a. Noonday Temperatures. Lat. Months. Averages. Max. Min. 29° s. Nov. Dec. of 3 observations 102° 103° 62° 32° s. Jan. Feb. » 18 „ 971 115 73 31° s. Feb. March „ 17 „ 90 110 80 30° s. March „ 20 „ 95 106 84 Nov. Dec, averaging at noon 102° Jan. Feb., „ „ 97| Feb. March, ,, „ 90 March, ,, ,,95 b. Night Temperatures. Occasional Temperature at Sunrise. 62° 58° 61° 61 69 47 61 64 48 68 65 47 (See Journal of Horticultural Society, III. 297.) 124 TEMPERATURE OF EARTH -Mean Temperature of the Earth and op the Air at Trevandrum, in India, lat. 8° 30', N.; eievatioh 200 eeet above the level oj? the SEA. Aa OBSERVED BY JoHN CaLDEOOTT, ESQ., AsTRONOMER TO THE EAJAH OF Tratanoore, ddrikg the tears 1843, 1844, 1845. Montlis. Meak Tempbeattjbe of THE Eauth. Mean Temp, of THE Am. DiFFEEENOE. Earth at 3 feet. 12 feet. 6 feet. 3 feet. Earth warmer than air. Earth colder than air. January . 85-528 85-618 84-954 78-930 6-024 February . 85-784 86-625 86-838 80-386 6-452 Maroh . . 86-373 88-110 88-789 82-730 6-059 April . . . 86-916 88-527 89-614 83-370 6-244 May . . . .... 88-224 88-413 81-603 6-810 June . , . 86-878 86-883 85-012 79-023 5-989 July. . . 86-537 85-114 83-250 78-450 4-800 August I . • 85-894 •84-736 83-566 7«-990 4-576 September ' . 85-633 85-133 84-575 79-973 4-602 October . . 85-680 85-632 84-722 79-076 5-646 November . 85-651 85-271 84-622 79-750 4-872 December . 85-607 85-303 84-228 78-030 6-198 86-043 86-264 85-715 80-025 5-690 000 Here, as at Dodabetta, tbe mean temperature of tbe earth averages higber tban tbat of the air in every month throughout the year, the excess on the whole being upwards of 5| degrees. At Trevandrum, it appears that the highest mean temperature of the earth at three feet deep occurs in April, and is nearly 90° ; the lowest occurs in July, when it is a little above 83°. Its mean range is between 6 and 7 degrees. The mean temperature of the air is highest in April, 83-37°, and lowest in December, 78° ; so that the difference between the hottest and coldest months is only 5 or 6 degrees. The preceding tables exhibit the relative temperature of the earth and air at a number of places very differently situated both as regards latitude and elevation ; from Dpsal in lat. 59° 52', to Trevandrum in lat. 8° 30' ; and from Chiswick, Copenhagen, and the Plains of Bengal, aU near the level of the sea, to Dodabetta and DorjUing, respectively 8640 and 7430 feet above that level. The general results deduced from these tables are as follows : — First. — That va. all cases the mean temperature of the earth exceeds that of the air, on the average of the whole year. IN THE PENINSULA OF INDIA. 125 Second, — That in some localities, tte montUy mean temperature ot the earth is in eyery month, more or less, higher than that of the air. Third. — That in other localities the mean temperatvue of the air exceeds that of the earth in the summer months only, or from April till July or August ; but from September till March, the earth is warmer than the air. The excess of mean temperature of the earth above that of the air j on the ayerage of observations taken at different places, is as follows : — Chiswick 1-13 TJpsal 3-54 Copenhagen ..... 1-11 Dodabetta 4-77 Dorjiling 2-70 Plains of Bengal 3-23 BeUary 1-90 Trevandrum 5'69 Average 3 -01 From this it will be seen that at these places the average difference between the temperature of the earth and the air is least at Copenhagen, and greatest at Trevandrum. But it must not be thence inferred that the difference is uniformly greater within the tropics than in high latitudes, for we have, on the other hand, a greater difference at Upsal, than at BeUary on the centre of the table-land of India. There appears to be no series 'of direct observations upon the superficial temperature of the earth, at the different periods of vegetation, in other countries ; but some statements are to be found, here and there, concerning the temperature occasionally observed, from which it is to be inferred that the earth is heated, at least for short periods of time, very much above the atmosphere, and it is probable that this excessive elevation of temperature is necessary to the healthy condition'of many plants. From some interesting Qbservations communicated to me by Sir John Herschel, it appears that the temperature of the earth at the Cape of Good Hope is often excessive. On the fifth of December, 1887, between one and two o'clock in the day, he observed the heat under the soil of his bulb garden, to be 159°; at three p.m. it was 150°, and even in shaded places 119°: the temperature of the air in the shade, in the same garden, at the same period, was 98° and 93° At 5 p.m. the soil of the garden, . having been long shaded, was found to have, at four inches in 126 EARTH TEMPERATDEE. depth, a temperattire of 103°. " On the third of Decemher, a thermometer huried a quarter of an inch deep, in contact with a seedling fir of the year's planting, quite healthy, and having its seed-leaves marked as follows.- — at ll"" SS"" a.m. 148-2°, at Qi" 48™ p.m. 149-5°, at 1'" 34'" p.m. 149-8°, at 1^ 54™ p.m. 150-8°, and at S^ 46™ p.m. 148°." Sir John Herschel observes that such ohservations " go to show that at the Cape of Good Hope, in the hot months, the roots of bulbous and other plants which do not seek their nourishment very deep, must frequently, and, indeed, habitually, attain temperatures which we can only imitate in our hothouses by actually suspending over the soil plates of red-hot iron. For it must be remarked, that heatiag the ground /rom behw would not distribute the temperature in the same way." Memoranda conoermng the temperature immediately below the surface of th.e earth, oeoasionaUy remarked in different countries : — 133°— 144° . ( ^'"'°r^™g ^ Edwards * ( and Colin. Often 126°— 134° .... Humboldt, Fragm. As. Coarse white sand at 140°, s the atmosphere being [ 84-5° 118°— 122°; once 127°, the atmosphere being 91-5° 113° — 118° among dry ] grass J 85° usual summer temp. one foot below surface . 159° under the soil of bulb garden 142° thermometer barely \ covered ....,; Water of rice fields 113° adjacent sandy soil much higher ; for towards midday the black sides of the boat were 142-50° Egypt. . . Tropics . . Oronoco . . France . . Chile . . . New Grenada Cape of Grood Hope . . Bermuda . . Lantao, Chinas: of a ) Humboldt. Arago, as quoted by Edwards and Colin. Boussingault. Hay, in Zoudon's Gard. , vi. 437. Herschel [MSS.). Col. Emmet. ^Meyen. These observations seem to confirm the late Mr. Harvey's suspicicJns, that the real force of the sun's rays in tropical countries is still far from being ascertained. When, therefore. BAETH TEMPERATDKE. 127 we are informed by travellers that tlie temperature in the sun, at Gondar, has been seen to be 113° (Bruce); at Benares 110°, 113° 118° (Harvey) ; or at Sierra Leone, 138° (Winterbottom) ; it must be supposed that, in reality, the temperature would have been found much higher in those places had more efdcient means of observation been employed. Mr. Foggo, indeed, succeeded, by means of a large thermometer, having the baU covered with black wool, and fully exposed to the direct rays of the sun, unsheltered from the wind, in obtaining, at Edinburgh, on the 29th of July, at B^ 10" p.m., an indication of 150°, and at 3*^ p.m. of 140°, while another instrument, similaxly prepared, and resting in contact with herbage, was found to indicate only 119° and 110°; so that, as Mr. Foggo remarks, a difference of 30° was produced in these cases solely from the manner in which the instruments were exposed. {EdAnhwrgh Philosophical Journal, No. xxvii.) For horticultural purposes a far more extensive series of observations than we at present possess requires to be made at a great number of different places, with a view to determine the connexion between the temperature of the soil and the seasons of vegetation. In making these, the nature of the soil in which the thermometers are plunged should, among other circum- stances, be very precisely described ; for it is obvious that the result will be essentially affected by the peculiar conducting power of the earth. In the meanwhile the two following diagrams, and the observations which follow, for which we are indebted to Mr. Thompson, throw much light upon this obscure subject. " It will be seen from the diagram of the mean monthly tem- perature of the earth and air at Chiswick, that the earth, at two feet deep, is warmer than the air by two or three degrees at the commencement of the year ; but the lines representing the progress of the respective temperatures gradually approximate, the ground one falKng and the air rising a little towards the end of February. In March, both take a decided start, and towards the end of that month the lines coincide, and then the air temperature is higher than that of the earth till August, when the contrary takes place. The mean temperature of the 128 EAETH TEMPEEATUEE, LONDON. & & w Is EH <1 m u e3 o »« K5 o W3 «s 3 A J / / / 1 1 13 y / • / / / / / U O y /■ • ' • ^ y' /' ^ ^ /* / / / / z' /" /* 1 / t f / 1 ( V \ \ \ hI \ s \ s 'n ^ s s S S S \ 1 s < s '\ ■s ^ 1 s \ s ^ \ g \ i 1 f - s o (0 o 15 nj o i us EAETH TEMPERATURE, INDIA. 129 1^ H m EH 1^ HI PS 130 RELATION BORNE BY THE TEMPERATURE air begins to decline about the middle of July ; that of the earth about the 1st of August; and as the latter does not rise so high nor so quickly with a generally ascending temperature, so it falls more slowly and not so low as the air when the general temperature is declining. The diagram for the temperatures at Trevandrum, exhibits two nearly parallel curved lines, the earth averaging a little more than five and a half degrees higher than the air. The greatest approximation is in August and September, as is generally the case at other places in the tropics, and likewise in colder latitudes ; but in the latter there is a coincidence of the lines in March or April which is not followed at Trevandrum. On the contrary, the powerful sun-heat which there prevails in the months of February, March, and April, appears to heat the earth more than the air, till the setting in of the rainy season, in consequence of which the earth is lowered from its maximum, 89"61 in AprU, to its minimum 83'25 in July, or more than 6°; whilst the air is lowered, during the same period, scarcely 5°. "From the foregoing facts and diagrams we can form a tolerably correct idea of the relation which the monthly mean temperature of the soil bears to the monthly mean temperature of the air throughout the year. The latter is known at a vast number of places ; but that of the earth comparatively at very few. It may, however, be estimated with sufficient accuracy for all practical purposes connected with horticulture and agri- culture. For example, we may take the tables and diagram for Chiswick as our guide, for all places having nearly the same monthly and annual temperature. Where the winters are colder, as at Copenhagen, we must add 2° or 3° more than for Chiswick to the temperature of the air in January, in order to obtain, approximately, the temperature of the soil for that month. In AprU, throughout the world, from lat. 60° to lat. 30°, the mean temperature of the earth and air may be considered to average alike, or to differ rarely more than 1°. From April to July, subtract about 2° from the monthly mean of the air for that of the earth. In August the temperatures again coin- cide. The earth, after this, maintains a higher temperature than the air throughout the remaining months ; so that in OF EARTH TO AIR. 131 September, 1° to 2°; October, 2° to 3°; and in November and December, between 3° and 4° must be added to the mean temperature of the air, in these months respectively, in order to obtain the approximate mean temperature of the soil. This will apply to aU places having a climate resembling that of Chiswick. But where the temperature of the air falls very low in the end of autumn, and beginning of winter, as at Upsal, where the mean of the air in October is 12° below that in September, 6 or 7° must be added to the mean of the air, for the mean temperature of the earth ; and 8 or 9° in each of the two following months. On the contrary, where the winters are milder than at Chiswick, the difference between the earth and air temperatures will be somewhat less than that which appears in the table, and represented in the diagram for that place. "Within and near the tropics the earth, it appears, is, on the average, always warmer than the air by several degrees. In some months, and at some places, both temperatures are nearly alike ; and in other instances they differ as much as 6 or 7°, much depending on the fall of rain, and the nature of the soil. If we add 2° to the temperature of the air, in June, July, August, and September, and 4° in the other months, we shall approach the monthly mean temperature of the soil between 0° and 30° latitude, sufficiently near for all practical purposes ; certainly much nearer than the temperature to which plants from that soil have been subjected by artificial treatment in this country." It must, however, be understood that such calculations are necessarily uncertain, and can only be taken as rough approxi- mations to truth, near enough for practical purposes, but nothing more. An infinite multitude of circumstances, reducible within no general rules, modify all such estimates. As regards the Indian seasons, the greater part of the west and south coast of the peninsula is so damp that the growing and flowering season lasts all the year round. Even of Eice there are, according to Buchanan Hamilton, two crops in Malabar : — one sown in May, transplanted in June, and reaped in July ; another sown in August, transplanted in September and October, and reaped in November. In Northern India the growing season for tropical crops — Eice, Millet, &c. — generally k2 132 TROPICAL SEASONS. speaking begins with the rains (May and June), and lasts all the rains; August and September are fruiting months, and these are followed by rest for such crops. Then, however, Oats, Barley, Tobacco, Wheat, Sesamum, Poppy, and all Pulses are put in to be reaped in spring. In Malabar on the average the seasons are the same, but the dry season is so damp that the most tropical crops can be raised all the year round. Of course in the Southern Hemisphere the seasons are the reverse of those in the Northern, midwinter in Sydney cor- respondiug with midsummer in Europe. In the tropical parts of America, where Humboldt found the mean temperature of the coldest month not to be lower than 79'16° at Cumana, we shall be justified in concluding that the temperature of the earth's surface never falls permanently below that amount ; and as the mean summer temperature of the place was found to be 83'04°, so it is probable that the earth wiU have somethiag above that degree of warmth, on an average, in the summer. For the warmest month, thia great observer gives 84-38° as the mean, which corresponds remarkably with the temperature a foot below the surface in New Grenada, where, according to a correspondent of Mr. Hay, it is 85° during summer, " as a gentleman, a planter there, wrote home for his information." (See LoudorHs Oard. Mag,, vi. 437.) BOOK II. OP THE PHTSIOIiOGHOAL PRINCIPLES UPON WHICH THE OPEEATIONS OP HORTICULTURE ESSENTIALLY DEPEND. All operations in horticulture depend for success upon a correct appreciation of the nature of the vital actions described in the last Book; for although there have been many good gardeners entirely unacquainted with, the science of vegetable physiology, and although many points of practice have been arrived at altogether accidentally, yet it must be obvious that the power of regulating and modifying knowledge so obtained cannot possibly be possessed, unless the external influences by which plants are affected are clearly understood. Indeed, the enormous difference that exists between the skiU of the present race of gardeners and their predecessors can only be ascribed to the general diffusion, that has taken place, of an acquain- tance with some of the simpler facts in vegetable physiology. In attempting to apply the explanations of science to the routine of horticultural practice, it appears desirable, in order to avoid frequent repetition, that mere details should be omitted, and that those general operations should alone be adverted to which, under many different modifications, and in various forms, constitute the foimdation of every gardener's education. CHAPTBK, I. OP BOTTOM HEAT. This term is, in common practice, made use of only in those cases where the temperature of the soil in which plants grow is artificially raised considerably ahove that which we are ac- quainted with in England; and there seems to be a general idea that such an artificial elevation of temperature is only necessary in a few special instances. It has, however, been shown (p. 135) that the mean temperature of that part of the soil in which plants grow is universally something higher than that of the air by which they are surrounded, and consequently it appears that nature, in all cases, employs some degree of bottom heat as a stimulus and protection to vegetation. At the same time, it must be admitted that, in some cases, the amount is extremely small ; for Von Baer found Ranunculus nivalis and Oxyria reniformis flowering in Nova Zembla, where the soil was not warmed above 34^" ; and, in Jakutzsk, Erdmann states that Summer Wheat, Rye, Cabbages, Turnips, Radishes, and Potatoes are cultivated, although the ground is not thawed above three feet in depth. How tie warmth of the soil may act as a protection to plants will be easily understood. A plant is penetrated in aU directions by in- numerable air passages and chambers, so that there is a free commxmi- cation between its extremities however far they may be apart. It may therefore be conceived that if, as necessarily happens, the air inside the plant is in motion, the effect of -warming the air in the roots will be to raise the internal temperature of the whole individual ; and the same is true of its fluids. Now, when the temperature of the soil is raised to 150° at noonday by the force of the solar rays, it will retain a con- siderable part of that warmth during the night : but the temperature NATURAL TEMPERATURE OF SOIL. 135 of the air may fall to such a degree that the excitability of a plant woTild be too much and suddenly impaired, if it acquired the coldness of the mediiun surrounding it ; this is prevented, we may suppose, by the warmth communicated to the general system, from the soU, through the roots ; so that the lowering of the temperature of the air, by radiation during the night, is unable to affect plants injuriously, in consequence of the antagonist" force exercised by the heated soil. It is not impro- bable that this fact may be hereafter applied in gardening to the acclimatising of half-hardy plants. "Were an open border heated artificially in the winter, it is possible that plants might endure an amount of cold upon their stems and leaves, which in the absence of such heat would be fatal to them. An experiment upon this subject was tried some years ago, and although it was conducted so negligently and unskUfully, as not to justify any inference being drawn from it, yet the result, such as it was, was full of promise. That elevating the temperature of moist soil produces an unusual degree of vigour in plants unaccustomed in nature to such an elevation is a fact which requires no proof; it is attested hy the condition of vegetation round hot springs, and in places artificially heated by subterraneous fires ; and this has probably been the cause of the employment of tan and hot-beds, by which means bottom heat has been generally obtained for rearing delicate species, and especially seeds. But if this stimulus acts in the first instance beneficially in all cases alike, it soon becomes a source of mischief in those species vyhich are natives of climates where such terrestrial heat is unknown, the latter " drawing up," as the saying is, becoming weak and sickly, and speedily presenting a diseased appearance. On the other hand, it is equally well known that, unless the temperature of the soil be raised permanently to at least 75°, the seeds of tropical trees will not germinate ; or, if they do, they push forth feebly, and from the first present the sickly appear- ance of plants suffering from cold. Hence arises the impossi- bility of making the seeds of tropical plants germinate when sown in the open air in this country, where the mean tempera- ture of the earth seldom rises to 65°, and that for only short periods of time. It is, therefore, obvious that aU plants require some bottom heat ; but the amount varies with their species, and the only means of determining what the amount should be 136 SOIL OF THE ORANGE AND VINE. is afforded by the known degree of warmth of the climate of which a plant may be a native. When plants are cultivated in glass houses, there is little difficulty in supplying them with the amount of bottom heat which they may require ; but this can either not be effected at all, or only to a limited degree, by a selection of soils and situ- ations, when plants are cultivated in the open air ; and hence one of the many difficulties of acclimatising in a cold country the species of a warmer climate. It is true that plants will exist within wide limits of temperature, and, consequently, a few degrees of difference in the natural bottom heat to which they are exposed may not affect them so far as to destroy them ; but it cannot be doubted that the conditions most favourable to their growth are those which embrace a temperature rather above than below that to which they are accustomed in their native haunts. The Orange-tree is found in perfection where the tempera- ture of the soil may be computed to rise to 80° or 85°, and never to fall below 58°, as in the Bermudas, Malta, and Canton. How injudicious, then, is our practice of exposing it during summer to the open air, in tubs, where the soil scarcely rises in temperature above 66°, and preserving it during winter in cold conservatories, the soil of which often sinks to 36° ; under such circumstances the Orange exists indeed, but where are the perfume and juiciness of its fruit, and where the healthy vigour of its noble foliage ? The Vine cannot be grown in the open air of this country to any useful purpose, except when trained to walls, in soils and situations unusually exposed to the beams of the sun; it is only then that it can obtain for its roots such a permanent warmth as 75° which it will have at Bordea,ux, or 80° in Madeira. It may hence be considered an axiom in horticulture, that all plants require the soil, as well as the atmosphere, in which they grow, to correspond in temperature with that of the countries of which they are natives. It has also been already shown, that the mean temperature of the soil should be above that of the atmosphere. How much above depends upon climate a,nd season. The meaii difference in favour of the. WARMTH CAUSED BY DRAINAGE. 137 ground at Chiswick is only 1°13 as is shown at p. 125, while that of Trevandrum, an Indian station, is 5°69. But it must be remembered that, disregarding means, the monthly temperature exhibits very much greater differences. Thus at Chiswick the earth is nearly 4° warmer than the air in December, and that of Trevandrum is nearly 6^° warmer in the month of February : these differences are themselves insignificant when contrasted with what occurs at Upsal (p. 119), where the earth is warmer than the air by 13°37 in the month of February. It seems evident that in the examples of a high winter tempera- ture of the earth in severe latitudes, we have an example of the protection thus afforded to the vitality of plants iu the manner suggested in the preceding page. There can be no sort of doubt, that the advantage derived from draining cold countries, is owing greatly, if not exclusively, to the augmented temperature which attends the removal of stagnant water from land. Undergeound Cximatb is not less important than that^ which is experienced above ground. It is only by perfect and skilful drainage that underground climate is improved. No other means of effecting it on a large scale are known ; it is probable indeed that the superiority of common littery stable manure over artificial composts, as weU. as the increased efficacy of the latter when mixed with the former, is a mere exempUflcation of the advantageous effects of perfect drainage. Some believe that the advantage of drainage consists in removing water. But water is not of itself an evil ; on the contrary it is the food of plants, and its absence is attended with fatal results. It is the excess of water which injures plants, just as an excess of food injures animals. Those who imagine that the advantage of drainage arises from the removal of stagnant water, or any such cause alone, overlook the great and important fact that drained land is, in summer, from 10° to 20° warmer than water-logged land. Professor Schubler long ago came to the conclusion that the loss of heat caused by evaporation in undrained lands amounted to 11J° to 13|° Fahr. Mr. Parkes has shown, in his " Essay on the Philosophy of Drainage," that in draining the Red Moss near Bolton-le-Moors, the thermometer in the drained land rose in June, 1837, to 66° at seven inches below the surface, while in the neighbouring water-logged land it woiild never rise above 47°, an enormous gain. In the garden of the Horticultural Society the mean temperature of the thoroughly drained soil at one foot below the surface is, in the month of July, 63°49 ; if we take that of water-logged land to be the same as spring water, or 47°, there is a gain of 16^°. Thus it 138 DRAINING SOIL WARMS IT. is eyident that drainage produces tie very important effect upon land of raising its temperature ; it communicates bottom heat, in the absence of some amount of which, even the common Nettle and Groundsel would perish ; and as scarcely any of our cultivated crops are natives of countries so cold as our own, it is manifest that they aU req[uire to have the earth warmed for them, or are much the better for it. The reason why drained land gains heat, and water-logged land is always cold, consists in the weU-known fact that heat cannot be transmitted downwards through water. This may be readily seen by the following experiments : — ExPBBiMEiirT Wo. I. — A square box was made of the form represented by the annexed diagram, eighteen inches deep, eleven inches wide at top, and six inches wide at bottom. It was filled with peat saturated — -U- ::::0 r.:. Fig. XXVII. with water to c, formiag, to that depth (twelve and a half inches), a sort of aitittoial bog. The box was then fiUed with water to d. A thermometer (o) was plunged so that its bulb was within one and a half inch of the bottom. The temperature of the whole mass of peat and water was found to be 39i° Fahr. A gaUon of boiling water was then added; it raised the surface of the water to c. In five minutes the thermometer arose to 44°, owing to conduction of heat by the thermometer tube, and its guard. At ten minutes from the introduction of the hot water the thermometer a rose to 46°, and it subsequently rose no higher. Another thermometer (6), dipping under the surface of the water at e, was then introduced ; and the foUowing ore the indica- tions of the two thermometers at the respective intervals, reckoning from the time the hot water was supplied : DRAINING SOIL WAEMS IT. 139 20 m. 1 h. 30 m. 2 h. 30 m. 12 h. 40 m. Thermometer b. Thermometer a. 150° ... 46° 101 ... 45 801 . ... 42 45 ... 40 The mean temperature of the external air to ■which the box was exposed during the above period was 42°; the maximum being 47° and the minim.um 37°. ExPEEiMENT No. II. — With the same arrangement as in the preceding case, a gallon of boiling water was introduced above the peat and water, when the thermometer a was at 36° ; in ten minutes it rose to 40°. The cock was then turned for the purpose of drainage, which was but slowly effected, and at the end of twenty minutes the thermometer a stUl indicated 40°; at twenty-five minutes 42°, whilst the ther- mometer 6 was 142°. At thirty minutes the cock was withdrawn from the box ; and more free egress of water being thus afforded, at thirty- five minutes the flow was no longer continuous, and the thermometer 6 indicated 48° The mass was drained and permeable to a fresh supply of water. Accordingly another gallon of boiling water was poured over it and in 3 minutes the thermometer a rose to 77° 5 „ „ feUto76i 15 j> J) J) 71 20 „ ,, remained at 70^ Ih. 50 „ „ „ 70| In these two experiments the thermometer at the bottom of the box suddenly rose a few degrees immediately after the hot water was added; and hence it might be inferred that heat was carried down- wards by the water. But in reality the rise was owing to the action of the hot water on the thermometer, and not to its action upon the cold water. To prove this, the perpendicular thermometers were removed. The box was flUed with peat and water to within three inches of the top ; a horizontal thermometer (af) having been previously secured through a hole made in the side of the box by means of a tight-fitting cork, in which the naked stem of the thermometer was grooved. A gallon of boiling water was then added. The thermometer, a very delicate one, made by Newman, was not in the least affected by the boUing water in the top of the box. In this experiment, the wooden box is a field ; the peat and cold water represent the water-logged portion; rain falls on the surface and becomes warmed by contact with the soil and thus heated descends. But it is stopped by the cold water, and the heat will go no further. But if the soil is drained and not water-logged, the warm rain trickles through the crevices in the earth, carrying to the drain-level the high 140 COLD BORDERS CAUSE SHANKING. temperature it had gained on the surface, parts with it to the soil as it passes down, and thus produces that bottom heat which is so essential to plants, although so few suspect its existence. This necessity of warmth at the root undoubtedly explains in part why it is that hardy trees, over whose roots earth has been heaped or paving laid, are found to suffer so much, or even to die ; in such cases, the earth in which the roots are growing is constantly much colder than the atmosphere, instead of warmer. It is to the coldness of the earth that must be ascribed the common circumstance of Vines that are forced early not setting their fruit well, when their roots are in the external border and unprotected by artificial means ; and to the same cause is often to be ascribed the shanking or shrivelling of grapes, which most commonly happens to Vines whose roots are in a cold and unsunned border. Mr. Knight long since mentioned an important fact connected with this subject: — " It is well known," he said, "that the bark of Oak-trees is usually stripped off in the spring, and that in the same season the bark of other trees may be easily detached from their alburnum, or sap-wood, from which it is, at that season, separated, by the interven- tion of a mixed cellular and mucUagiuous substance ; this is apparently employed in the organisation of a new layer of iibre, or inner bark, the annual formation of which is essential to the growth of the tree. If, at this period, a severe frosty night or very cold winds occur, the bark of the trunk, or main stem, of the Oak-tree becomes agaiu firmly attached to its alburnum, from which it cannot be separated tUl the return of milder weather. Neither the health of the tree, nor its foliage, nor its blossoms, appear to sustain any material injury by this sudden suspension of its functions ; but the crop of acorns invariably fails. The Apple and Pear-trees appear to be affected to the same extent by similar degrees of cold. Their blossoms, like those of the Oak, unfold perfectly weU, and present the most healthy and vigorous character ; and their poUen sheds freely. Their fruit, also, appears to set well ; but the whole, or nearly the whole, falls off just at the period when its growth ought to commence. Some varieties of the Apple and Pear are much more capable of bearing unfavourable weather than others, and even the Oak-trees present, in this respect, some dissimi- larity of constitution." [Hort. Trans., vi. 229.) It is also the coldness of the soil which causes the production of roots upon the stems of the Vme in a hot damp Vinery ; AEEIAL VINE ROOTS. 141 which diminishes or prevents colouring; which renders it impossible to ripen wood ; and which deteriorates the quality of the Grape. Hence all good Vine-growers now look more to the temperature of their borders than to its mechanical condition. The FoHMATioN OF Aeeiai Roots by Yines is an. immistakeable sign of tiie eoldness of the border. Viaeries may be seen ■with these roots hanging down like beards from the branches ; and these are always followed by bad giapes, unless means are taken to heat the border. The explanation of the phsenomenon seems to be this : — The Vine possesses a very strong vegetating power, which is mani- fested whenever sttfflcient heat and moisture are present. It is also well known that if one portion or shoot of a Vine-plant is introduced to an atmosphere congenial to its growth, the buds will push into foliage and shoots ; whilst the rest of the plant, exposed to cold, will not be perceptibly affected, and will contribute nothing to the active vegetation of the branch introduced to heat and moisture. According to circumstances, therefore, vegetation may be active in one part, and at the same time comparatively dormant in another part of the same Vine-plant. If the natural roots are dormant owing to the low temperature to which they are exposed, then unnatural roots wiU be formed by branches if in a state of growth. Moisture favours the formation of these roots ; they shrivel in hot dry weather, but push again on the return of a dull or moist state of the atmosphere. They arise from the shoots being in a highly favourable situation for growth, and the roots in the reverse. The leaves elaborate a quantity of sap proportionate to their size, and to the share which light has had in perfecting their development. Part of this elaborated sap is appro- priated by the above-groxuid portion of the plant. But in ordinary cases, and more especially where a vigorous growth is promoted, there is always a surplus beyond what the stem and its dependencies above ground reqidre, and the proper destination of this is the roots, in order that their increase may correspond with that of the plant above them. But roots in a border five feet deep, and of a clayey nature, wLU be in a temperature little above 40° early in spring. At about 40° water has its greatest density. Under such circumstances any movement in the fluids of the roots must be extremely sluggish ; and were these roots as open to observation as the stem is, there is no doubt they would be found as dormant as a shoot left outside in the cold, compared with another introduced to the heat of a forcing-house. When the roots of Vines are healthy, in proper soil sufficiently warm, their growth proceeds in due proportion to that of the top, but if they are badly conditioned, they can neither act their part nor appropriate their share of the returning juices ; consequently an accumulation of the latter takes 142 AJERIAL VINE ROOTS. place in the stems, and, favoured by the moist warm atmosphere of the Vinery, bursts through the bark in the form of fibres, continuing to lengthen tiU they are checked by drought. An extraordinary pro- duction of these aerial roots was observed to take place whilst an experiment was being made with a Black Hamburgh Vine, in the garden of the Horticultural Society. It had grown vigorously in an open border, when, being in freedom, no rootlets broke from the shoots. A 3-light frame was placed over this plant, and made as air-tight as possible ; the sashes were never opened, except to supply water to the roots ; a thermometer inside the frame was generally raised every day above 140° by sun heat. An Orchid placed in a shaded part of the frame was killed in two days, yet the Vine continued to grow. It burst its wiater buds rapidly into shoots, and almost as soon as the buds on these young shoots were formed, they also pushed, weaker of course, and agaia stUl weaker growths proceeded from these secondary shoots. Meanwhile a vast number of roots issued from the shoots trained horizontally near the glass, and these roots soon reached the surface of the ground, which became matted by them, for it was moist, and for a little way sufficiently warm, by reason of the sxm.-heated air in the frame. But with regard to the old roots in the earth, the case was very different. The heated air of the frame could but slightly affect the soil at the depth where they were situated, whilst those extending beyond the limits of the fram.e were of course entirely beyond its influence. The consequences of a profusion of branch-roots on the Vine are these ; they absorb moisture from the air in the house, and so tend to increase the breadth of the foliage and swelling of the berries ; even the thickness of the wood is considerably increased by them, for it is not uncommon to see a Vine branch smaller at the base than higher up ; in short they are sources for the supply of nourishment, but they are sources which dry up when they are most wanted. They assist in forming a widely expanded foliage during moist weather; and when dry weather demands a greater supply, to compensate for increased evaporation from broad foliage, the stem-borne rootlets contribute nothing. To their precarious supply may be partly attributed the shanking and shrivelling of fruit. They should be checked in time by allowing the air in the house to become occasionally dry. But above all things, their appearance should be prevented by maintaining a due proportion between the temperature of the air and earth in which the Vines are plunged. The effect of aeiipiciallt warmiks a Vine bokdeb, in this country has been seen in many instances; not the least instructive of which occurred to Mr. Purday, the eminent and scientific gunsmith. In his garden at Bayswater, a Vinery was filled with wood and produced an abundance of excellent Grapes in little less than two years, by merely VINE BORDERS HEATED ARTIFICIALLY. 143 wanning the border. The first year the Vines made wood thirty-seven feet long, strong, short-jointed ani well ripened. But the plan was carried out still better at Castle Malgwyn, near Pembroke, the seat of A. L. Gower, Esq., by Mr. Hutchinson, who has described it in the Journal of the Horticultural Society. " The bottom of the border," he says, "is gently sloped from the houses to the extreme edge, where is bmlt a box-drain extending the whole length of the border, as shown in the accompanying section marked 1 ; this drain is one foot square, the top of it being level is) BOILER BOILER® Fig. XXVIII, — Ground plan of houses, showing cross walls beneath the Vine borders. with the bottom of the border, as also shown in section. When this was completed dwarf walls, marked 3, were built across the border, three and a half feet apart, one foot square, in the pigeon-hole manner : on the top of these walls are laid rough flags ; these in reality form the bottom of the border, and upon these is placed about six inches of broken stones and bricks, marked 4, then covered with turf with the grassy side down, to prevent the soil mixing with the stones. There are flues or chimneys at each end of the border and centre communicating with the drains in the bottom, as shown in section marked 2. The top of these flues is nicely made of stone ten inches square, through which is cut a hole of six inches square, into which is inserted a plug of a wedge-like form, so as to fit tightly, but removeable at pleasure ; these flues are about an inch above ground. At the back of the border are placed cast-iron pipes (marked 5), perpendicularly, and also oommimicating Ui CONCRETma VINE BORDERS. •with, the drains underneath; those being higher than the flues in front cause a motion in the air beneath the border. After a long continuance of rain the plugs in the flues in front are taken out, thereby creating a great circulation of air, and thus to a vast extent accelerating the proper dr3dng of the borders, -which is deemed of much importance. In the winter season the borders are covered with leaves and stable manure to the depth of twelve inches. It is obvious that the whole aim of the con- structor of this border was to do that which experience shows to be so important. He not only got rid of superfluous water, but he introduced air in abundance, and at the same time the natural warmth which it carries with it. The result was Black Hamburgh Grapes, weighing from two pounds nine ounces up to Jive pounds a hunch — beautiful fruit of admirable quality, on Vines just seven years old. The experiments with coKCKBiiua Vine bobbee, were all made with the same end in view, namely, the elevation of the temperature of the soil in which Vine roots are formed. By keeping them near the surface, they derive much more advantage from the sun than if they penetrated deeply into the ground, which a concrete bottom renders impossible. Mr. Fleming, the experienced gardener at Trentham Hall, in Staffordshire, found it impossible to obtain good Grapes in that cold soil until the plan of concreting was employed. As soon as the bottom of his border was artificially rendered impenetrable by the Vine roots, all difficulty disappeared. In illustration of the effect of the system he mentions in the Gardener's Chronicle for 1850, p. 723, the following circumstance. In one of the houses which had been planted eight years, the black Grapes ceased to colour well ; and as the border was well made, and rested upon well prepared concrete, having a declivity to throw off the wet quickly, he was much disappointed. IJpon opening the ground in front of the border, the cause of the Grapes not colouring was immediately discovered ; the roots had got into the drain, and across it into the subsoil beyond the concrete. Mr. Spencer, of Bowood, one of the most experienced and perfectly well informed of aU our great English gardeners, has carried out the plan of concreting in a different manner, of which he has given an account,* which contains so much practical wisdom that it is here republished with little curtailment. "On many descriptions of soils, the Viae grows with great vigour, and wiU bear large crops of fruit, Mth but little or no assistance in the way of manure — such appears to be the case with the one at Cumber- land Lodge,t the Hampton Court Vine, and others in various places. * See Oardmer's Chronicle for 1850, p. 772. t Tte following is the history of the great Vine at Cumberland Lodge, in Windsor Park, which is aUuded to by Mr. Spencer. It was planted about fifty years ago, in common light garden soil resting upon a bed of hard gravel and clay. In 1860 it produced BEST SOIL FOR VINES. 145 The two Vines in question both grow on shallow rich soils, the one at Cumberland Lodge being a light sandy loam resting on the gravel and clay of the London basin, while at Hampton Court it is a finely divided alluvial soil resting on gravel, the subsoil in both cases being dry and compactr Such being the case, it matters little what the material con- sists of, for a clay bottom may be equally good with a gravel one if drained naturally by fissures, or other causes. In such situations the Vine finds all the elements it requires for its growth. The fertilising particles of matter are equally distributed through the soil. There is no disposition in any portion of such soils to run together, or to become sour ; every facility is afibrded the roota to permeate the earth, while the finely divided state of the various ingredients composing them (and their perfect admixture) favours the production of those minute fibrous roots (never found on strong heavy soils) which are so essential an element of success in Grape growing. Here, then, is all the Vine requires to produce good and abundant crops, and to form for itself a constitution enabling it to supply generations with its generous produce. I am not aware of any pecxdiarity in the loams resting on the London clay (such are, however, much the best for all descriptions of potting) except it be in the finely divided state of the parts composing them; and the presence of rich calcareous matter ; but I have seen the Vines growing on similar soils in Hampshire with much freedom, and ripening out of doors fruit in good perfection. Again, on the southern slopes of the hills near Bath the Vine grows vigorously in the natural soU, though the oolite rocks on which the surface soU rests is much colder than either a gravelly or a well-drained clay one. Many of these soils are rich in potash, from being more or less mixed with portions of the fiUler's-eaith beds. The best natural soils for the Vine are those formed by the decomposition of voleanid rooks, such being invariably of a dry, porous quality, and are rich in inorganic matter. Such being the nature of the soils on which the Vine thrives in the greatest perfection, it would be supposed that in the formation of borders expressly for its growth, some approximation would be made towards them by making the borders for the most part, if not all, of the same constituents ; or in other words, forming " a warm, light, dry, shallow soil." In place of this, however, much labour and expense have been incurred in making borders, in which the Vine refuses to thrive at all. .What I may term artificial Vine borders are generally composed of various ingredients, of which loam, dung, and some dry material, as brickbats, mortar, rubbish, &c., may be considered as the principal. To these some add carrion, or other similar substances. Now we will suppose these materials to be two thcusand terge bimclies of magnificent Gfrapes, filled a house one Enndred and thirty-eight feet long and sixteen feet wide, and had a stem two feet nine inches in circumference. The border in which it grows is wctrm, light, dry, &ti& shaXUm. L 146 SPENCER'S OPINION AS TO the best of their kind, that they have been properly mixed and pre- pared, and that the border has been made, and the Vines planted, in the usual way. There can be no question but that (if other things are favourable), on a border of this description, the Vine wiU grow vigorously, and mature fine crops of Grapes. But let us wait some eight or ten years, when the fibre of the loam is rotted, and its elasticity destroyed, by which time the dung has become a sour pasty mass ; while the rain during that period wiU have washed down the more soluble parts, and will have partially, if not totally, stopped the natural drainage. If at the same time the loam has been somewhat of a heavy texture, the evil wiU. be increased. In fact, it will be foimd, on exami- nation, that what was, for the first few years, a rich porous border, has become, through causes perfectly natural, unsuited for the growth of the Vine. " I consider that when healthy and permanent Vines are wished for, more loam, and that of a sandy nature, should enter into the composi- tion of Vine borders, and that a large portion of the following should be intimately incorporated with it, viz., charcoal dust, charred matter, wood ashes, and soot. What manure is used should be perfectly rotten, and as dry as can be procured, and that road scrapings, or (what is better) the sweepings of large towns, well rotted, and mixed with the above, will be found one of the best materials for a sound healthy border. "In preference to concreting the bottom, I would recommend the border to rest on any description of rough paving stones, raised on rough walls, one foot or more, according to the situation, thus forming a series of air drains under the border, the outlet to which may either be in the house, or in some place enabling you to connect them with the external air. With a bottom of this description I would then certainly concrete the surface. I use gravel, lime, and coal ashes made into mortar, and spread two inches thick ; in addition, when the above is dry, it gets a coat of gas tar over the sur- face ; this forms a compact substance, treading firm underfoot, and efiectuaUy throwing ofi' rain ; common 3-inoh draining pipes are placed upright in the border previously, which stand one inch above the surface when the concrete is laid on. When it is necessary to water the border, it can be done to any extent by pouring water down the pipes. In winter, all agree the drier the border the better ; and plugs are then placeci in them. It will, however, be found that less water will be required than might be expected, arising from the obstruction to free evaporation by the concrete. In a small Vinery, planted in August, 1848, the border of which was concreted after planting, I have only watered the outside border once (the inside border being only two feet wide), and yet the Vines have never shown the least indications of having required more, irrespective of the advantage of having in our THE BEST SOIL FOK VINE BORDERS. 14? climate the roots of the Vine under control as respects moisture. Another point gained by concreting is the additional heat the border gains by the absorption of solar heat. I have proved frequently that a border, concreted as I have described, obtains an increase, at twelve inches deep, of from twelve to fifteen degrees, and even more during hot sunshine. This increase of heat on the surface of the border -will have the efieet of causing that part of the border to be the dampest, as it will be the warmest ; the roots accordingly will be more numerous immediately under the concrete, and precisely in that position most favourable for their healthy development. An additional advantage of the concrete is its preventing the border becoming compact, from , walking over it, and consequently its porosity is preserved. I say nothing of the disadvantage ascribed to it, from its supposed prevention of atmospheric air to the border, because I believe the thing impossible ; and on the principles described above, air has access at all times under- neath the border, if it is required, which I believe it is not. It certainly looks somewhat unsightly during summer, but a few pots of flowering plants set on it during summer, and a slight coat of Fern or thatch during winter will do away with its formal appearance.'' This plan of concreting the surface is, as wiU have been seen, intended to increase the temperature of the Vine border. In order to secure all the advantages of the method without any disadvantages, it seems essential that the border should rest upon rough materials, so put together that air can readily find its way upward through them into the border. Mr. Spencer's border rests on rough paving-stones raised on rough walls, and is then connected with the external air or with that of the Vinery itself. Under such circumstances, air will find its way to the roots more readily than by any other known method ; and thus the conditions demanded in a perfect Vine border, viz., warmth, dryness in winter, and damp in summer, vrith permeabUity at all seasons, are perfectly fulfilled. That the raising the border on a vaulted bottom is of very great value, concrete or no concrete, is admitted by the best Gfrape growers. Mr. Hutchinson's borders at Castle Malgwyn are so managed ; and the early houses at Trentham, built under Mr. Fleming's direction, have borders of the same kind. We would not, however, be understood to say that these contrivances are at alL times necessary. On the contrary, when soil and situation are naturally suitable to the Vine, very fine Grapes are obtained without any such aids. The important point is, how to deal with this valuable fruit-tree when, as so often happens in Great Britain, the soil and situation are unfavourable ; and that can be only accomplished by securing a sufficient amount of bottom heat, Mr. Reid, of Balcarras, has shown that one of the causes of canker and immature fruit, even in orchards, is the coldness of L 2 148 NECESSITY OF BOTTOM HEAT. the soil. He found that, in a cantered orchard, the roots of the trees had entered the earth to the depth of three feet; and he also ascertained that, during the summer months, the average heat of the soil, at six inches below the surface, was 61°; at nine inches, 57°; at 18 inches, 50°; and at three feet, 44°. He took measures to confine the roots to the soil near the surface, and the consequence was, the disap- pearance of canker, and ripeniag of the fruit. (Memoirs of Caledonian Hort. Soc, vi., part 3 ; and Gardener's Magazine, vii. 56.) The same fact has been observed in many other instances. If, on the other hand, we take cases of growth in the artificial climate of hot-houses, we find that Bignonia venusta, and many- other tropical plants, will not flower, unless in a high bottom heat ; and that Palm-trees, planted in the soil of conservatories which it is impracticable to heat sufficiently, soon become unhealthy. The reason why it is necessary to plants in a growing state, that the mean temperature of the earth should be higher than that of the air, is sufficiently obvious. Warmth acts as a stimulus to the vital forces, and its operation is in proportion to its amount, within certain limits. If, then, the branches and leaves of a plant are stimulated by warmth to a greater degree than the roots, they will consume the sap of the stem faster than the roots can renew it ; and, therefore, nature takes care to provide against this by giving to the roots a medium perma- nently more stimulating, that is, warmer, than to the branches and leaves. We regard warmth not merely as a stimulus of vegetation; it is extremely necessary for tlie solution of various substances witk wMcli tlie water comes in contact. It also seta free certain gases which the leaves take up, and through these sources of nourishment promotes the growth of plants. — Oerman Hd. Such being the fact, it is obvious that one of the first of a gardener's cares should be, to secure the means of insuring a proper -temperature to the soil in which he grows his plants, and that this is Requisite for hardy as well as tender species. CHERRIES AND LETTUCES, HOW FORCED. 149 I entertain little doubt that the time is at hand when it will he considered quite as necessary to furnish heat for the soil as- for the air; not, however, heat without moisture, for that would evidently produce much greater evils than it was intended to cure, as has indeed been found by inconsiderate experimenters. Mr. Writgen is probably right in believing that it is the temperature and moisture of a soil quite as much as its mineralogical quality, that determine its influence upon vegeta- tion. (See Erster Jahresbericht, dc, am Mittel und Nieder- Bhein,. p. 64.) It must not, however, be supposed that the nature, whether chemical or physical, of soil is unimportant. A crop of wheat cannot be had on peat, nor will salt plants thrive when the soil contains no marine salt. Mr. Fintelinann, the king of Prussia's gardener at Potsdam, is celebrated for his success in the difficult art of forcing Cherries, and he has given an account of his practice {Gard. Mag., vol. iii., p. 64), in which it appears that the most pecuKar feature is the strict attention he pays to the temperature of the roots. He first soaks the roots in water heated by the mixture of equal parts of boiling and cold water ; he afterwards sprinkles the trees with luke-warm water, and he continues to employ it of the same temperature as long as watering is required. Thus his roots are constantly maintained at the requisite temperature by the trickling of the warm water into the soil. It seems, indeed, clear, that the success of the Dutch in obtaining an abundance of fresh vegeta]j)les, such as Lettuces, during the whole winter, is in part owing to their being able to maintain a gentle bottom heat. No doubt this is connected with the abundant light which their forcing structures admit, and with other causes of considerable importance, such as an abundant, constant, and skilful introduction of fresh air; but none of those causes can be supposed likely, in the absence of the bottom heat, to produce such a result as the Dutch gardeners obtain. If it is necessary that the temperature of the soil in which plants grow should be carefully regulated, and adjusted to their natural habits, it is no less requisite that the water in which 150 WATER FOR AQUATICS MUST BE WARMED. aquatics are cultivated should be also brought to a fitting heat. Mr. William Kent succeeded well in making many tropical species flower, by growing them in lead cisterns plunged in a tan-bed {Hort. Trans., iii. 34) in a close heat. In like manner, Mr. Christie Duff procured flowers in abundance from Nymphsea rubra, cserulea, and odorata, by placing them in a cistern in a pine stove upon the end flues, where the fire enters and escapes ; or by plunging them into tan-beds in pine-houses, varying in temperature from 80° to 100°. {Hort. Trans., vii. 386.) Very lately, Mr. Sylvester, of Chorley, in Lancashire, obtained fine flowers from Nelumbium luteum, by paying attention to the temperature of the water. When he kept the latter at 85°, the plants grew vigorously, and were in perfect health, but flowerless ; but by lowering it to 70° — 75°, which more nearly approaches the heat to which the plant is naturally accustomed, the mag- nificent blossoms were produced and succeeded by seeds ; the red Nelumbium, however, which inhabits countries with a greater summer heat than the yellow, at the same time suffered by this lowering of temperature, none of its blossom buds having been able to unfold. {Bot. Mag., xiii., n. s. t. 3753.) The water of rice fields, in which the red Nelumbium flourishes, was seen by Meyen at 113° at Lantao, in China. The Victoria Lily affords another instance. It will grow while its roots are in a temperature wholly insufficient to enable it to ilower. And another water plant, the Aponogeton distachyum, iiowers abun- dantly even in winter wherever the temperature of the pond in which it grows rises sufficiently. Well-regulated bottom heat being thus shown to be of such immense importance in gardening, it is surprising that more attention should not be paid to economising the waste water of steam engines where factories are conveniently situated. "What may be done, without cost, by atten- tion to this, is shown by the following experiment tried by Mr. DOlwyn Llewellyn, of Penllergare. From a small eight-inch cylinder engine, employed by him for agricultural purposes, this gentleman conducted a jet of steam for twenty minutes daily, through an inch iron pipe, into a bed of rough stones, covered by a glazed frame. A journal of the tem- perature was kept for eleven days, with the following result : — APPLICATION OF WASTE STEAM. 151 glATBMEHT Ot EXPERIMENT WITH WaSTB StHAM, AS A MEDIUM OF BoiIOM HeAT, MADE AT PbNLLEKOABE, 1850. Date. Time of Observation. Tliermo- meter. April. 9 . 12 Noon . Degrees. 51 Steam introduced about 12 o'clock. )) 5 P.M. . . 54 )> 7 V.M. , . 56 10 . 12 Noon . 68 Steam introduced. u 3 P.M. . . 73 ■)> 5 P.M. . . 85 J) 7 P.M. . . 96 11 . 7 a.m.. . 108 Steam not introduced. )) 12 Noon . 104 tt 5 P.M. . . 98 12 . 10 A.M. . . 83 Steam not introduced. )> 7 P.M. . . 79 13 . 10 A.M. . . 69 Steam introduced. )) 6 P.M. . . 75 14 . 10 A.M. . . 82 Steam not put on. )) 7 P.M. . . 79 15 . 10 A.M. . . 70 Steam introduced. J) 6 P.M. . . 73 16 . 10 A.M. . . 81 Steam introduced. 17 , 10 A.M. . . 76' Steam introduced. )» 4 P.M. . . 79 18 . 10 A.M. . . 94 Steam introduced. i) 5 P.M. . . 110 19 . 10 A.M. . . 108 Steam not introduced. » 6 P.M. . 96 From this it appears, 1st, that although steam was introduced among the stones for only twenty minutes a day, the temperature was raised from 51° to 68° in the first twenty-four hours ; 2nd, that the tempera- ture continued to rise for many hours after the second application of steam, until the thermometer reached 108° ; 3rd, that at the end of nineteen hours the heat of the 'frame diminished; yet 4th, that at the end of seventy hours the temperature still was 69°, This appears a conclusive answer to those who think that masses of heated water, or heated porous materials, like, rough stones, will become so reduced in temperature by a few hours' withdrawal of the prime heating power as to endanger the plants cultivated in houses thus warmed. The experi- ment continued to be successful, and enabled Pine-apples of the most perfect quality to ripen. 152 DOUBTS ABOUT BOTTOM HEAT. An opinion has, nevertheless, been entertained, that bottom heat is useless; there is in the Horticultural Transactions, (vol. iii. 288) a paper to show that it is injurious; and the authority of Mr. Knight has been referred to in support of the opinion, in consequence of that great horticulturist having expressed a belief that the " bark-bed is worse than useless." {Hort. Trans., iv. 73.) But Mr. Knight repeatedly disavowed entertaining any such sentiments. In one place, he stated that the temperature of the air of the stoves in which his Pine-apple and other stove plants grew, without ba/rk or other hot-bed, usually varied from 70° to 85° ; and that the mould in his pots, being surrounded by such air, acquired and retained, as it necessarily must, very near the same aggregate temperature, but subject to less extensive variation {Gard. Mag. , v. S65):m another, he says the temperature of the air was varied in his stove generally from about 70° to 85° of Fahrenheit; and he ascertained, by keeping a thermometer immersed in the mould of the pots, that the temperature of the soil varied very considerably less than that of the air of the stove ; the mould being in the morning generally some degrees warmer than the air of the house, and in the middle of the day, and early part of the evening, some degrees cooler. ( Hort. Trans., vii. 255.) It is, therefore, clear that he considered a high temperature necessary for the roots of his Pine-apple plants ; and we find from one of his papers {Hort. Trans., iv. 544), that he considered it better to obtain the requisite temperature from the atmosphere than from a bark-bed, the usual source of bottom heat, " because its temperature is constantly subject to excess and defect;" and he even admitted that if the bark-bed could be made to give a steady temperature of about 10° below that of the day temperature of the air in the stove. Pine plants would thrive better in a compost of that temperature than in a colder. The dispute about bottom heat was not as to the necessity of it, but as to the manner of obtaining it, which, as it concerns the art of gardening, I need not further notice. We have, doubtless, much to learn as to the proper manner of applying bottom heat to plants, and as to the amount they will bear under particular circumstances. It is, in particular, EXTREME CLIMATES. 153 probable ihat in hot-houses plants will not bear the same quantity of bottom heat as they receive in nature, because we cannot give them the same amount of light and atmospheric warmth ; and it is necessary that we should ascertain experi- mentally whether it is not a certain proportion between the heat of the air and earth that we must secure, rather than any absolute amount of bottom heat. It may also be, indeed it no doubt is, requisite to apply a very high degree of heat to some kinds of plants at particular seasons, although a very much lower amount is suitable afterwards ; a remark that is chiefly applicable to the natives of what are called extreme chmates, that is to say, where a very high summer temperature is followed by a very low winter tempera- ture. Such countries are Persia, and many parts of the United States, where the summers are excessively hot, and the wiater's cold intense. The seeming impossibility of imitating such conditions artificially will probably account for many of the difficulties we experience ia bringing certain fruits, the Newtown Pippin, the Cherry, the Grape, the Peach, and the Almond, to the perfection they acquire in other countries. The great point to attend to in these considerations is the extremes of temperature to which plants are subject when growing; for this reason the calculations of M. Boussingault have less value than might have been anticipated. This disr tinguished French writer upon rural economy proposed, some years ago, a method of determining what amount of heat a plant requires, ia order to be enabled to perform the functions allotted to it by Nature. This method consisted in determining the length of time over which a function extends, and also the mean temperature during that period. Thus, if a given plant requires 20 days to ripen its seeds after flowering, and the mean temperature during that time was 10°, it would be assumed that the plant in question requires 200° of heat to complete the ripening process. Or if the period occupied was 10 days, and the mean heat 10°, then only 100° of heat would be required, and so on. M. Boussiagault's method was a great improvement upon the previous modes of computation. Observers had been previously contented with annual or quarterly, or other long 15i INUTILITY OF MEAN AIK TEMPERATURES. means of temperature, as furnishing the elements required to determine whether a given plant could be adTantageously cultivated in a given country. But these means were aU more or less fallacious, and might have led to serious mistakes. Mean temperatures are useless to cultivators unless they repre- sent what takes place during the period of vegetation. We do not want to know what the temperature is of seasons when, or of places where, plants do not grow, unless for the purpose of determining the amount of winter protection which they may require; and all indications of climate in which the dormant season is mixed with the growing season only mislead. Suppose, for example, it was to be said that the mean annual tempera- tures of Longville and Bretville are the same (say 35°), this would be no proof of similarity of climate, for Longville might have the winter mean 30°, the summer mean 50°; while Bretville might have the winter mean 30°, and the summer mean 40° — cold winters and temperate summers characterisiag one place, mild winters and bad summers characterising the other. Nor are daily means much more useful. Let us suppose that Longville has in June a daily mean of 45°, while that of BretviUe is 50° ; it might be that these means represented hot days and cold nights in the one case, and cool days and mUd nights in the other — conditions which for the purposes of cultivation are whoUy different. That M. Boussiugault's method of explaining the relation between plants and climate was an important improvement upon the usual indications is not to be denied. But it was not wholly satisfactory. Pushed to its limits the theory was manifestly untenable, for it amounted to this — that if a plant requires 30 days with 10° of heat in each day, or 300° to do a certain thing, and if it can do the same thing in 10 days, with 80° of heat in each day, then it ought to accomplish the same end in one day by the aid of 800° of heat, which is absurd. In all considerations relating to ground temperature, the gardener should inform himself more especially upon three points : — 1, the temperature of the soil when plants are at rest; 8, that when they are in vigorous growth ; and 3, that when they are ripening their fruit. The first points out the bottom NATURAL GROUND TEMPERATURES. 155 heat to be maintained in winter, the second in summer, the third in autumn. Information upon this question can be had by consultiag the tables of temperature published in the Journal of the Horticultwal Society, vol. iv., and comparing them with the remarks at the pages following p. 1 13 of this work. In what way such evidence is to be practically employed will be seen m the succeeding table, calculated by Mr. E. Thompson, with a view to explaining what the natural temperature is to which certain plants commonly cultivated are exposed in the climates best adapted to their healthy development. I. — A Table of Ground Tempebatttrbs natceal to Certaiit Plants, as either AOIUALLY OBSERVED, OR OALOULATED FROM KNOWN AlR TeMPEEATBRE. Name. = Most . Suitable Climate. Season of Growth. Season of Eipening. Season of Best, Apple, Pear, &c. Peach and Nectarine Apricot .... Cherry Gooseberry,' &c. . . Q,mnce Tine, Muscats . . ,, Sweetwaters . Fig Melon Plantain, or Banana Pine-apple . . . Mango Vanilla . . . . Orange . . . . Mangosteen . . . Loquat . . . . Litchi Oats Barley Wheat Maize nice North of Prance Persia Armenia . Asia Minor Lancashire Portugal Sicily . . Paris . . Smyrna . Smyrna . Jamaica . Suriilam . Bengal . Surinam . Malta . . Malacca; . Japan . . Canton . Scotland . England . Castile Virginia . Bengal . 59 65 67 56 54- 62 66 58 60 60 82 82 85 82 60 84 70 74 51 54 61 70 89 64 78 72 68 61 70 80 66 80 80 88 88 89 88 77 86 80 86 67 62 78 79 92 41 55 27 43 44 55 65 41 46 80 81 83 81 66 81 49 59 41 42 46 156 NATURAL GEOUND TEMPBRATUEES. ir. — A TabIE of the ASOERTAIIfED, OK ESTIMATED AvEKASE ©KOtJSD TEMPERATnKESl IK BIPFEKBHT PARTS OF THE WOKLD. Country. Season of Growtli. Ripening. Best. LoNDoir (CHswiok) Africa, South (Cape of Good Hope) , ,, ,, (Gfraf Reynet) , . . Algiers ,, (Constantiae) AmBterdam. Armenia (ErzeroTim) Astraohan Australia (Coburg Peninsula) . , ,, (Port Jackson) . . . . ,, "Western (Perth.) . . . Ava Azores (St. Michael's) Batavia Berlin Berne Beyrout .... Bogota Bombay .... Brussels .... Bucharest .... Cairo Calcutta .... Canada (Toronto) . Canton ..... Caraocas (Maraoaybo) Ceylon (BaduUa) . „ (Candy) . . Constantinople . . Dantzic .... Dublin Edinburgh . . . Falkland Islands Morenoe .... Fort Vancouver . . 55 62 65 66 66 57 57 56 83 67 67 79 65 82 84 59 49 65 64 84 59 58 70 82 58 74 87 73 75 64 54 56 61 49 64 54 62 67 74 76 82 64 72 74 85 75 81 88 68 83 91 64 59 '79 64 87 65 65 87 90 66 84 89 76 78 73 64 60 57 56 76 65 42 68 68 57 49 40 27 23 80 88 69 68 60 80 67 36 33 69 62 82 41 30 62 75 30 67 86 71 74 44 30 44 41 42 44 41 NATUEAL GROUND TEMPERATURES. 157 Table of Avekahe Gkound Tbmperatukes — confirmed. Country. Season of Growth. Bipening. Best, Geneva Genoa Guatemala ..... Guinea Havamiab. Himalayas (Khasia) . . Hotart Town Honolulu ...... Hlinois (St. Louis) . . . Jamaica (Kingston) , . . Java (Bnitenzorg) . . . Jerusalem lima Lisbon Liverpool ■ Macao Madeira (Funehal) . . . Madras Madrid Manilla Melbourne Mexico . MontpeUier Montreal Moscow Munich Naples New Orleans Kew York , Kew Zealand (AucHand) , Nova Scotia (HaJifas) . , Niger Ootacamund . . . . , Oran Oregon (Columbia) . . . Palermo Paris .,,..., Penzance 58 65 70 86 80 78 53 77 65 82 80 65 75, 64 .54 .72 .65 ,85 61 78. 60 64 65 65 57 59 64 76 64 59 50 88 63 66 65 66 58 56 70 76 72 87 83 85 6? 80 .77 , 88 81 76 , 82 71 62 85 74 88 78 90 65 67 74 72 65 64 76 84 72 66 69 91 66 75 75 80 66 63 33 51 70 84 77 64 44 74 34 80 79 52 70 56 44 60 67 83 46 74 51 58 46 25 24 33 50 56 36 53 26 84 56 53 41 55 41 47 158 NATURAL GEOUND TEMPERATURES. Tabie of Ayerage Gkocnd Temperatures — continued. Country. Persia (Bushire) . . Persia (Mosul) . . , Polynesia (Eaiatea) . . Quebec Quito Rio Janeiro . . . . Rome St. Petersburg . . . Sebastopol Shanghae Sincapore Surinam (Paramaribo) , Teflis Trebizond Trincomalee . . . . Virginia (Norfolk) . . Vera Cruz Venice Vienna "Washington . . . . Season of Growtli. Eipening. Best. 79 90 64 65 93 48 81 84 79 58 64 77 71 66 84 20 63 74 64 45 76 60 49 25 60 73 84 82 70 80? 85 88 39 49 83 81 65 63 84 77 75 88 37 50 80 68 80 48 81 60 63 60 86 ■74 69 77 74 40 34 34 The temperature here estimated as that of the season of rest is to' be understood as what roots are probably exposed to at a foot below the surface. Of course, upon the surface, the temperature would be lower. CHAPTER II. OF THE MOISTURE OF THE SOIL.— WATERING. It has already been shown that water is one of the most important ingredients in the food of plants, partly from their having the power of decomposing it, and partly because it is the vehicle through which the soluble matters found in the earth are conveyed into the general system of vegetation. Its importance depends, however, essentially upon its quantity. We know, on the one hand, that plants will not live in soil which, without being chemically dry, contains so little moisture as to appear dry ; and, on the other hand, an excessive quantity of moisture is, in many cases, equally prejudicial. The great points to determine are, the amount which is most congenial to a given species under given circumstances, and the periods of growth when water should be applied or withheld. When a plant is at rest, that is to say, in the winter of northern countries and the dry season of the tropics, but a small supply of water is required by the soil, because at that time the stems lose but little by perspiration, and consequently the roots demand but little food; nevertheless, some terrestrial moisture is required by plants with perennial stems, even in their season of rest, because it is necessary that their system should, at that time, be replenished with food against the renewal of active vegetation. Hence, when trees are taken out of the earth in autumn, and allowed to remain exposed to a dry air all the winter, they either perish, or are greatly enfeebled. If, on the other hand, the soil in which they stand is filled with moisture, their system is distended with aqueous matter at a time when it cannot be decomposed or thrown off, and the plant either 160 EFFECTS OF EXCESSIVE WINTER-WET. loses its roots by rotting, or becomes unnaturally susceptible of the influence of cold in rigorous climates, or is driven prema- turely iato growth, when its new parts perish from the unfavourable state of the air in which they are then developed. The most suitable condition of the soil, at the period of vegetable rest, seems to be that ia which no more aqueous matter is contained than results from the capillary attraction of the earthy particles. During the season of 1852 and 1853, in wMcli rain fell, witli little inter- mission, from November till March., and inxmdated permanently gardens in low situations, Ehododendrons, although fond of moisture, perished to a great extent. During winter they seemed to be healthy, but when spring arrived their leaves became dull, changed to brown, and withered, and the buds refused to push ; or, when attempts were made by planta to renew their vegetation, their growth was feeble, and most of them died in the course of the following autumn or winter. Nevertheless, there are exceptions to this, in the case of aquatic and marsh plants, whose peculiar constitution enables them to bear with impunity, during their winter, an immersion in water ; and in that of many kinds of bulbs, which, during their season of rest, are exposed to excessive heat and dryness. The latter plants are, however, constructed in a peculiar manner; their roots are annual, and perish at the same time as the leaves, when all the absorbent organs being lost, the bulb cannot be supposed to require any supply of moisture, inasmuch as it possesses no means of taking it up, even if it existed in the soil. The conditions under which true ac[uatics exist have been so well explained by a philosophical writer, in the ~ Gardener's Chronicle, 1852, p. 19, that I quote his statement without curtailment, although his remarks, in part, refer to other questions besides the moisture of ^e medium in which roots are placed :^— Plants growing entirely under water are to some extent protected from those great and sudden changes of temperature to which ordinary land plants are frequently exposed ; at the same time, however, water plants are very often injured by cold, and it not unfreqiiently happens, that on a cold winter's night plants in a pond will be greatly injured, or even killed, whilst those in a neighbouring pond will remain quite uninjured. In order to understand the precise cause, of this pheno- menon, we must examine the conditions under which plants grow, and the peculiar sources of injury to which they are "consequently exposed. EVAPORATION— CONDUCTION. 16t ^er'e are ttree perfectly distinct modes in wLich. tlie surface Of tW earth becomes cooled, and these are by evaporation, by conductionj and by radiation. When water evaporates it becomes colder, because, in the formation of vapour, heat is always absorbed. This simple fact is of the greatest importance to the Hfe of both plants and animals* When plants are exposed to a hot sunshine, the moisture which they contain gradually evaporates, and in so doing absorbs the great heat of the sun's rays, which would otherwise injure plants and bum them up. Evaporation from the surface of the leaves is generally in proportion to the direct heat of the sun, and it is necessary as a means of keeping the plant cool, and preventing it from being scorched ; if soil is dry, so that the plant cannot obtain, by means of its roots, a constant supply of moisture to keep up this daily evaporation from its leaves, it has no power of withstanding the heat of the sun, and it withers and fades the first hot day. Whenever, and ia whatever manner, we check the constant evaporation which always goes on in the leaves of a healthy plant, we run a risk of killing it by exposure to hot sunshine. The common experience of the gardener gives plenty of examples of the truth of this; but there are other eases in which, though the same effect is produced, and the same principle is involved, its influence is not so self-evident. When, for example, a plant is placed in a close hothouse, confined in a hot damp air, its perspiration is cheeked, because the air being already saturated with moisture, it has little power of carrying off the moisture evaporated by the leaves, and consequently the plant has less power of withstanding the heating influence of the sun's rays than it has in the open air, or in a state of nature. As evaporation, on the oiie hand, is a natural means of counteracting the excessive heat of the sun, so, on the other hand, it is the chief cooling agent in nature, and every ciroumstance tending to increase evaporation from the surface of the soil tends also to cool it. As a moist air and a diminished circulation are most unfavourable to evapora- tion, so a dry air and free circulation grea/tly facilitate it.. The cooling effect of a cold dry wind is familiar to every one ; its iofluenee depends on the fact, that dry air readily absorbs moisture from any surface exposed to it, whilst the rapid motion of the wind, by carrying away the moisture as fast as it is formed, insures a constant supply of fresh, dry air, and thus, by aiding in the formation of moisture, rapidly cools the surface on which it blows. The second mode in which plants are cooled is by conduction, or by the mere contact of cold air ; and this is quite independent of the cold produced by evaporation. When a cold wind drives along the surface of the ground it gradually cools it, and, of course, likewise the plants growing on it, by the simple abstraction, or carrying away of heat. S» long as the surrounding air is colder than the plants it wiU tend to reduce their temperature ; and if the air is in motion, as fresh portions 162 RADIATION. of cold air will continually come in contact with, tie plants, they inust gradually get colder and colder, even though no evaporation takes place, till they are as cold as the air itself. Radiation, the .third mode in which plants are influenced by cold, depends upon the curious fact, that when two substances are placed opposite to each other in the free and open air, if the one is warmer than the other, it will immediately begin to give out its heat, which will be received by the colder substance. The diflPerenee between this mode of cooling and mere conduction is, that in the latter heat travels from the hot to the colder surface by contact, and therefore only when they absolutely touch each other, whilst in radiation, the two surfaces are at a distance, and the heat passes at once through the air, and without in any way warming it. The heat of the sun is radiant heat — it passes through the clear air without communicating any warnith to it, though it warms the earth below ; and then when the sun's rays have warmed the earth, the latter in turn begins to warm the surround- ing air — ^but this effect is no longer one of radiation, it is simply an effect of conduction. On a clear night the surface of the ground may be exposed to all three of these cooling influences at once ; it may be cooled by evaporation, by contact with cold air, and by radiation. In reality, however, it is very seldom that all these cooling influences are in operation at the same time, because there are several counteracting powers at work tending to keep the surface of the soil at a tolerably uniform temperature ; and foremost of these is the formation of dew. As the evaporation of water is a cooling process, heat being absorbed, so the condensation of moisture is a warming process, an equal amount of heat being given out ; consequently, just in proportion as the surface of the earth after sunset is cooled by radiation, it will acquire the power of condensing the moisture in the air, and by that very act will gain. heat. It must also be remembered that radiation only takes place in a still and clear night ; when there are clouds or mist, radiation does not occur. • "Water may be cooled either by evaporation, or by the contact of cold air, but it differs from the soil in the fiacility with which it is moved, and the readiness with which currents are formed m it. When the . earth is exposed to cooling inftuences, the surface soon becomes cold, .but as heat travels very slowly through the porous soU, it takes a very long time before,the cold penetrates, or rather before the heat escapes .from any depth below the surface; in the case of water it is quite different, because when the surface is in any way cooled, the water becomes heavier or denser, and a kind of circulation is immediately established, the cold water descending, and the warmer water rising to its surface. In this manner, then, so long as the cooling influences 1 continue, the water goes on sinking in temperature, the whole body of it getting colder ; this, however, does not continue after it has arrived COOLING OP WATER. 163 at a temperature of 40°, or about 8° abote the freezing point ; wlien thia is the case, all circulation in tbe water ceases, because if the surface ■water is then cooled still lower, it no longer continues to contract and become denser, but on the contrary expands, so that it then remains floating on the surface. It follows from this very interesting fact, that when on a cold winter's night the surface of a pond is cooled, the whole body of water sinks in temperature to 40°, after that, the surface only continues to get colder, and a film of ice is soon formed, while the water below continues at a temperature of 40°. In consequence of this kind of circulation, and the facility with which it is produced, a body of water is easily cooled down to within 8° of freezing, but when once it has arrived at that point its further cooluig proceeds very slowly, even though the cold becomes much more intense ; for the water below is in fact protected from contact with the cold air by the film of ice at the surface, and ice is so bad a conductor of heat that the freezing of the water under the ice goes on very slowly ; in temperate climates ice is seldom more than a few inches in thickness, and the water in deep ponds not only never freezes, but, indeed, never falls in temperature much below 40°. Water plants, therefore, axe, in. fact, preserved from cold by the coating of ice which forms over the surface of the pond in which they grow ; if the water is deep they are seldom injured ; but if the water is shallow, and the cold long-continued, the whole depth of it will in time freeze, and the plants will be more or less injured. Plants growing in water thus walled over with ice are protected from all the three cooling influences to which we have alluded ; but there are some circumstances under which water plants suffer greatly, and from a very singular cause, but one which, when looked into, is sufficiently simple and intelligible. The surface of clear water does not become cold from radiation, but from contact with cold and dry air ; consequently in a fine but very still night it is much less rapidly cooled than the earth, which, in addition, is exposed to the cooling influence of radiation. Under such circum- stances it sometimes happens that the usual order of things is reversed,, the bottom of the pond oooUng more rapidly than the surface ; on a clear still cold night radiation sometimes occurs from the bottom of a pond, the plants and soil ia which they are growing radiating towards the sky just as if the water were not above them, and the consequence is that they become very cold, in fact, some degrees below the freezing point, though the water above them is still at 40°. This effect can only happen in clear water, and on a night when there are no clouds, for the same circumstances which prevent radiation from the surface of the ground wiU also prevent its taking place from the bottom of a pond. When plants under water are cooled by radiation, they soon become encased in ice, and though the ice thus formed generally melts the next M 2 Ui SEASON OF GROWTH DEMANDS WATER. morning, yet at the time of its formation the plants are often exposed to a very intense cold. A singular effect, somewhat similar in nature, though caused in a very different manner, is sometimes observed ; as clear still water offers no obstruction to the passage of radiant heat, it occasionally happens that water plants are injured by the great heat of the sun's rays ; like land plants they receive abundance of radiant heat from the sun, but, imlike land plants, they do not experience the compensating effect of evaporation ; they only feel the less perfect cooUng influence of the sur- rounding water. It therefore occasionally happens that plants growing in water, and surrounded by it, are burnt and scorched by the heat of the sun's rays, the radiant heat of which produces no effect on the water through which it passes, any more than it does in passing through the air ; its effects only become evident when its rays fall upon a solid substance, such as the surface of the ground or the leaves of a plant. It is wlien plants are in a state of growth that an abundant supply of moisture is required in the earth. As soon as young leaves sprout forth, perspiration commences and a powerful absorption must take place by the roots ; the younger the leaves are, the more rapid their perspiratory action; their whole epidermis must, at that time, be highly sensible to the stimu- lating power of Hght : but as they grow older their skin hardens, the stomates become the only apertures through which vapour can fly off, and by degrees even these are either choked up, or have a diminished irritability. As a general rule, it is safe to conclude that the ground should be abundantly supplied with moisture when plants first begiajto grow, and that the quantity should be diminished as the organization of a plant becomes completed. There are, however, ' some especial cases which appear to be exceptional, 'm consequence of the unnatural state in which we require plants to be preserved for our own peculiar purposes. It has been remarked by one of the translators of this work that " care should be taken that plants in pots have not too great a quantity of moisture when they first begin to vegetate." Plants should not have too much moisture at any time. The meaning of the caution seems to be that, as plants in bud are less able to assinulate moisture than if in fuU leaf, so the supply of moisture to the former should be in proportion small. But this caution is needless if the cultivator recognises the general axiom that " Plants should nevek hate moee moisiitbe CULTIVATION OF BULBS. 165 THAN THET CAN CONSUME," whether by assimilation; or rejection in the form of perspiration (see p. 65). In the case of bulbs, which may be kept perfectly dry, whUe really at rest, when they are stimulated into growth, moisture must be administered with the greatest caution. "When a bulb has lain dormant in the earth during its natural period, it is ready to spring into renewed life upon the application of warmth and moisture; and it may seem to matter little whether it is suddenly transferred from dryness to moisture, or whether the change takes place gradually; because its powers of life are unimpaired, But in nature no such sudden changes occur : on the contrary, when rain begins to fall, it soaks slowly into the earth ; and when it reaches the bulb, it is still arrested in its action by the numerous dry coats with which this body is invested, and through which it must gradually filter. But when a bulb has been long out of the earth, its yital energies are much diminished, and it cannot bear even that slow supply of moisture which is furnished by wet soil, whose humidity penetrates the bulb coats, and is absorbed by the living tissue. If a weakened bulb is suddenly brought in contact with water, it wUl absorb it, but may be unable to digest it. The water wiU then become stagnant and putrid, and destroy the bulb ; although, could the bulb have digested it, it woxdd have been converted into new elements and have proved a proper aliment. The rule, therefore, to observe with newly-imported bulbs is, to place them where they absorb moisture very slowly. The driest earth is full of water, which can only be driven off by the application of intense heat. A bulb, therefore, should be planted in what is called dry soil, and placed in a shady part of a green-house until it has become plump, and begun to shoot ; if it has begun to shoot when received, still the same treatment should be observed, and the driest soil used to plant it in. It is only when decisive signs of natural growth can be detected that a very little water should be given, while the temperature is at the same time slightly increased ; and no considerable quantity of water should be administered untH the leavfes are an inch or two above ground, and evidently disposed to grow rapidly. If these precautions are taken, no failures are ever likely to occur ; if neglected, no success can be antici- pated. A chest full of bulbs of Calochortus macrocarpus, one of the rarest and finest of all plants, was destroyed in the Garden of the Horticultural Society by an imskUful gardener, who planted them in the wet earth of an open border immediately after their arrival from a fifteen months' voyage. Every bulb would have grown had he under- stood the principles of horticulture. Dutch gardeners perfectly comprehend this, as wiU. be seen from the following practical remarks on the management of Hyacinths, by Mr. Theodore Storm, one of the most experienced Dutch growers of this plant. Moisture being the most destructive agent against which the 166 CULTIVATION OF BULBS. amateur has to' guard, great care should be taken to protect Hyacinths from it, by selecting the most eleyated spot in his garden. If this is surrounded by a shallow trench, a little distance off, it mil be useful ; and the bed should also be raised seven or eight inches above the ground level. It must not be imagined that this precaution is useless because many parts of England are more elevated and lie drier than Holland, an opinion too prevalent among foreign amateurs, which occasions them the loss of many bulbs. In all the treatises that have appeared on the culture of the Hyacinth, this important circumstance has been almost wholly overlooked. The truth is, that the soil which suits the Hyacinth is very light, and disposed to absorb the rain and snow which falls between the months of November and March. The paths around the beds being more close and compact, do not absorb this moisture which lodges upon the beds, and renders them so wet that they absolutely become like mud to the depth of sixteen or twenty inches. The bulbs having by that time formed roots eight or twelve inches in length, their extremities are continually immersed in water, which, from want of a slope to carry it off, causes the roots to putrify, and to communicate a disease to the bulbs, which either totally destroys them, or renders the flowers poor and small. The bulb becomes weak, and when taken up will be found shrivelled and separating into scales. To prevent this there should always be a gentle descent or small trenches around the beds to drain off the wet. The surface of the beds should also be at least seven or eight inches above the path. The vitality of a bulb being thoroughly aroused, and the leaves being in full and healthy action, many of these plants may almost be regarded as aquatics, their leaves being able to consume all the moisture that the roots, even though immersed in water, can absorb. Of this the Hyacinth is a familiar example; Crinums, Pancratiums, Hippeastrums and all such soft-leaved genera are others, as is seen by the case of the Amaryllis Belladonna, which acquires its greatest beauty by the side of ditches in Madeira, where it is dried up at the period of rest, and deluged while in leaf. One of the effects of an excessive supply of moisture is, to keep all the newly formed parts of a plant tender and succulent, and therefore such a constant supply is desirable when the leaves of plants are eaten as in the case of Spinach, Lettuces, and other oleraceous annuals. Another effect is, to render all parts naturally disposed to be succulent much more so than they otherwise would be ; thus we find market-gardeners deluging their Strawberry plants with water while the fruit is swelling, in order to assist ia that, to them, important operation. While, however, ui this case, the size of the fruit is increased RELAJ?ION OP WATER TO SUCCDLBNCB. 16? by a copious supply of water to the earth, its flavour is, in proportion, diminished ; for, in consequence of the rapidity with which the Strawberry ripens, and, perhaps, the obstruction of light by its leaves, the excess of aqueous matter taken into the system cannot be all decomposed, and formed into those products which give flavour to fruit ; but it must necessarily remain in part in an unaltered condition. It is for the reason just given that the quantity of water in the son should be diminished when succulent fruit is ripening; we see this happen in nature, all over the world, and there can be no doubt of its being of great importance. Not only is the quality of such fruit impaired by a wet soil, as has just been shown, but, because of its low, perspiratory power, the fruit win burst from excess of moisture, as occurs to the Plum and Grape in wet seasons. Some fruits are much more subject to this bursting or cracking than others, as is seen in the Stanwiek Fectariiie, the Chasselas musquS grape, &c. In such cases it is clear that the dryness of the soil is of more than ordinary importance. It is also to be observed that bursting may arise from mere skin disease ; as happens with mildewed or rusty grapes, in which, by one cause or other, the power of the skin to distend as the berries fill with fluid is destroyed — ^in the one case by the action of a mUdew-plant, in the other by greasy fingers or currents of cold air, or impurities of the atmosphere caused by bad fumigation, sulphuring, &c. The Melon, although an apparent exception to this rule, is not reaUy so; that fruit acquires its highest excellence in countries where its roots are always immersed in water, as in the floating islands of Cashmere, the irrigated fields of Persia, and the springy river-beds of India. But it is to be remem- bered that the leaves of this plant have an enormous perspira- tory power, arising partly from their large surface, and partly from the thinness and consequent permeability of their tissue, so that they require a greater supply of fluid than most others ; and, in the next place, the heat and bright light of such countries are capable of decomposing and altering the fluids of the fruit with a degree of rapidity and force to which we here have no parallel. In this country the Melon does not succeed 168 EFFECTS OF WET SOIL. if its roots are immersed in water, as I ascertained some year^ ago, in the Garden of the Horticultural Society, by repeated experiments. Melons were planted in earth placed on a tank of water, into which their roots quickly made their way ; they grew in a curvilinear iron hot-house, were trained close under the glass, and were consequently exposed to aU the light and heat that could be obtained. They grew vigorously and pro- duced their fruit, but it was not of such good quality as it would have been had the supply of water to the roots been less copious. In the tropics, if the quantity of rain that falls in a short time is enormous, and plants are forced by it into a rapid and powerful vegetation, they are at the same time acted upon by free currents of warm air and a light and temperature bright and high in proportion, the result of which is the most perfect organization of which the plants are susceptible ; but, if the same quantity of water is given to the same plants at similar periods in this country, a disorganization of their tissue is the result, in consequence of the absence of air, light, and heat in sufficient quantity. The effect of contiuuing to make plants grow in a soil more wet than suits them is well known to be not only a production of leaves and Ul-formed shoots, instead of flowers and fruit, but, if the water is in great excess, of a general yellowness of appearance, owing, as some chemists think, to the destruction, by the water, of a blue matter, which, by its mixture with yellow, forms the ordinary verdure of vegetation. If this con- dition is prolonged, the vegetable tissue enters into a state of decomposition, and death ensues. In some cases the joints of the stem separate, in others the plant rots off at the ground, and all such results are increased iu proportion to the weakness of light, and the lowness of temperature. De CandoHe con. siders that the collection of stagnant water about the neck of plants prevents the free access of the oxygen of the air to the roots ; but the great mischief is undoubtedly produced by the coldness of the soil in which water is allowed to accumU' late. It is also possible that the extrication of earburetted iiydrogen gas is one cause of the injury sustained by plants whose roots are surrounded by stagnant water; .^ut upoa MADDEN ON DEAINAGE, 169 this point Ave want much more satisfactory evidence than we yet possess. Dr. Madden' s views of the effects of drainage may be quoted in con- nection with, this subject (see his prize essay). 1. One great evil pro- duced by an excess -oi water in soil, is the consequent diminution in the quantity of air within it; which air we have proved to be of the greatest consequence, not only in promoting the chemical changes requisite for the preparation of the food of plants, but Kkewise to the roots of the plants themselves ; for Saussure and Sir H. Davy have proved that oxygen and carlaonic acid are absorbed by the roots ; which gases, however, especially the former, can be conveyed to them only by the air. 2. An excess of water injures soil by diminishing its tempe- lature in summer and increasing it in winter — a transposition of nature most hurtful to perennials, because the vigour of a plant in spring depends greatly upon the lowness of temperature to which it has been subjected during winter (within certain limits of course), as the difference of temperature between winter and spring is the exciting cause of the ascent of the sap. 3. The presence of a large quantity of water in soil alters the result of putrefaction, by which some substances are formed which are, in all probabilityj useless to plants, — such, for example, as carburetted hydrogen, — and diminishes the proportion of more useful ingredients, as ulmio acid. 4. An increase in the proportion of fluid in soil has a most powerful effect upon its saline constituents, by which many changes are produced diametrically opposite to those that take place in soil where the vrater is in much less quantity; and in this manner the good effects of many valuable constituents are greatly diminished, as, for instance, the action of carbonate of ammonia upon humus, and of gypSum upon carbonate of ammonia. 5. The directions of the currents which occur in wet soil are entirely altered by drainage; for whereas in undrained soil the currents are altogether from below upwards, being produced by the force of evaporation at the surface, and consequently the spongioles of the plants are supplied with exhausted subsoil water, when land is drained the currents are from the surface to the drains, and the roots are consequently in this manner supplied •with fresh aerated water. Lastly, an excess of water in soil produces a constant dampness of the atmosphere, which we have shown to be injurious to plants in three distinct ways : — ^1. by diminishing evapora- tion, and thus rendering the process of assimilation slower; 2. By diminishing the absorption of the carbonic acid, and thus lessening the atmospheric supply of food ; 3. By creating a tendency in the plant to produce leaves possessing a different structure from those which the same plant produces in dry situations. Thus we have sis distinct methods in which an excess of water in soil has been proved to be greatly injurious to plants. 170 IMPOETANCB OF DBAINAQE. The removal of superfluous water by drainage lias been already shown to be attended by an elevation of earth-tempe- rature (see p. 137). Its other efi'ects, of taking out of land the water which plants cannot assimilate (and no more), and at the same time of enabling rain water charged with salts of ammonia, a direct food of plants, to reach the roots with every shower, probably constitute the whole rationale of this important operation. In bibulous soils lying high this contrivance may be unne- cessary ; but in those which are tenacious, or which, from their low situation, do not permit superfluous water to filter away freely, such a precaution is indispensable. No person has ever seen good crops produced by trees growing in lands imperfectly drained; and aU experienced gardeners must be acquainted with cases where wet unproductive borders have been rendered fruitful by contrivances which are chiefly valuable because of their efficiency iu regulating the humidity of the soil. Such preoautiona as are detailed in the foUowing good accotuit of preparing a Vine border, stow how important it is to provide effectually for the removal of superfluous water from roots, and how useless a waste of money is that which is expended in forming deep rich beds of earth. " In preparing a Vine border," says Mr. Griffin of "WoodhaU, a success- ful grower of Grrapes, "one foot in depth of the mould from the surface is cleared out from the whole space ; a main drain is then sunk parallel to the house, at the extremity of the border, one foot lower than the bottom of the border ; into this smaller drains are carried diago,naUy from the house across the border. The drains are filled with stone. The cross drains keep the whole bottom ciuite dry ; but if the subsoil be gravel, chalk, or stone, they will not be necessary. The drainage being complete, the whole bottom is covered with brick, stone, or lime rubbish, about six inches thick, and on this is laid the compost for the Vines." {Hort, Trans., iv. 100.) This is in accordance with a practice well known in vineyard countries. "In France, in the Vine districts, where water frequently collects in great quantities at a certain depth in the earth, the trees are planted upon an under-layer of stones, which are covered with earth, and in this manner the roots are kept from too much moisture, and the water is drained away.'' {German Translator.) The practice of placing large quantities of potsherds or broken tiles at the bottom of tubs, or pots, or other vessels in which plants are rooted, is only another exemplification of the WATERING THE SOIL. 171 great necessity of attending to the due humidity of the soil, and to the prevention of stagnant water collecting about the roots. In like manner the injury committed by worms upon the roots of plants in pots chiefly consists in these creatures reducing the earth to a plastic state, and dragging it among the pot;- sherd.s so as to stop up the passages between them and destroy the drainage. One of tiie means of guarding the earth against an access on the one hand, and a loss on the other, of too much water, is by paying the surface of ground with tiles or stones, ind the advantages of this method have been much insisted upon. But, iu cold summers at least, such a pavement may prevent the soU from acquiring the necessary amount of heat ; and it may in some degree obstruct the free communication between the atmosphere and the roots. It is therefore a. practice that should be adopted cautiously. It is in places fuUy exposed to the sun, and liable to "bum" in summer, in consequence of loss of moisture, tbat paving answers best. On heavy land where trenches have been formed to hold peat for American and similar fibrous-rooted plants, it is sometimes found impossible to keep them alive in summer until the surface ip paved, after which they succeed perfectly. Here, however, it is found that the best kind of paving consists of round pebbles of gravel spread over the surface, with peat sifted between them. Flagstones, tiles, or large nodules of flint are objectionable. More commonly recourse is had to the operation of simple watering, for the purpose of maintaining the earth at a due state of humidity, and to render plants more vigorous than they otherwise would be ; an indispensable operation in hot-houses, but of less moment in the open air. It is, indeed, doubtful whether, in the latter case, it is not often more productive of disadvantage than of real service to plants. When plants are watered naturally, the whole air is saturated with humidity at the same time as the soU is penetrated by the rain ; and in this case the aqueous particles mingled with the earth are very gradually introduced into the circulating system, for the moisture of the air prevents a rapid perspiration. Not so when plants in the open air are artificially watered. This 172 WATBEING IN THE OtBN AIE. operation is usually performed in hot dry weather, and must necessarily be hmited in its effects ; it can have httle if any influence upon the atmosphere : then, the parched air robs the leaves rapidly of their moisture, so long as the latter is abundant ; the roots are suddenly and violently excited, and after a short time the exciting cause is withdrawn, by the momentary supply of water being cut off by evaporation, and by filtration through the bibulous substances of which soil usually consists. Then, again, the rapid evaporation from the soU in dry weather has the effect of lowering the temperature of the earth, and this has been before shown to be injurious ; such a lowering, from such a cause, does not take place when plants are refreshed by showers, because at that time the dampness of the air prevents evaporation from the soil, just as it prevents perspiration from the leaves. Moreover, in stiff soils, the dashing of water upon the surface has after a httle while the effect of "puddling" the ground and rendering it impervious, so that the descent of water to the roots is impeded, whether it is communicated artificially or by the faU of rain. It is, therefore, doubtful whether artificial watering of plants in the open air is advantageous, unless in particular cases ; and most assuredly, if it is done at all, it ought to be much more copious than is usual. It is chiefly in the case of annual crops that watering artificially is really important; and with them, if any means of occasionally deluging ground can be devised by means of sluices or other- wise, in the same way as water-meadows, it may be expected to be the most advantageous. The best gardeners employ overhead watering in the open air only in cases of absolute necessity. A curious case is recorded of a garden in a sandy soil at Tonbridge, in Surrey, which, through the hot and dry summer of 1842, remained in the most luxuriant beauty without receiving any assistance from watering. In this case the gardener stated that the garden in question was some eight years previously partly pond, and partly a sandy bank. The former was filled up witiL earth ; the latter was removed to the depth of three feet. A compost prepared of sandy loam, decayed vegetable mould, silver sand, and lime, well mixed and seasoned, was substituted, to the depth of three feet; and, under these circumstances, although not even a thunder WATERING IN THE OPEN AIK. 173 shower fell, some Lobelias and Fuchsias were the only plants that needed water. Watering is, however, sometimes- indispensable. When that is so, various plans are adopted to increase its efficiency, and as a substitute for overhead showers. Mr. S. Taylor, in the Gardener's Magazine for 1840, recommends the use of bottles, with two small holes in the sides, near the bottom. The bottles are buried to the neck near the roots of the flower which requires watering; and after being filled and corked, the water is allowed gradually to exude through the holes. This is objectionable, because the roots of the plants are liable to be injured in plunging the bottles, and it requires too many of them, where copious watering is necessary. Mr. W. P. Ayres thinks — " A better plan is to take moderate-sized flower-pots, and having placed an inch or two of rough gravel in the bottom of each, to place them round the plant to be watered, and fill them with water, which as it percolates gradually through the gravel, will soak into the ground. For plants such as Standard Koses, Rhododendrons, &e., closely turfed over on lawns, or for anything in a sloping situation, this is a most excellent plan, as the pots filled with water may be placed at night and removed the next morning, so as not to become an eyesore. Watering plants in flower- beds is at all times a difficult matter, because if the borders are sa&- ciently full of soil to give them a convex form, which they always ought to have, the water runs to the sides of the borders as fast as it is poured on. In such cases it will be found advisable to perforate the beds as thickly as possible, without injuring, the roots, to the depth of six or eight inches, with a stick one inch in diameter, and by filling these ten or a dozen times the groundwUl become thoroughly soaked. With Annuals, Verbenas, and other grouping plants, I have found this a most excellent method." The TIME OE DAT at which watering should be practised in the open air has given rise to much difference of opinion. Some gardeners insist upon the morning, others upon the evening. The first rest their opinions upon such considerations as the following : " Two acknow- ledged agents in vigorous growth are heat and jnoisture ; plants out of doors must take the heat as they find it, and as we cannot increase, our •object should be not to diminish it : moisture is under our control, but if we exercise that control, and water our plants in the evening during dry weather, we do so at the expense of a great portion of the heat we desire to preserve. Two influences are at that time brought into operation in cooling down the plants, and retarding their growth, which we thus vainly endeavo\ir to urge forward by moisture : these are evaporation and radiation. Evaporation is the more rapid in proportion "to the dryness of the air ; and hence it is most energetic, when the necessity for watering is most urgent: but evaporation cannot take ]place without producing cold, and .that cold is proportionate to the 174 THE APRIL MOON. rapidity of the process. dLemistry points out tte reason of this, vapour having a greater capacity for heat than water, the heat sensible in the water hecomes latent in its vapour, and the sensible temperature falls ; additional heat to keep up the temperature not being quickly enough supplied by the surrounding media. Let us look at the effect of this evening's supply of water to plants : the air is irj, evaporation goes on briskly ; the temperature sinks, the plants are chiUed, there are no sun's rays to communicate fresh warmth, and their growth is sometimes even more unsatisfactory than that of such plants as are growing in the apparently arid soU, and which have been allowed to take their chance. The other source of diminished temperature I noticed was radiation : every warm body tends continually to throw off its heat to all others of lower temperature, near or remote: but radiation in meteorology is more particularly confined to ' the radiation of heat from the surface of the earth and objects on it into a clear sky.' All objects do not radiate heat with equal rapidity : rough surfaces doit more readily than smooth, and dark surfaces than those of a lighter shade of colour. Apply the latter remark to the process of evening watering : almost all soils are darkened in their colour by moisture, and hence soil by this practice is reduced to the best possible condition for getting cooled down during the night." This is, in fact, a commentary upon what the French call the Zune JRousse or April moon, which they fancy rusts their crops. M. Ajago has shown that this notion is erroneous, the effect aUuded to being clearly owing to another cause, but one which must necessarily be in active operation on bright moonlight nights. He observed that in the months of April and May the temperature at night is often not more than four or six degrees above the freezing point ; and under these circumstances, when the sky is most unclouded and the moon shining brightest, heat wiU be radiated from the earth sufficient to reduce the temperature at the surface some degrees lower, or below freezing point; henoe the tender leaves and roots of plants are nipped by cold, and that appear- ance given to the former which is intended to be conveyed by the French word rousse. But it maybe doubted whether, under such con- ditions as are above assumed to exist, watering should be practised at aU. The principle is not to water if it can be avoided ; it is in hot. dry weather that the operation is most needed, and at that time the lowering of temperature at night is more beneficial than disadvanta- geous. It is evident indeed that the arguments just quoted are alto- gether one-sided, the real questions to be determined are, 1st, "Whether such a loss of heat is detrimental to plants ? and 2ndly, Whether there may not be some compensating advantages? "We believe that all plants are retained in a more healthy state by lowering their tempera- ture at night, and that no «rror is greater than that of supposing warm nights advantageous to them. In aU countries nature cools down the WATER SHOULD BE WARM. 175 soil very considerably at those seasons when plants are growing, and she ceases to do so only when vegetation is exhausted — or, perhaps, we ought rather to say, vegetation is exhausted when she ceases to do so. It is doubtless true that this cooling process may be carried too far. But that the amount of evaporation is not very considerable at night, is shown by the damp state of the soil the next morning after a watering. In watering at night the grojmd is soaked with moisture at a time when plants are exhausted of their fluids in conseq^uence of the perspiration that has been going on all day long ; the sooner that loss is supplied the better ; and during the night, when perspiration ceases, or very greatly diminishes, a plant is enabled to absorb by its roots the water it wants, so that by the return of day it is filled with fluid, and in the best possible state to resist the renewed action of the sun. But when water is applied in the morning the result is very different. The plant is called on to throw off moisture by its skin before it has been refilled by the absorbing action of the roots; the ground, too, which at night retains its water and conveys it to a plant, is called on to give it up immediately to the dry, warm, and gradually heating air. So that, in fact, a morning's watering cannot convey to the interior of a plant anything like so much water as that of the evening. I entertain no doubt that the great object of the cultivator should be to avoid the necessity of watering ; by shading the earth, or the plants themselves, or by the common operations of mulching and top dressing. When watering is inevitable the tempeeatukb oe the watee is a matter of great moment. Theoretically water should always be a few degrees warmer than the soil; practically this cannot be always ensured. All that a gardener can do is to keep his attention fixed upon the principle. In summer the earth may be taken to stand at 60° while cold spring water is not more than 50° ; to be beneficial the water ought to be 62° at least ; if warmer so much the better. For this reason water from ponds or- other places heated by the sun, should always be employed when circumstances permit it. In hot-houses rain water is now generally preserved in raised tanks which acquire the tempera- ture of the house. By such means warm water is secured. The practice has been arrived at by the teaching of experience, which shows that cold water applied to the roots of hothouse or greenhouse plants; is in the highest degree injurious, if not fatal. Among the evils of watering plants, is hardening the soil by the mechanical action of water frequently dashed upon it. In this way a hard crust is formed upon heavy soil, or the particles of sandy land are forced together into a compact mass, which interferes with the perco- lation of rain, and the free access of air to the roots. It is for this reason, that the application of liquid manure by engines, or by any contrivance that may cause it to fall from a height, is regarded as objectionable, and 176 MILDEW PEEVENTED BY WATERING. even likely to frustrate the object for which, it is used. To meet- this difficulty subterranean irrigation, by means of pierced pipes filled -with fluid under pressure, has been advocated by Mr. Chadwick, Mr. Kennedy and others ; and there is no doubt that it is the most effectual and xmobjectionable of all methods proposed for communicating fluids to the soU. It is, however, to be feared that cost will always be a bar to the adoption of this plan. Mildew, wHch is so often produced by cold dry air acting upon a delicate surface of vegetable tissue, is completely pre- vented in annuals by Yerj a bundant watering . The ravages of the Botrytis effusa, which attacks Spinach; of Acrosporium monilioides, which is found on the Onion ; and the mildew of the Pea, caused by the ravages of Erysiphe communis, may all be stopped or prevented by abundant watering in dry weather. Mr. Enight first applied this fact to the securing a late crop of peas for the table, in the following manner ; — The ground is dug in the usual way, and the spaces which will be occupied by the future rows are well soaked with water. The mould upon each side is then eoUeoted, so as to form ridges seven or eight inches above the previous level of the ground, and these are weU watered; after which the seeds are sowed, in single rows, along the tops of the ridges. The plants very soon appear above the soil ; and grow with much vigour, owing to the great depth of the soU, and abundant moisture. Water is given rather pro- fusely once in every week or nine days, even if the weather proves showery ; but, if the ground be thoroughly drenched with water by the autumnal rains, no further trouble is necessary. Under this mode of management, the plants wUl remain perfectly green and luxuriant till their blossoms and young seed-vessels are destroyed by frost, and their produce will retain its proper flavour, which is always taken away by mUdew. [Hort. Trans., ii. 87.) CHAPTER III. — ♦ — OF ATMOSPHERICAL MOISTURE AND TEMPERATURE.* The constituents of the atmosphere that surrounds us are either the same in different regions, or the differences, if any, are not appreciable By chemical processes. It is far otherwise, as regards temperature and humidity, which are so intimately connected that they cannot be considered apart from each other. From what has been already stated (Book I. Chap. V.), it is apparent that of the vital functions of plants none are more important than perspiration and evaporation ; and that, while a certain amount of loss of fluid particles is necessary to them, a great excess or diminution of the loss must be injurious. Although the solar rays appear to be the immediate cause of perspiration, which proceeds in proportion to their intensity, yet this action is necessarily modified by the state of the medium, that is, of the atmosphere, which surrounds them ; in proportion to its heat and dryness will their power be aug- mented, and in proportion to its cold and moisture diminished. The physiological effect of an excessive augmentation of perspiration is to dry up the juices and to destroy the texture pf the leaves ; on the other hand, an excessive obstruction of that function prevents the decomposition and assimilation of fluids, and the formation of new organised matter, as well as of * TMs suljjeot Has already been folly treated by the late Professor Daniell, in his excellent paper " On Climate with, regard to Horticulture," published in the Tramsac- tions of the fforticvltwal Society, vol. vi. p. 1. It is impossible to discuss the same topic •without profiting largely by this important treatise, which I have much foDowed in the present chapter. 178 THE HTGEOMETEK. the Becretions peculiar to a species. A state of the atmosphere, therefore, which is most favourable to the maintenance of the perspiratory action in the most healthy state, is that which it must be the business of a gardener to secure by all the means in, his power. The fitness of an atmosphere for maintaining a healthy vegetation depends upon the amount of moisture suspended in it, and upon its temperature. The hygrometer indicates the former, as the thermometer does the latter. Among the hygrometers intended for measuring the quantity of elastic vapour in the atmosphere, the most convenient for use is that invented by Daniell. In this instrument, the amount of moisture in a given atmosphere is indicated by what is called the dew-point ; that is to say, by the point of the thermometric scale at which the cold is sufficient to cause a deposition of dew. It is impossible for any one to know what degree of moisture he really maiatains in a forcing-house without an instrument by which to measure it ; that instrument is the hygrometer. Of Daniell's hygrometer the annexed cut exhibits the general appearance. It measures the moisture in the air quickly and precisely, and is not subject to get out of order. The air we breathe is a per- manently elastic fluid, containing watery vapour in mixture, its power of retaining which is greater when temperature is high than when low. It may be compared to a sponge ; if this substance, when dry, is soaked in water, a portion of the fluid is absorbed ; but if the sponge is again dipped without squeezing, and before it has had time to dry, no additional quantity of water wiU be taken up by it, because the first immersion saturated it; in like manner, when air has taken up as much moisture as it can contain, it is said to be in a state of saturation. If when thus saturated a reduction of temperature takes place, the capacity of the air for moisture is diminished, and precipita- tion ensues. "When air, on the contrary, is in an undersaturated, or dry state, it takes up moisture from the substances with which it comes in contact. If moist air is brought into contact with a substance sufficiently colder, a part of the moisture is condensed, and is so con- verted from a state of invisible vapour into water. If, for instance, a cold wine-glass is brought into a warm room, the sides of the glass become covered with dew, which is the water that existed in the air as vapour, and which, condensed on the cold glass, is changed into water. The effect, therefore, of bringing warm moist air into contact with a cold surface is to rob the air of a part of its moisture. Thus, in a cold night, the glass roof of a greenhouse may be seen streaming with water, which runs down and forms "drip," and in this often unsus- THE HYGROMETER. 179 pected manner air is rendered dry, notwitlistanding the operations of syringing, steaming, &o. Daniell's hygrometer is constructed with reference to these considerations. The figure represents two hollow glass balls, containing ether, and communicating by the glass tabe which rests on the support. The ball which forms the termination of the longer leg is of black glass, in order that the formation of dew on its surface may be the more perceptible ; it includes the bulb of a delicate thermometer, dipping in the ether, its scale being inclosed in the tube above the ball ; and whatever change takes place in the temperature of the ether is indicated by this thermometer. The other ball is covered with muslin. In making an observation, it is first necessary to note down the temperature of the air, next to turn the instrument so that when the muslin-covered ball is held in the hand the ether may escape into the blackened ball ; and it should also be held tiU the included ther- mometer rises a few degrees above the temperature of the air, when it should be replaced on the support. Then drop, or gentiy pour, a little ether on the muslin ; the evaporation of this extremely volatile sub- stance produces cold, and attention must be instantiy directed to the black glass ball and included thermometer ; the latter will be seen falling rapidly, and at length a ring of dew will appear at the line which runs across the black ball, — quickly if the air is very moist, slowly if the air is dry. If the air is in a very dry state no moisture will be thus deposited tDl the thermometer falls to perhaps 10°, 20°, or 30° below the temperature of the air ; but at whatever temperature the dew forms that temperature should be noted as the dew-point and the differ- ence between it and the temperature of the air at the time is the degree of dryness according to the indications of this hygrometer; thus, in a moderately dry day, let it be supposed that the temperature of the air is 65° in the shade, and that the muslin requires to be kept moist, before dew is formed, till the blackened ball containing the ether has its temperature reduced to 60°, as indicated by the included ther- mometer, there are then said to be 15° of dryness. Again, supposing the temperature is 85°, and the dew-point found, as before, to be 70°, the degree of dryness is still expressed by 15°; but the quantity of moisture diffused in the air is, notwithstanding, somewhat greater in the latter case than in the former. If 1000 represent complete saturation, the quantity of moisture when the temperature is 65° and the dew-point 50°, will be 609 ; but when the temperature is 85°, and the dew-point 70°, the moisture wiU be represented by 623 ; these numbers being ascertained by tables prepared for the purpose. The difference, however, in such a case, is so small that it is not worth taking into account in a horticultural point of view. But as these numbers can only be ascertained by calculation it is more convenient to reckon by the degrees of dryness, bearing in mind that the dryness of the air is indicated by the difference between the temperature of the N 2 180 DANIELIi'S HYGROMETER. air and of the dew-point. Thus, if the ring of dew is formed as soon as ether is applied, and only one degree of difference is observable, the air is nearly saturated ; if the difference is 5° to 10°, the dryness is very moderate, while 15° to 20° of difference indicate excessive dryness, and beyond this the air is parching. ^ Fig. XXIX. The objection to this instrmnent consists in its not being well suited to the hands of a person unaccustomed to use philosophical apparatus. In order to overcome this difficulty, Mr. Harris has proposed the following contrivance. ' ' It consists of an old-fashioned instrument commonly sold in the opticians' shops as Leslie's differential thermometer, (Pig. XXX. in the opposite page). It is arranged so that when not in use the fluid stands at zero in the stem, A ; over the bulb of the opposite stem, I, place a piece of muslin, C, which has been well soaked in a strong solution of common salt in water ; the muslin having been out into a circular shape, is laid on the bulb whilst wet, and the moisture wiU make it adhere sufficiently. A shelf, or bracket, with sides, top, and back, is made for it to stand on, to seclude it from the sunshine, an essential precaution, and .also to prevent the damp wall from having effect upon the muslin, so that it may draw all its moisture from the atmosphere alone. It will be found convenient to have a thermometer hung on the same stand, as in all hygrometric observations the state of the thermometer must be attended to. The rationale of its action is simple. If the absorption of moisture exceeds the evaporation from the muslin, heat wfll be generated which wiU expand the air in the bulb, C, and drive the fluid up the opposite stem, indicating the degree by HARRIS'S HTGEOMETER. 181 its rise. On the contrary, if the evaporation exceeds the absorption, cold will be produced, causing the fluid to fall. The general range of the scales made are from zero to 40°. In Mr. Harris's stove, under the general treatment of orchidaceous plants, temperature ranging from 78° to 95°, the hygrometer usually ranged from 15° to 30°." R*p ^ Fig. XXX. Of this instrument it has been complained that its divisions are in a great measure arbitrary and different from those of the thermometer to which gardeners are accustomed. But this is unimportant, inasmuch as men soon become acquainted with the value of the indications of any instrument, and it gives an absolute, if not a comparative result, which latter may be dispensed with. Mr. WaUes has expressed his opinion that " the wet-bulb thermometer, which has been long known, though recently improved in form, under the name of Mason's Hygrometer, is the one best fitted for the hothouse, being ' simple, self-acting, econo- mical, and certain,' and requiring the least attention to keep it in working order. Miason's instrument is, however,' not indispensable, as every gardener may readily convert any common thermometer into 182 TABLE OF DEW-POINT. a hygrometer. All that is reqiiired is to cut away a portion of the wood on which the tube is mounted, so as freely to expose the bulb, and to cover the latter with a fold of cambric, to which water must be supplied by means of a few threads from a phial placed near. Of course another thermometer, to indicate the temperature of the air, req[mres to be suspended near to that with the wet bulb, and care must be taken that, when dry, both mark the same degree of heat. To be quite accurate the dry-bulb thermometer should be covered with a similar piece of cambric, though this is hardly necessary, and may be incon- venient where the syringe is so often used. The mode of using any wet bulb thermometer is explained by the foUowing table and the remarks accompanjdng it, which were published some years ago by Mr,' Wailes, of Newcastle. Table op the Dew-Point when the Temperatitre of the Air, in the Shade, is between 55° and 100° of fahrenheit. Tempe- rature. Difference between the dry and Moistened Thermometers in degrees of Fahrenheit. 1" 2" B" 4° 5° 6° r° 8° 9= 10° 11° 12° 13° w 15° 55° 53 50 48 46 43 41 39 36 34 32 29 27 26 22 20 56 54 51 49 47 44 42 40 37 35 33 30 28 26 23 21 57 55 52 50 48 45 43 41 38 36 34 31 29 27 24 22 58 56 53 51 49 46 44 42 39 37 35 32 30 28 25 23 59 57 54 52 50 47 45 43 40 38 36 33 31 29 26 24 60 58 55 63 51 48 46 44 41 39 37 34 32 30 27 25 61 59 56 54 62 49 47 45 42 40 38 35 33 31 28 26 62 60 57 55 63 60 48 46 43 41 39 36 34 32 29 27 63 61 58 56 64 51 49 47 44 42 40 37 35 33 30 28 64 62 59 57 55 52 50 48 45 43 41 38 36 34 31 29 65 63 60 58 56 53 51 49 46 44 42 39 37 36 32 30 66 64 61 59 57- 64 52 50 47 45 43 40 38 36 33 31 67 65 62 60 68 65 53 61 48 46 44 41 39 37 34 32 68 66 63 61 59 56 54 52 49 47 46 42 40 38 35 33 69 67 64 62 60 57 55 53 50 48 46 43 41 39 36 34 70 68 65 63 61 58 56 54 61 49 47 44 42 40 37 35 71 69 66 64 62 59 57 56 62 50 48 46 43 41 38 36 72 70 67 65 63 60 58 56 63 61 49 46 44 42 39 37 73 71 68 66 64 61 59 67 54 52 60 47 46 43 40 38 74 72 69 67 65 62 60 58 55 53 51 48 46 44 41 39 75 73 70 68 66 63 61 59 56 54 52 49 47 46 42 40 76 74 71 69 67 64 62 60 57 56 63 50 48 46 43 41 TABLE OF DEW-POINT. 183 Tabm op the Dew-Point, &o., eontmued. Tempe- rature. Difference between the pry and Moistened Thermometers in degrees of Fahrenheit. {Continued.) V 2"- 3° 4° 5° &•■ 7° •8° 9° 10- 11° 12" 13° 14° 15° 77° 75 72 70 68 65 63 61 58 56 54 51 49 47 44 42 78 76 73 71 69 66 64 62 59 57 55 52 50 48 45 43 79 77 74 72 70 67 65 63 60 58 56 53 51 49 46 44 80 78 75 73 71 68 66 64 61 59 57 54 52 50 47 45 81 79 76 74 72 69 67 65 62 60 58 55 53 51 48 46 82 80 77 75 73 70 68 66 63 61 59 56 54 52 49 47 83 81 78 76 74 71 69 67 64 62 60 57 55 53 50 48 84 82 79 77 76 72 70 68 65 63 61 58 56 54 51 49 85 83 80 78 76 73 71 69 66 64 62 59 57 55 52 50 86 84 81 79 77 74 72 70 67 65 63 60 58 56 53 51 87 85 82 80 78 75 73 71 68 66 64 61 59 57 54 52 88 86 83 81 79 76 74 72 69 67 65 62 60 58 55 53 89 87 84 82 80 77 75 73 70 68 66 63 61 59 56 54 90 88 85 83 81 78 76 74 71 69 67 64 62 60 57 55 91 89 86 84 82 79 77 75 72 70 68 65 63 61 58 56 92 90 87 85 83 80 78 76 73 71 69 66 64 62 59 57 93 91 88 86 84 81 79 77 74 72 70 67 65 63 60 58 94 92 89 87 85 82 80 78 75 73 71 68 66 64 61 59 95 93 90 88 86 83 81 79. 76 74 72 69 67 65 62 60 96 94 91 89 87 84 82 m 77 75 73 70 68 66 63 61 97 95 92 90 88 85 83 81 78 76 74 71 69 67 64 62 98 96 93 91 89 86 84 82 79 77 75 72 70 68 65 63 99 97 94 92 90 87 85 83 80 78 76 73 71 69 66 64 100 98 95 93 91 88 86 84 81 79 77 74 72 70 67 65 Th.e bulbs of both, tbermometers should be covered with a fold of white silk or muslin, and pure water supplied to one of them from a phial or other vessel placed near it, by a thread of floss sUk acting as a siphon. The cover of the moistened bulb and the thread must be renewed occasionally. — The above table is sufficiently accurate for all practical purposes, but the true decreasing ratio is 2*33 for each degree of depression indicated by the moistened thermometer,* '^, After having obtained by Mason's hygrometer, 1st, the temperature of the air, as indicated by the dry thermometer, and, 2nd, the difference * To find the corresponding degree of Leslie's hygrometer, multiply the numher of degrees of difference between the dry and moistened thermometers by 6. 184 OTHER HYGROMETERS. between that and the indication of the wet-bulb thermometer, the dew-point can be ascertained by the accompanying table thus : — Supposing the temperature of the air, as indicated by the dry thermometer, is 70° Whilst the wet-bulb thermometer is 64° Degrees of dryness by this instrument 6° If we look in the left hand column, headed " temperature," we shall find 70° ; opposite this, and under 6° in the top column, we find 56°, the dew-point, or temperature at which the dew is deposited, according to DanieU's hygrometer, and 70°— 56°= 14° the degree of dryness by Daniell's instrument. By practice, or rather experience, a gardener would form as true a notion of the condition of his plants, with regard to moisture, by the indications of one instrument as he would by the other. He would learn that by Mason's 3° was a moderate state of dryness, but that 12° was excessive, just as easily as he would by observing 7° of dryness was moderate, according to Daniell's, but that 28° was parching (3 and 7, 12 and 28 are the corresponding degrees on the two instruments). So far these instruments are on an equality as regards their results ; whilst Mason's has the advantage of not requiring any experiment to be made, nor an ex- pensive substance like ether to be applied. Other modifications may be adopted, such as Rutherford's thermo- meter; or by using Six's, or one constructed after Dr. Traill's method, the maximum and miTiimiim of moisture can be registered by one bulb. Finally there is Simmons's Hygrometer, or more properly hygroscope, which has been much used, and of which a full account by Mr. BelviUe wiU be found in the Gardener's Chronicle for 1847, p. 815. The fault of this is that like all wood hygroscopes it is apt to get out of order, and to lose its hygrometrieal property with time. By means of these and similar contrivances, we are at all times able to ascertain exactly the quantity of water that exists in an elastic state ia the air. When the hygrometer was first brought into use, what was called a damp atmosphere was frequently seen to indicate a degree of moisture faUing short of •500, saturation being represented by 1000; and it was found that "120 was not uncommon — a state of thiags suf&cient to impair the vitality of the most vigorous vegetation. In this country, the changes of moisture are said to extend from I'OOO, or saturation, to '389, or even so low as '120, under a south wall for a short space of time ; " a state of dryness MOISTURE OF THE AIR. 185 wHch is certainly not surpassed by an African harmattan," but one which produces less disastrous consequences, because it is accompanied by a far lower temperature and a weaker solar radiation. The mean degree of moisture of the air near Xondon has been found by Mr. Thompson to be "897, on an average of ten years, while the mean temperature is 50'63 :* in other parts of the world it is very different ; and the amount of those differences, together' with the means of imitating them artificially, constitutes one of the most delicate and difficult parts of the gardener's art. All that relates to this subject, however, to be treated usefully, must be considered in a very special way, and in such detail as can only be expected in a separate work upon the subject. An idea of the difference between the atmospherical moisture of London and that of other parts of the world may, however, be collected from the following table showing the amount of rain that falls in a few different countries. Incites per annum. London 24'01 Average of 10 years. St. Petersburg ... IB- Algiers 27* Fattehpiir (East Indies) 35*94 Average of 4 years. Madeira 31- Sagar (East Indies) . . 31-15 to 64-76 SikHm, at 11,000 feet . 40- Bahamas 54-99 Calcutta 59-83 to 81- Ceylon 84-3 Macao 48-8 to 107-3 Equator 96- Dorjiling 122-26 Coast of Malabar . . . 123-50 Average of 14 years. Grenada. ..... 126- Leogane, St. Domingo . 150- Bengal 20 to 22 inches in a single month. Bombay 32 inches in 12 i ™, f 203-5 inches in six months ; as much as 8-5 ^^"^ I in a day (July 31, 1831). • See the various meteorological journals putlisied by the Horticultural Society, in their Transactions, from the year 1826 inolusi-^e. 186 WIND CAUSES EVAPOEATION, We possess, to a small extent, the power of modifymg the moisture of the air, even in the open air, and have almost complete control over that of glazed houses. It is found by experience that the effect of wind is to increase the dryness of the air, and, consequently, the perspiration of vegetable surfaces. It is through wind that the moisture of plants and the earth is constantly borne away, and thus the evaporation of plants is increased. "Evaporation," says Daniell, "increases in a prodigiously rapid ratio with the velocity of the wind ; and anything which retards the motion of the latter is very ef&ca? cious in diminishing the amount of the former. The same surface which, in a calm state of the air, would exhale 100 parts of moisture, would yield 125 in a moderate breeze, and 150 in a high wind." Hence, the great importance, in gardens, of walls and screens, which break the wind, and keep the air in repose in their vicinity. The difference between the effect of a given amount of cold upon the blossoms of exposed fruit trees, and those of the same species trained upon walls, is well known; and appears to be owing to this circumstance, much more than to any difference of temperature in the two situations. This has heen illustrated by Howard, in the results of some interest- ing experiments made by him on the annual amount of evaporation. During three years, in which the evaporating gauge was placed forty- three feet from the ground, the annual average result was 37 -85 inches ; during other three years, when the instrument was lower and less exposed, the average was 33'37 inches ; and when the gauge was upon or near the ground, the annual average was only 20-28 inches, or little more than half the amount evaporated in a free and elevated exposure. It is to be remarked that the easterly winds are, in this country, both the coldest and the driest. Daniell tells us that the " moisture of the air flowing from any point between N.E. and S.B. inclusive, is, to that of the air from the other quarters of the compass, in the proportion of "814 to '907, upon an average of the whole year ; " and Mr. Thompson has found the hygrometer to indicate not uncommonly from 20° to 30° of dryness, during the long prevalence of the north-easterly winds in spring. At the same time, the air is very cold, the effect of which is to cause the sap-vessels of the stem to contract, and AND CONSEQUENTLY COLD. 187 refuse to convey their fluid, bo that the blossoms of fruit-trees in a north-east wind, while they are robhed of their fluid con- tents by evaporation, can get no assistance from the roots through the stem, and necessarily perish; and this is no doubt one reason why open standard trees cast their flowers under a low temperature during the cold dry winds of our springs. I have now before me a standard "WasHngton Plum, bearing a crop of fruit in a garden where nearly everything else lost its blossoms on the 24th of April, 1854, when the thermometer fell to 18° Fahr. In this case a pile of firewood had been heaped round the stem to the height of the branches, and thus effectually guarded it from cold, Probably something was also owing to the warmth radiated from the pile of wood. This, however, only belongs to a class of facts of which the Magnolia grandiflora is an instance. Formerly there were trees of this species in Paris, whose only protection in winter was a heap of dry straw piled over their roots, so as entirely to cover them, and thatched to the height of five or six feet, so that the head of the trees formed the apex of a cone, the base of which was straw. By this precaution the earth is unable to freeze, and the fluids in the interior of the tree are maintained at a temperature approaching to that of the earth. "While, on the other hand, if the earth is frozen hard, the fluids in the roots are frozen also, and they thus tend to lower the temperature of the fluids and the branches. But this is, perhaps, not the only reason why tender trees are preserved by this sort of protection. It is to be observed that the destructive effects of frost are in proportion to the succulence of the parts on which it acts ; and it may be, that the con- tracting influence of cold gradually forces the fluids out of the unpro- tected branches into those lower parts which are guarded from the action of cold. Then the branches being pro tanto emptied of fluid, or dried, are thus deprived of a part of their susceptibility to cold. It has been objected by a critic that there is no experimental proof of contraction of tissue taking place under the influence of cold. But if the reader wiU turn to Biot's curious and little known observations, briefly reported in Senslow's Botany, p. 205, he wiU find that contraction imder cold has received the most conclusive experimental proof at the hands of one of the best of modern observers. There is also a fact on record which has hitherto remained without explanation, but which was probably con- nected with the contracting power of cold. In the winter of 1838, when the thermometer feU to 2° Fahr., Mr. Rogers observed the following phenomena : — During the extreme cold the branches of a Lime-tree, which overhung a part of his garden, drooped so as completely to lie upon the ground, and those above fell proportionately. The branches 188 SOUTH WINDS ARE THB DRIEST reo6vered ttemselve^ aa the day advanced and grew warmer, and eventually they so completely regained their original position that Mr. Eogers at first thought his gardener had Cut away all that drooped and impeded the path the day before. In this case it is almost certain that the drooping was caused by the expulsion of air and fiuid from the tissue by the contraction caused by cold, and that the revival was attributable to the reflux of air and fluid. I find, however, from Mr. Thompson's observations, that the greatest dryness we experience in this climate is, not when the wind is in the east, but when it is in the south. For example : - in nine years, between 1836 and 1834, the four driest days were in the year 1834, in June, when it was 33° on the 1st, 35° on the 2nd, and 31° on the 21st; on the 1st of June, 1833, it was 30°, and always with a south wind ; and, during the whole of those nine years, there was but one other day on which the dryness was found as high as 30°, namely, on the 10th of April, 1834, with a north-east wind. The duration of dryness, with a south wind, was, however, very short, not exceeding one or at most two days, and was invariably accompanied with great heat and foUowed.by heavy rain, while the north-easters last for weeks, without rain, and with a comparatively low temperature. The following statement puts this in a clear light. There occurred between 1886 and 1834, inclusive, — "Wind North . . . ... 7 „ North-East . . . .39 „ East . . . . 114 48 „ South-East . . . . ( 27 „ South . . . ... 35 „ South-West . ... 30 „ West . . . ... 35 „ North- West . ... 22 7 days, above 20° of dryness. These facts sufficiently explain the fatal effects of certain winds upon vegetation, the small comparative value in this country of walls with north and east aspects, and the general want of success that attends late spring planting. Here, also, we in part discover an explanation of the utility of shades interposed between the sun and plants newly committed to the earth : they not only cut off the solar rays, but also intercept SCREENS AGAINST WIND. 189 Pig. XXXI. currents of air, and thus diminish the amount of perspiration by two opposite methods. For screening plants from dry winds various means are employed, of which the following is a good example. In Prance a basket is employed, composed of two moveable semi-cylinders, constructed in the way of straw hives. To these semi-cylinders are fixed soUd feet of wood, for the purpose of being driven into the ground. If it is only necessary to shelter one plant from east or north-east winds, one semi-cylinder is sufficient ; but if it is a plant which you are forced to protect, is delicate, and requires a more complete protection, you inclose it between the, two semi-cylinders fixed one to the other by means of hooks represented in the drawing. A lid of the same construction, furnished at its edge with a circle in woodwork, is fitted, when necessary, upon the cylinder, and thus, perhaps, offers a more effectual shelter against the severity of cold winds and excessive heat than any other. These sorts of shades are light to move, very solid, and very warm; for, letting but little of the exterior air penetrate, they preserve at night the heat which accumulates in the interior. They also guard plants well from the action of sun, and thus offer a means of checking the natural perspiration of green parts. The following table, for which I am again indebted to Mr. Thompson, wiU be found to show that the average degree of dryness, in the middle of the day, throughout the year, is, with a — Degrees Amount of Dryness, of Moisture. North, wind 6-55 = 816 North-east V-30 = "794 East 6-20 = 825 Average, with wind from the three ) coldest points ..'...'...) ^'^^ " ^" South wiad 4-23 = 877 South-west . ■ 4-70 = 859 "West 6-20 = 733 Average, with wind from the thfee ) _ warmest points ." ) 190 TABLE OP DRYNESS AND WINDS. OT a oo g pa 'o M o ^ 11 •4j O H ^ E o « a Pi « ^ if g ^ en <1 o OQ a JO 99139(1 1IB9H o 8 U5 t- 1:^ CO t- It- i-( »-i 1 JO 99jS9a: TI'B9M o 6 1> 00 000 MOO C5 @ "ETPSM CO l:™ p "p w CO i* lO CO CO CO •BrarniM wBQyi m ob CO >o cq p M5 A 05 ■* (M (M co •tsthtx'bh: u'B9H CO ep 10 to CO 000 r^ CD CO CO Ti( ■* p « cq •BTP9H O -^ tp CO o 03 t^ « « W CO CO -^ «3 W5 tr~ T-t ^ ^ ■"dH t^ Jr^ A Jr- ! CD CO »0 >0 CO >p "^miTiijf TiBaj^ »0 CO »C >C »p -^ ^ I^ »0 (?q 00 CO CO ^ ^ J:- CO s § ^ ^ § •■ cq "Bniix'Bj^[ nsaj^ CO ':d i:^ O ^ ?s ^ s s »p >o p 00 1^ l~- do CO r- J:^ CO «3 ■<*< 05 do •rtooji ^B 9jn:^ST0K JO 99J59Q; U-BQfl COJr-CZ>QOJr^CNCOCDO OO O5»oooj:^oo^ocoo -ocq COCDCOJr-CO»f3ir-000 -005 1—1 1— ( JO 99JS9(3: TI'B9M coocoicoootpo o*? WC^O^wAtI^IOO lOCfl 1-1 f-l ,-( rH ,-1 CO 1^- i •eipsw OW3»f3*pO>CiO(NO >pcq COCO-^-p ATHOob-^tHos^-os :^-cb (MCOtHCOtH-*'*»J^tH (MCM CO "ennx'BK n^gj^ OOOCpClOOipO ■ ' t^ OS CO 00 •TIOO^ i^-B 9S9Tl£jC[ JO oajSaa traaK j> o »p CO o 90 « CO ! OS ! (N w : i-H i-H p CD El i ■Brp9H ip cq »p qp CD T^ 6s ! oo t^ ! tH 0 CO «5 CO CM •'em^nm. ^^W 00 000 ^ ^ 6i >h ;coj>-6s Icodb r Cq CO TtH -* -* «3 -^ CO eq •bhitxbh: TI'B9P[ cq *o -^ » '?' -^ CO ; w « CD : »b : CO tH CO ir- CO Xr^ ZD 1— ( do W3 t-i a =^ • - • • -g "l §3 "d '^ 1 TABLE OF DRYNESS AND WINDS. 191 o (M 1-* CO tT> CO lO m f-1 05 tH o >o 1^ ffl IN o m o -^ g JO oa^aoa ireaM 1-H 05 CD CD ra o CO lO o o •O a CO •* ■* ^ o o o o >o O U5 o >o o ^ o "Bmnnin tib9H[ t~ 05 on J~ y-t O tr 00 ?a 00 i CO -* (M -* >ra lO -* IN -* CO o O O o o >I3 «3 CO o >o E-i "BDns'BK ti-egj^ o O 1— ( ■* as O CO o r- -* lO CO LO t- Ir- CD us ■* >o o- ^ cr (M 1^ 't^ co r-l 05 ^ CO CO •Tioo^ qia gjn^ffioj^ w o Ti o o rf CO CO cr. ■^ O) CO JO eaj39(x n-Baj^ o- O) cc t- Ir- CD cu i^ ai 05 05 ■uoo^ IJ-B SSaTlj£lQ[ C£ T-( O «5 00 02 05 >o c CO CO cq ^ N JO 99x39(1 n-Baji C CO 1— ( ;^ T— ( tH (J- CO ■* O t- r- 00 IN «2 00 05 CO » "BTpSW t^ • iH t- CO o lO '^ 05 »c CO IN »— 1 s C^ Th tH •* CO CO CO ID »c TJH tH «5 a o o »o 00 -* CD O »c r-t CO IN o "ETnmtJI XL-BBfl V ■* o- co o CO i-( 1—1 a: a> t^ CO i ir CO CO CO K> >o m >ra ^ CO CO ■* c t- 0- o CO o o lO us U5 CD ■* Eh ••BTmxvpi UVQfl ^ ur t^ o on or) r~ ,H on l~ 05 •* ■* «: lO J:~ t- ir- CO CD -* Tt* >o t- Tt< cr o rV <-i tH CO IN 00 05 05 i c- 1:- Tl . o CO u: IN lO Cf CO CO >o JO G3J39(I TIB8M: c 00 oc o CO t- r- 00 00 05 05 00 •Tioo_ti ^JB ssatr^d c CD o o ■!jf eo o 00 CD o 05 J> 1 w JO aajcSao: xib9M c o o CM i-H ■* ■* c Tj< CO o CO o lO 00 ■*< 05 o eq i i 9 •BrpoH (T ^-H en >o CO ■* t- J^ CO :51 CO IN o C 00 cc o ira o o o CO IN CD eq O 'IjUlLUL^ UVd^ «: CO or Cf) (M ■* 05 CO CO or J:- ^ oo ■* CO TtH >o «5 "O ■* Th CO CO c T-H o o (M O o CO cq t- «5 ■* H ■-eraixBn xvesyi Ir m Tt (M •^ ■* CO CJ5 CO r-l on o <^ U5 w CO P- 1:- CO >ra ■* CO CD CO «? o o a i a 1 CO tH 03 t- r-l oc oo oo ir- w JO 99x39(1 ireaH a ■nooH ?« BB9iiira JO 09139(1 ^«9W: IN 6 rH 1?- 1^ 05 o oc CO 6 o on a t »o CO CO Oi 00 CO CO .-1 i-H 'i* i '«TP9H V 1 o» CO CO •* CO T— 1 00 o 1:- T— 1 c 5 CO ■* "O X5 CD CO ■* 0( 3 O O CD 1— ) O ■* CO CO o 1:~ ■iBUiimM u-ESM f ■) CO a> Tti (M CO IN CD cq CO 1 c 3 CO CO ■* Tt( o -^ c 5 O t- o 00 CD 05 CO CD eq »-l E^ "Bnnx'Bj[ Tnjaj^; ^ A CO ■*( (M r- t- o »c CO IN 05 Ti 4 ^ O CO co Jr- 1~- S ' b-. • • ^ s fs ^1 •g 1 life" Irj 1-7 ^1 ^ O 03 O ^ P a 192 DRYNESS IMPORTANT TO RIPENING. The dryness of the atmosphere, which proves so fatal to plants when in a state of growth, is, when accompanied by warmth, of the greatest importance to them while ripening their fruit. Together with the high temperature of the soil, it is this which causes so great a difference in the quality of the same kinds of fruit ripened in the South and the North. The excellence of Syrian Apricots is not approachable in England. The Grapes of the Mediterranean shore are only equalled in England in the best managed hothouses, when sun heat and artificial heat are skilfully employed to dry as well as warm the air, at the season of ripening. The richest and strongest wines in the world are those of Hungary, which, according to Wahlenberg, owe their excellence to the great dryness of the autumnal climate of the vaUey of the Theiss. Dryness of the air then, which is fatal to plants in a rapid state of growth, is in the highest degree beneficial when their functions are limited to the consolidation of tissues already formed and the elabora- tion of their final secretions. In the open air in England, the ripening process is usually incomplete, and hence the inability of plants from the United States, and other countries with hot autumns, to bear with us a winter far less severe than that which is natural to them. Nothing can iEustrate this truth in a more striking manner than the follcwing statement by the late Sir Augustus Poster. Writing from Genoa he says : — " Being under the impression that single Orange or Lemon-trees, or rows and groups of Orange or Lemon-trees, might with care be brought to grow out of the groimd in England like other plants, I have thought it might be worth while to mention the success which has now for several years attended a plantation that I made of seven Orange-trees in a much colder climate, in the garden of my country residence, on the lull of Turin, facing the highest range of the Alps. I was led to make the experiment from having by accident, in the jBrst year of my arrival at Turin, seen the way in which the Orange-trees in boxes were treated in the cellars of a Piedmontese nobleman's house during winter, where they were placed for several months, without light, or heat, or water, and exposed to severe cold which almost every winter reaches to — 12° or even — 16° of Eeaxtmite's thermometer (+5° to 4° Pahr.). My group of Orange-trees were taken out of boxes, and planted in earth prepared for the purpose, in the year 1826. In the very severe winter of 1828-9, three of them HARDINESS OF THE ORANGE-TKEE. 193 perished, but not of the eold so much as the damp, for they were ex- amined, and seen to be still safe in February, after the frost had reached above 15° of Rbatjmite ( — 2° Fahk.), and perished a few days later from a return of the cold, attended by the drippings of a preyious thaw. I had the three which died replaced, and from that time to this they have flourished and increased in size. I have them covered with a round cabin of planks, roofed with straw on the outside, at the end of October or beginning of November, and uncovered in April. They bear abundance of Oranges and Lemons, the former occasionally becoming eatable with sugar. At no other place in this country am I aware that the experiment has been tried, unprotected by a wall. But with a wall and a covering of wood and straw, to be taken off in the summer, I can scarcely doubt that the plants might be made to grow, without the clumsy accompaniment of large wooden boxes, in an English garden." This case establishes the fact that in the north of Italy the Orange-tree bears a degree of winter cold unknown in England. For this it is prepared by the complete ripeness of its wood, a state to which it can never arrive in this climate in the open air. But are we therefore to infer that it will not live with less shelter than it now receives ? Such an inference is scarcely justified, and it is worth the consideration of those who have Orange-trees at command, whether they wiU. not pass the winter in barns, or dry out-houses, or under wooden screens where no artificial heating is applicable. Dryness in such an experiment is the first condition to secure ; darkness is the second. The Orange-tree will bear to be deprived of water during the whole of its season of rest, provided its roots are kept in the earth they grew in ; how much dryness, beyond this, they will bear, is shown by the long exposure to the air which they undergo in the shops of the Italian warehousemen in London ; and experience tells us that the effect of cold upon plants is feeble in direct proportion to their dryness. All trees kept in the dark, or at least kept where no sun can shine upon them, will bear without injury a degree of cold which would be fatal to them if ex- posed, when frozen, to the direct rays of the sun. Camellias, Chinese Azaleas, ladian Ehododendrons, and many New Holland plants, take no harm in cold pits in winter, provided those pits face the north. Some of them live out of doors perfectly well during winter, if under north walls ; and we have in our possession a small Orange-tree which passed the winter of 1853-4, when the thermometer fell to 4 ° Fahr. un- injured in a cold pit facing the north. As to temperature in the open air, unconnected with atmospherical humidity, there seems to be no means of regu- lating or modifying it to any considerable extent. In some respects, however, we have even this powerful agent under our 194 SOLAE RADIATION. control ; but in order to exercise such control, it is necessary to understand correctly the theory of what is called eadiation. This cannot be better explained than in the words of DanieU. " The power of emitting heat in straight lines in every direction, indepen- dently of contact, may be regarded as a property common to all matter ; but differing in degree in different kinds of matter. Co-existing with it, in the same degrees, may be regarded the power of absorbing heat so emitted from other bodies. Polished metals and the fibres of vege- tables may be considered as placed at the two extremities of the scale upon which these properties in different substances may be measured. If a body be so situated that it may receive just as much radiant heat as itself projects, its temperature remains the same ; if the surrounding bodies emit heat of greater intensity than the same body, its tempera- ture rises, till the quantity which it receives exactly balances its expenditure, at which point it again becomes stationary ; and if the power of radiation be exerted under circumstances which prevent a return, the temperature of the body declines. Thus, if a ther- mometer be placed in the focus of a concave metallic mirror, and turned towards any clear portion of ijie sky, at any period of the day, it wilL faU many degrees below the temperature of another thermometer placed near it, out of the mirror; the power of radi- ation is exerted in both thermometers, but to the first all return of radiant heat is cut off, while the other receives as much from the surrounding bodies, as itself projects. This interchange amongst bodies takes place in transparent media as well as in vaouo ; but in the former case, the effect is modified by the equalising power of the medium. Any portion of the surface of the globe which is fully turned towards the sun receives more radiant heat than it projects, and becomes heated ; but when, by the revolution of the axis, this portion is turned from the source of heat, the radiation into space still continues, and, being un- compensated, the temperature declines. In consequence of the different degrees in which different bodies possess this power of radiation, two contiguous portions of the system of the earth wiU. become of different temperatures ; and, if on a clear night we place a thermometer upon a grass-plat, and another upon a gravel walk or the bare soil, we shall find the temperature of the former many degrees below that of the latter. The fibrous texture of the grass is favourable to the emission of the heat, but the dense surface of the gravel seems to retain and fix it. But this unequal effect will only be perceived when the atmosphere is unclouded, and a free passage is open into space ; for even a light mist will arrest the radiant matter in its course, and return as much to the radiating body as it emits. The intervention of more substantial obstacles will of course equally prevent the result, and the balance of temperature will not be disturbed in any substance which is not placed SOLAE RADIATION. 195 in the clear aspect of the sky. A portion of a grass-plat under the protection of a tree or hedge, will generally be found, on a clear night, to be eight or ten degrees warmer than surrounding unsheltered parts ; and it is well known to gardeners that less dew and frost are to be found in such situations, than in those which are wholly exposed." {Sort. Trans., vi. 8). This very important subject has received further explanation from a writer, whose words we quote, with some omissions, from the Gardener's Chronicle of 1853, pp. 679 and 627. The action of the sun upon aU. things that receive his rays is a matter of common notoriety. How important to the growth of plants, to the formation of colour and taste, to the ripening of fruit, to the consolidation of all vegetable tissues, is solar light it is needless to say. But few persons are aware of the amount of that force, or of the views of modem philosophers as to the manner in which it takes effect. We may view the surface of a lake exposed to the sun's rays during a warm summer's day, whilst the whole scene may seem to be one of the utmost tranquillity, so that we might naturally conclude that no movement of any import- ance was then going on. It will be found, however, that such in reality is not the case ; for the rays of the sun exert a force of which we can scarcely form any adequate idea. Supposing the lake is only two miles square, it may be calculated that there wiU be raised from its surface in one day more than sixty-four thousand tons weight of water (64,821), by means of solar radiation. This is at least equal to the work of 10 steam-engines of 200 horse-power each for the same space of time, presuming that the above weight is only raised to an average height of between 300 and 400 feet. To balance that weight, a hill of earth would be required, 30 feet high, 100 feet wide, and 600 feet in length. In making the calculations which have led to these statements, it has been assumed that, in a hot day in summer, a quarter of an inch of water would be evaporated from an exposed surface of a lake in twelve hours, and this from an area of two miles square would amount to 2,323,200 cubic feet, which, at 62^ pounds per cubic foot, is equal to 64,821 tons. Now, a quarter of an inch is not a maximum amount of evaporation. The Comte de Gasparin observed 0-59 inch ( Gardiner's Chronicle, 1849, p. 757), and on five successive days the average exceeded haK an inch. Howard, in his Climate of London, has recorded as much as 0*39 inch in one day. It therefore appears that 0-25 inch, that which we have assumed, is not an exaggerated quantity ; on the contrary, it is but one-half of that which, according to good authorities, has been actually removed by evaporation, and under a temperature of from 73° to 75° Fahr. Instead of 64,000 tons, facts would justify us in stating that 130,000 tons might be raised in one day from a surface of water not exceeding two males square. Some idea may be formed from these statements of the immense 2 196 SOLAR RADIATION. power of solar radiation in a comparatively limited space ; but the many thousands of tons raised from that space do not represent the full power of the sun's rays. They merely represent weight raised, without our taking into account the force exerted in converting the water into vapour, and in that form elevating it hundreds, or it may he thousands of feet, notwithstanding the pressure of the atmosphere. In a commu- nication on the Mechanical Action of JRadiant Seat or Light, by Professor William Thomson, Philosophical Magazine, fourth series, vol. iv., p. 256, it is stated that "mechanical effect of the statical kind might be produced from the solar radiant heat, by using it as the source of heat in a thermo-dynamic engine. It is estimated that about 556 foot-pounds (that is, so many pounds raised one foot high) per second of ordinary mechanical effect, or about the work of ' one- horse power,' might possibly be produced by such an engine exposing 1800 square feet to receive solar heat during a warm summer day in this country ; but the dimensions of the moveable parts of the engine would necessarily be so great as to occasion practical difficulties in the way of using it with economical advantage that might be insurmountable.'' This is more than twenty times the power we have assigned to the raising of water, |iiid even this appeared so vast that until the data were thoroughly examined, the statement appeared incredible. The same author proceeds to state that " the deoxidation of carbon and hydrogen from carbonic acid and water, effected by the solar light on the green parts of plants, is a mechanical effect of radiant heat. In virtue of this action, combustible substances are produced by plants, and its mechanical value is to be estimated by burning them, and multiplying by the mechanical value of the thermal unit. Taking from Liebig's Agricultural Chemistry the estimate, 2,600 poimds of dry Fir-wood, for the annual produce of one Hessian acre, or 26,910 square feet of forest land, which is at the rate of 4208 pounds or nearly 2 tons per English acre, and assuming, as a very rough estimate, 4000 thermal units centigrade as the heat of combustion of dry Fir-wood, the author finds 650,000 foot-pounds, or the work of a horse power, for 1000 seconds, as the mechanical value of the mean annual produce of a square foot of the land ; and taking 50° 34', that of Giessen, as the latitude of the locality, he estimates the mechanical value of the solar heat, which, were none of it absorbed by the atmosphere, would fall annually on each square foot of the land, at 630,000,000 foot-pounds ; and infers that probably t-oW of the solar heat which falls on growing plants is con- verted into mechanical effect. "When the vibrations pf light thus act during the growth of plants, to separate, against forces of chemical affinity, combustible materials from oxygen, they must lose vis viva to an extent equivalent to the statical mechanical effect thus produced, and therefore quantities of SOLAR RADIATION. 197 solar heat are actually put out of existence by the growth of plants, but an equivalent of statical mechanical elTect is stored up in the organic products, and may be reproduced as heat by burning them. All the heat of fires obtained by burning wood grown from year to year is in fact solar heat reproduced." And so, we may accordingly add, must be the heat derived from the combustion of at least the portions which have had a vegetable existence, of wood-coal and other matters. Professor Thomson has concluded, and with reference to an equivalent conclusion by Sir John Herschel, that heat radiated from the sun (sunlight being included in this term) is the principal source of mechanical effect available to man. From it is derived the whole mecha- nical efiect of animals working, water-wheels worked by rivers, steam- engines, and galvanic engines, &c. Vegetation is the great support of animal power, but vegetation could not be maintained without the action of the sun's rays, received directly or indirectly. "Without such powerful evaporation caused by the sun's rays, as we have endeavoured to exemplify, the rivers would soon lose their general source. And it has been already stated that combustible materials, without which steam-power could not be generated, are stores of solar heat. This gives some idea of the immense power of solar radiation ; and within their respective spheres of action, both horticulturists and agriculturists may advantageously direct their attention to the subject. For instance, the former would avoid watering at a time, and in a manner, that would render nearly all the water he supplied liable to be carried oflf by evaporation before it could reach the principal roots of his plants ; and the farmer, knowing the effects of radiation on a moist surface, would hesitate before he flooded say four acres with manure water, at the risk of losing a hundred tons of it, together with its portion of ammonia, by evaporation. The same subject is taken up by the Comte de Gasparin in a commu- nication to the Institute, printed in the Comptes Mendus for June, 1853. The effects, he observes, of solar radiation on vegetation are so apparent and so well known that no one doubts their importance. When one plants a Vine, he does not require scientific information to direct him in choosing a southern aspect; nor to plant fruit-trees against a wall which receives and reverberates the rays of the sun; nor to place exotic plants under glass, which readily admits direct rays of heat and light, but through which obscure heat, or that derived from a heating apparatus in a hothouse, passes slowly, and thus an accumiilation of heat takes place ; practical men do all these things as a matter of course. But there are many other effects resulting from the same cause, which do not come so directly under our senses. . The Olive is unproductive at Agen, with a mean temperature 9f 57° Fahr., and fertile in Dahnatia with 55^° ; the limit of the Viue is arrested by 54° mean temperature on the banlcs of the Loire, but grapes ripen where the mean temperatuie 198 SOLAR KADIATION. is only 50° on the Ehine ; the harvest near London is matured with a mean summer temperature of 62°, and in the same time at Upsal with 59°. When we take these phenomena into consideration, we must conclude that they depend upon the presence or absence of that important element of heat, solar radiation, by which the temperature of opaque bodies is raised above that which they could receive from the diffused heat of the atmosphere. When we also know that the absorp- tion and assimilation of carbon, the substance of which about half the mass of plants is composed, does not take place except under the influence of light, and is proportionate to its intensity, we feel assured that the determination of its effects must prove interesting to cultivators. Under this impression, the Comte de Gasparin made various experiments. In 1840 he communicated some observations on three Mulberry-trees, of the same variety. One of these was fully exposed to the rays of the sun, the second only till noon, and the third was whoUy in the shade. The solid matter of the leaves of the first was 45 per cent, of their weight ; that of the second, 36 per cent. ; whilst that of the third was only 27 per cent. In 1852 he ctdtivated some Broad-beans on a plot of ground divided into two equal parts by a partition which shaded one half the ground from the rays of the sun. After being dried, the plants grown on the south side weighed 21 ounces ; hut those grown on the north side,, although much taller, weighed only twelve ounces. The difference in their fructification was, however, still more remai'k- ahle. The plants on the south side had 131 pods, those on the north only 4*7. It is impossible to attribute these results to the simple augmentation of heat. The plants in the above experiment had a mean, atmospheric temperature of 59J° Fah. for 84 days, and 5|° was the average d.aily amount of solar radiation. Certainly an additional 5J° of obscure heat would not produce such results. The laws indicated by Daniell plainly direct us to the means we are to employ to moderate atmospherical temperature. A screen, of whatever kind, interposed between the sun and a plant, intercepts the radiant heat of the sun, and returns it into space ; and thus, in addition to the diminution of perspiration by the removal of a part of the stimulus that causes it, actually tends, to lower the temperature that surrounds the plant. In like manner, the interposition of a screen, however slight, between a plant and the sky, intercepts the radiant heat of the earth; and, instead of allowing it to pass off into space, returns it to the ground, the temperature of which is main- tained at a higher point than it otherwise would be. Hence it is that plants growing below the deep projecting eaves of NOCTURNAL RADIATION. 199 houses, or guarded by a mere coping of thatched hurdles, suffer less in winter than if they were fully exposed to the sky. It is also obvious from what has been stated that plants growing upon grass will be exposed to a greater degree of cold in winter than such as grow upon gravel: but it does not therefore follow that hard gravel is, with respect to vegetation, a better coating for the surface of the ground than turf ; it has its disadvantages as well as its advantages, and the former probably outweigh the latter. Its superior heating power is its only advantage ; the objections to it are, its dryness in summer, and its comparative impermeability to rain, so that it causes the force of perspiration to be inversely as the absorbing power of the roots. In Grermany, where the winters are very severe, it is customary to cover the roots of plants on grass with a mulching of leaf mould, six inches deep and a foot in diameter ; but this can have, I think, no sensible effect upon roots, because of the inconsiderable area that it occupies. It is well known that blackened surfaces absorb heat much more than those of any other colour ; and it has been expected that the effect of blackening garden walls, on which fruit-trees are trained, would be to accelerate the maturation of the fruit ; but, notwithstanding a few cases of apparent advantage, one of which, of the Vine, is mentioned in the Horticultural Transac- tions, vol. iii., p. 330, this has been, in general, found either not to happen at all, or to so small an extent as not to be deserving of notice in practice. It is true, that so long as the wall is but little covered by the branches and leaves of a plant, the absorbent power of the blackened surface is brought into play; but this effect is lost as soon as the wall becomes covered with foliage. In the early spring before the leaves appear, the flowers are brought rather more forward than would otherwise be the case, which is in England a disadvantage. It would seem, however, that in autumn the wood becomes more com- pletely ripened ; but the effect is very slight. It is rather to a judicious choice of soil and situation that the gardener must look for the means of softening the rigour of climate. Wet tenacious soUs are found the most difficult to 200 RELATION OP SITUATION TO COLD. heat or to drain, and they will, therefore, he the most unfavour- ahle to the operations of the gardener ; extremely light sandy soils, on the other hand, part with their moisture so rapidly, and absorb so much heat, that they are equally unfavourable. It is the light loamy soils, which are intermediate between the two extremes, that, as is weU known, form the best soil for a garden. Situation is, however, of more consequence than soil, for the latter may be changed or improved, but a bad (that is, cold) situation is incurable. Cold air is heavier than warm air, and, consequently, the stratum of the atmosphere next the soil wiU. be in general colder than that above it. "When, therefore, a garden is placed upon the level ground of the bottom of a vaUey, whatever cold air is formed upon its surface remains there, and surrounds the herbage : and moreover, the cold air that is formed upon the sides of low hills rolls down into the vaUey as quickly as it is formed. Hence the fact which to many seems surprising, that what are called sheltered places are in spring and autumn the coldest. We aU know that the Dahlias, Potatoes, and Kidney-beans of the sheltered gardens in the valley of the Thames, are killed in the autumn by frosts whose effects are unfelt on the low hiUs of Surrey and Middlesex. Daniell says he has seen a difference of 30°, on the same night, between two thermometers, placed the one in a valley, and the other on a gentle emiuence, in favour of the latter. Hence, he justly observes, the advantages of placing a garden upon a gentle slope must be apparent; "a running stream at its foot would secure the further benefit of a contigu-. ous surface not liable to refrigeration, and would prevent any injurious stagnation of the air." One of our German translators has expressed his opinion that no such difference as 30° can have been observed, and alters the statement to 3° Reaumur! But if he had consulted Darnell's Meteorological Essays, Ed. 2. p. 525, he would have found that the quotation is exact. No doubt it was an extreme case ; but Mr. Thompson remarked last April that at the time when fruit-buds near the ground had been universally kUled by , 14° of frost, they were safe on trees twenty-five to thirty feet above the level, and he beUeves there may have been a difference of 10° — 12° in favour of even that slight height. As a good example of the practical mode of dealing with low LOW SITUATIONS, HOW IMPEOVED. 201 situations, with a cold bottom, the following operation, described by Mr, W. BiUington the elder, may be advantageously imitated : — "About the middle of June 1800, I arrived at Brocklesby, Lincoln- shire, as gardener to the late Lord Yarborough. At that advanced season I found the Peach-trees in a deplorable state, with scarcely any leaves upon them, few branches, and very little fruit ; the few leaves that remained were all curled or diseased, and soon after shrivelled up and feU off. The trees were not very old— about thirty years, but had extended over a, fine wall without flues. The site of the garden was very unfavourable, a worse could not have been found near the mansion ; for it was both low and wet. Previously to its being made into a garden, the water used to stagnate and cover a great part of it through the winter ; but it had been drained at a great expense, and fresh soU had been brought in for the fruit-tree borders, &c. But after aU. the situation could not be essentially improved, nor the ill effects upon vegetables and tender fruit-trees entirely averted in an atmosphere so damp from the exhalations that arise in such places in the autumn and spring months, when sunny days and frosty nights are so prevalent. The fruit-tree borders had been weU made and well drained ; the trees had grown luxuriantly and covered the walls : but no fruit was pro- duced of any consequence, and that was not well-ilavoured, either on the walls or elsewhere. The Peaches and Apricots on walls would make efforts in the spring of each year to produce wood and leaves, hut when the cold weather prevailed, in April, May, and June, with easterly winds and frost, the leaves became diseased and curled, and were either pulled off or fell of themselves in June or July. Thus the trees became inactive for want of healthy leaves, at the time when they should have been making and perfecting the wood for the next year's crop. But towards the end of summer, when the earth had become dry and warm to a great r alkaline pole of a galvanic battery caused seeds to germinate in much less time than the positive or acid pole, he was induced 236 EFFECT OF DEOXYDISINGt SEED. to observe the effects on seeds of acetic, nitric, arid sulphuric acids, and also of water rendered alkaUne by potash and ammonia. " In the alkaline the seeds vegetated in thirty hours, and were well developed in forty ; while in the acetic and sulphuric they took seven days ; and, even after a month, they had not begun to grow in the acetic." This experiment led to others upon limie ; " a very easily procured alkaH, and which he inferred to be more efficient than any other from the well known affinity of quick or newly slacked lime for carbonic acid. Lime, as taken from the quarry, consists of carbonate of lime, or lirae united to carbonic acid; but, in the act of burning, the carbonic acid is driven off; and hence the great affinity of newly slacked lime for carbonic acid. He depended, there- fore, upon this affinity to extract tlie carbon froUi the starch, assisted by moisture ; " (Gard. Mag., xiv. 74) and he reported that the results were exceedingly striking. Old Spruce Fir seed, which would scarcely germinate at two years old, produced a fine healthy crop when three years old, having been first damped and. then mixed with newly slacked lime ; and, under the same treatment, ari average crop of healthy plants was obtained when the seed was four years old. The manner in which the original experiments upon acids and alkalies were conducted is not explained ; it is to be presumed that the water employed was only acidulated with the acids spoken of. It is, however, certain that whatever effect may be practically experi- enced when particular solutions are employed it has no relation to electrical action. Mr. Edward SoUy proved experimentally in the garden of the Horticultural Society that electricity has no discoverable influence upon vegetation either in its active growth or during the period of germiuation. (See Journal of Hort, Soc. vol. i., p. 81, and ii., p, 45.) The last method of promoting germination, to which it is necessary to advert, is the mixing seeds with agents that have the power of Hberating oxygen. It has been shown that a seed cannot germinate until the carbon with which it is loaded is to a considerable extent removed ; the removal of this principle is effected by converting it into carbonic acid, for which purpose a large supply of oxygen is required. Under ordinary circum- INUTILITY OF SEED-STEEPING. 237 stances, the oxygen is furnished by the decomposition of water by the vital forces of the seed; but when those forces are languid, it has been proposed to supply oxygen by some other means. Humboldt employed a dilute solution of chlorine, which has a powerful tendency to decompose water, and set oxygen at liberty, and, it is said, with great success. Oxalic acid has also been used for the same purpose. Mr. Otto, of Berlin, states that he employs oxaKc acid to make old seeds germinate. The seeds are put into a bottle filled with oxalic acid, and remain there tUl the germiuation is observable, which generally takes place in from twenty -four to forty- eight hours, when the seeds are taken out, and sown in the usual manner. Another way is to wet a woollen cloth with oxalic acid, on which the seeds are put, and it is then folded up and kept in a stove; by this method small and hard seeds will germinate equally as well as in the bottle. Also very small seeds are sown in pots and placed in a hotbed; and oxalic acid, much diluted, is applied t,wice or thrice a day till they begin to grow. Particular care must be taken to remove the seeds out of the acid as soon as the least vegetation is observable. Mr. Otto found that by this means seeds which were from twenty to forty years old grew, while the same sort, sown in the usual manner, did not grow at all {Gard. Mag., viii. 196); and it is asserted by Dr. Hamilton (16., x. 368, 453,) and others, that they have found decided advantages from the employment of this substance. Theoretically it would seem that the effects described ought to be produced, but general experience does Hot confirm them; and it may be conceived that the rapid abstraction of carbon, by the presence of an unnaturally large quantity of oxygen, may produce effects as injurious to the health of the seed, as its too slow destruction in consequence of the languor of the vital principle. It is an old assertion, revived within