Cornell University Library TD 910.C13 1880 Sanitary engineering. 3 1924 004 131 391 Cornell University Library The original of tiiis book is in tine Cornell University Library. There are no known copyright restrictions in the United States on the use of the text. http://www.archive.org/details/cu31 9240041 31 391 North Carolina Board ofiiEAtf^ Sanitary Engineering. SECOND EDITION. By WILLIAM OAIN, O. B. Member of the North Carolina Board of Health. KALEIGH : P. M. HALE, AND EDWAKDS, BEOUGHTON & 00., State Printers and Binders, ISSO. /cornell\ university UBRARY^ SANITARY ENGINEERING. SECOND EDITION. By ■VV'ir.LI^M: CA.IN, C. E. CHAPTER I. GENEEAL CONSIDERATIONS. Death rates lowered by sanitary works.— We are told upon the best authority that in England there occurs annually upwards of four million cases of preventable sick- ness; and that 125,000 persons are premature cut off every year from a neglect of sanitary precautions. Now if this be true in a country which has adopted the best known sanitary precautions, at great expense, how much more significant will the records in this State appear, where the only outlay that may be classed under the head " sanitary," is generally made in meeting doctors' bills and fwneral expenses. It is further stated thait in England, since the sanitary precautions have been instituted, that the death rate has been lowered by from one-fourth to one-third, and is besides decreasing from year to year. The following table, refer- ring to a jew localities in England, taken from Latham's " Sanitary Engineering," speaks more forcibly than all the other arguments that may be presented, especially to those who have paid but little attention io sanitary subjects, and are inclined to be skeptical as to the great actual saving of life that may be attained. I presume the table is made out SAKITARY ENGINEERING. for 1873, the date of the publication, and that the " works " are of the " water sewerage " kind : Name of Place. Banbury,.... , Cardiff, Corydon, , Dover , Ely Leicester, Macclesfield, Merthyr, , Newport, Kugby, Salisbury, .... ■Warwick, ..., Population in 1861. 10.338 32,954 30,229 23.108 7,847 68,056 27,475 52,778 24,756 7,818 9.030 10,570 ^ o n oS.2 - a> t- S o tJB j; o fe "^25 23.4 33.2 23 7 22.6 23.9 26.4 29.8 33.2 31.8 19.1 27.0 23.7 is- SCO a ft s ° -^^.a a o a 20.5 23.6 1S.6 20.9 20.5 35.3 23.7 26.2 21.6 18.6 219 21 12J .32 22 7 14 20 18 32 ^ 20 n a > ur as two or three people. It is true that the gas gives ofif no organic impurities, but if not burning brightly the poisonous carbonic oxide is always formed- If we adopt 6 volumes in 10,000 as the safe limit of the amount of carbonic acid to air, then it follows that for every man or lamp or two candles in a room, we must sup- ply at least 1,000 cubic feet of pure air in every hour to dilute the A cubic foot of carbonic acid formed- A gas jet will require two or three times as much pure air. But since the admitted air contained carbonic acid, we must supply more air to not exceed the maximum adopted : thus if the admitted air contain three volumes in 10,000 of carbonic acid, we must admit 2,000 cubic feet for every per- son, since the 6-10 of carbonic acid admitted, added to the 6-10 expired per hour, gives the ratio of 12 to 20,000 or 6 to 10,000 allowed. It is said by some, that experience in hospitals shows that from 2,000 to 3,000 cubic feet of fresh air should be admit- ted every hour for each individual } whilst again we are told that for a healthy person in a barrack room 1,200 cubic feet per hour will suffice, and that the vitiation, tested by the sense of smell, for hospitals is not perceptible when somewhat less than the 2,000 to 3,000 cubic feet are pro- vided. No fixed standard has thus been agreed upon. In fact, it doubtless varies with the climate and the health of the person. The Laplander can breathe impure air better than we, probably because the organic impurities thrown off by him are not so readily decomposed as in our warmer air. The carbonic acid formed by combustion and respiration being heavier than air at the same temperature, would sink to the floor ; but in consequence of its high temperature, it first rises to the ceiling ; so that as much as 60 to 70 parts of it in 10,000 of air has been found at the top of an ordinary sized room in which two people were sitting and three gas VENTILATION, 21 jets burning. At the same temperature, however, we should expect to find the largest amount of it at low elevations, thus vitiating the lower strata of the atmosphere, or room, very greatly. Fortunatelj'^, however, gases have the power of " diffusion," so that a heavy gas will actually rise to mix with a lighter gas; further, it will pass through membranes and thin plates of stucco to effect the same object, so that the amount of carbonic acid is not generally a function of the elevation of a localitj'. Where a room has no flue or chimnej^ to keep up a con- stant circulation, then openings should be provided near the top of the room to let the warmer impure gases out, and not let them cool and descend again to vitiate the air we breathe. Vitiation by Perspiration. — In addition to the carbonic acid given off by the lungs and skin of a iran, there is ex- haled a considerable degree of moisture, generally loaded too with organic matter, which produces smell. The amount has been estimated at from 1.5 pounds to 2.5 pounds per day on an average. A high temperature, or exercise, causes greater perspiration, thus cooling the person somewhat. The amount of moisture given off is considered by some in connection with the carbonic acid exhaled, to ascertain the iheoretical amount of air to admit; but this theoretical amount for most houses is larger than healthy persons seem to require, according to certain experience. This is account- ed for by the fact that opening doors and windows, es- pecially if they are kept open for some time, the draft through cracks, &c., add very much to the volume of ad- mitted air, though not considered in the computation. Lime as a Purifier. — If a house has been lately plastered or white-washed, the lime will, at first, take up the carbonic acid with avidity; so will any ordinary mortar; in fact, I have seen artificial stone made by passing the products of combustion of a stove (carbonic acid mainly) by a flue into a room where was placed the mortar, moulded into the re- 22 SANITARY ENGINEERING. quired form. The lime of the mortar changed to carbonate of lime, which cemented firmly the grains of sand into a hard rock. It destroys organisms to whitewash. It would seem, there- fore, that a plastered wall whitewashed was better than either the "hard tinish" or papering. The accumulation of filth in successive coats of papering in old houses is probably frightful. Most of us have seen the trunks of trees white- washed. This seems to me a misdirected effort to promote health. Why should such indignity be practiced on our noblest growths, stopping up the pores of the bark and probably injuring the tree, in order to remove a little car- bonic acid out of doors, where it is not in excess? The Leaves of Plants as Purifiers. — The carbonic acid thrown off into the air by decomposition, lighting, heating and the breathing of animals, is taken up by the leaves of growing plants, where it is decomposed, by aid of the sun's rays; the carbon being appropriated to help make woody fibre, &c., and the oxygen being given back to the air to fit it for respiration. We cannot imitate this process in venti- lation schemes, but have to resort to heated currents or to fans to expel the foul air from our rooms and leaye it to nature to carry the foul air by the winds to her millions of laboratories and return it to us pure. If there was no vege- table growth, however, it has been computed that the breathing of animals would not vitiate the air perceptibly, over the whole globe, in some thousands of years. Limit to Ventilation Schemes. — It is impossible to change the air, iidth comfort, in a room, as often as the winds do, out of doors; but we can easily prevent the air in the rooms from becoming too impure to breathe. Even when there is no special attention paid to ventilation, it is found that the hotter inside air is going out continually, thi-ough every possible outlet, and cool fresh air coming in to take its place. In very open houses, ventilation is often secured VENTILATION. 23 by the poor construction, in spite of the inmates, but it is often at the sacrifice of comfort. Ventilation by the Open Fire-place. — Let us now con- sider one method of supplying pure air to a room contain- ing an open fire-place. A fire must be kept brightly burn- ing in the fire-place, to heat the air in the chimney or flue, causing a difference of pressure in the external and internal air, so that the out-door air rushes in through every crack and crevice, even through the solid walls, and thus forces the foul air up the chimney. It is found, however, by experience, that the openings mentioned are not generally sufficient to admit a sufficient volume of pure air. Hence our custom is, at intervals, when headaches or debility are experienced, to open the doors or windows " to let in a little fresh air." A wise pre- caution certainly; but it does not meet the whole case, for air should be admitted without draft — i. e., without the influx of sharply defined cold currents, which, as is well known, produce colds, with their attendant evils. The problem has been solved, however, in several ways, the details of which are simple in the extreme. Thus, if the lower sash of the window is raised a few inches and the opening belo^is4t is completely closed by a strip of plank, there will still remain an opening between the sashes where they overlap, through which the air will pour, being necessarily directed upwards. It thus strikes the ceiling, and is then gradually diffused through the room without draft. A common expedient of simply lowering the top sash al- lows the cold air to " trickle down" on our heads. In the latter case, however, a board may be placed at an inclina- tion against the upper part of the sash, so as to give the en- tering current an upward direction. Either of these plans is liable to failure when curtains or blinds are used. So that a more generally applicable method would consist in boring holes through the upper 24 SANITARY ENGINEERING. part of the doors or walls, and giving the entering air an up- ward direction by means of inclined planes of some kind ; or tubes of wood or iron may be passed through the walls and turned directly upwards on entering. They should ex- tend to at least 7 feet above the floor. The air in all cases should be drawn directly from out- doors, and not from passages or other rooms. The open- ings, moreover, should admit of being partially or entirely closed on very stormy and windy days. Ail of the above plans have been tried in dwellings, club rooms, etc., with complete success. The proper size of tube or opening to use must be deter- mined by experience. Two tubes, of two inches diameter each, may be tried for an average-sized room for two per- sons. It is stated that "two square tubes, 5x5 inches, will keep a good-sized club-room fresh." Now, this method of ventilation is dependent upon a fire being maintained at the lower level of the room to cause the currents to enter with sufficient velocity. The system fails in summer; when, however, we do not object to the draft caused by opening the doors and windows. Known Properties of Air. — The mathematics of this branch of the subject, (which is not given, as it seems out of place here,) depends upon certain known properties of air which may be briefly mentioned. Thus 12.4 cubic feet of air weighs 1 pound, when at a temperature of 32° P, the barometric height being about 30 inches, the average pressure at the sea level. Since air is compressible, (its volume varying inversely as the pressure,) it follows that as we ascend, the weight of tlie same volume of air becomes less, since there is less air above us than before, so that the same weight of air is not compressed into so small a place. Air likewise expands or contracts 1-491 part of its volume for each degree Fahrenheit above or below the frezing point, the pressure remaining the same; so that 491 volumes of VENTILATION. 25 air at 32° becomes 499 volumes at 40°, 509 at 50°, 519 at 60°, 529 at 70°, 539 at 80°, and 549 volumes at 90°, whilst the 491 volumes at 32° F. become 479 at 20°, 469 at 10°, and 459 at 0° Fahrenheit. Again, it is found that one pound of air can be raised 1° F. by the same amount of heat that will raise 0.2874 lbs. of water through one degree, the air being subjected to con- stant pressure. From such data, in connection with the heat afforded by different fuels, and the laws affecting the flow of gases, we are enabled to compute the velocity of the air flowing out of the chimney, which is thus a measure of the inflow of the fresh air. Suffice it to say that the higher the chimney or flue the stronger the draught, as thereby the difference of weights of the heated air in the chimney and a similar column outside the chimney is greater. Ventilation by Gas Jets. — In theatres and closed halls, a series of gas jets may be used to create a current, the heated air passing outdoors through flues placed directly over the gas jets. It is stated that this plan has met with great success in two churches in New York, the size of one of them (Dr. Scudder's church) being 150x100, of the other (Dr. Hep- worth's) 125x125 ; the first seating 2,200 and the second 2,400. There were 14 to 20, 12 inch round tin pipes, carried up in walls from near the floor to and above the roof. In each of these tubes was placed three gas burners, just above the registers that admit air from the outside. On simply heating some of these gas jets, the registers being opened the proper amount, there is caused a quick exhaust, under complete control, and an inflow of pure fresh air. There i? an opening in the centre of the ceiling of the auditorium into an octagon shaped shaft 11 feet in diameter in one church, 16 in the other, extending above roof, containing sashes and outlets to the outer air. Gas jets are placed under tubes in these shafts to increase the current. At other parts of the ceiling are similar shafts, etc. The nu- 26 SANITARY ENGINEERING. merous gas jets produce such a current that, in warm weather, the entire air of the church can be changed every five minutes. The churches are heated by hot air furnaces or steam coils. (See "Plumber and Sanitary Engineer," March, 1879.) Ventilation by Fans. — Still another method of ventila- tion is by pumps and fans. Most generally, air is drawn from without by fans located in the basement, and is pro- pelled along ducts — over steam pipes or furnaces, if it is to be heated — to openings into the various halls and rooms, from whence it escapes by suitable openings, generally placed in the roof. The air is often drawn from near the ground, but it is best, especially in densely populated cities, to draw the fresh air from a point 100 to 200 feet above the ground down vertical shafts. In Paris, the air is drawn down a shaft 180 feet in height, to supply the Assembly room. (See Appendix III for a description of the ventilation of the N. Y. Lunatic Asylum.) Good Effects of Ventilation. — It is evident how im- portant a factor of health ventilation is in crowded school rooms ; in fact in all places where crowds may congregate and speedly vitiate the air. The bad effects are everywhere admitted. The good effects of the systems proposed have been proved by mortuary statistics, especially in school houses and hospitals. In a Dublin hospital, in 1783, for ■ 25 years when the ventilation was bad, 3,000 out of 18,- 000 children, born there, died within the first fortnight of their birth. With better ventilation in the succeeding 28 years, 550 died out of every 15,072. The report of 1861 states that further improvements in ventilation have been made, and deaths from the " nine-day fits," which carried off most of the infants, was then almost unknown. The records concerning ventilation in connection with lung diseases is equally striking. Such diseases thrive in cities where the smoke resulting from the burning of coal VENTILATION. 27 is charged with impurities, such as " hydrocarbons, sulphide of ammonium, carbonic oxide, and probably very minute quantities of arsenic." Even now the cry is going up from London for a purification of its atmosphere from smoke. This gvil we do not suffer much from in North Carolina, the population being scattered and the cities small. But we need a thorough inspection of public buildings with a view to proper ventilation. When it is known that 30 parts of carbonic acid to 10,000 of air is often found in theatres and public halls, which is five times the admissible amount, it will be admitted that reform is needed. Cubic Space Allowed. — The amount of space per head allowed in the room by various authorities, varies from 300 to 1,000 cubic feet, the amount being smaller when the room is only occasionally filled with its maximum number. It is true that the air can be changed in a small room more frequently than in a large one to maintain the proper degree of purity or rather impurity, but the increased draught may be objectionable. The amount of space act- ually given -per head in various school houses varies from 70 to 100 to 200 cubic feet. The effect is that 12 parts of car- bonic acid in 10,000 (double the admissible amount) is com- mon, and even 20 and 50 parts are not unknown. The effect upon both teacher and pupils is of course, headaches, listlessuess and debility. Lighting. — The proper lighting of school rooms is as necessary as ventilation. The light should come from 6e- hind the pupil on to the book or blackboard, when possible, and the windows should be high, as most of the available light comes from above the level of our heads. Lighting directly from the top is probably the most efficient means of all where practicable. The light should come mainly from one side — the side opposite the blackboards — and the pupils should sit with their backs to it. The desks should be at such heights that the book or paper, &c., shall not be 28 SANITAKY ENGINEERING. too near the eyes, so that the tendency to near-sightedness may be prevented. This defect is becoming alarmingly prevalent, and the teacher should insist upon the pupil reading with the book at the proper distance to suit his vision, at all times. Useful Hints. — Finally, let it be impressed upon all that the sense of smell when coming from outdoors into a room should warn us when our rooms are foul, and that doors and windows should be opened when convenient, and articles of clothing and bedding should be aired frequently to purify them. Also let it be remembered that even brick walls can trans- mit gases. "Pettenkofer got 2,650 to 3,320 cubit feet of air through the brick walls and crannies of his room, when the difference of temperature inside and outside was 34° F. When all the crannies had been carefully stopped up, 1,000 cubic feet per hour still came through the walls." There- fore never allow filth about any room or cellar of the house, nor against the outside walls, for such filth will contami- nate the air that comes into the room, and has been found to cause sickness. If the house is liable to such contagion from adjoining buildings, endeavor to make it as air tight as possible, after providing for the admittance of the purest air that can be obtained through proper openings. The floors of all houses should be as tight as possible. Heating. — Intimately connected with ventilation is heat- ing; in fact the two have generally to be considered to- gether. In cold weather we require more heat than our bodies generate to make up for the loss by radiation ; at the same time we need fresh air to breathe. How admirably are these two conditions realized around a good camp fire, on a still, cool night! The active worker has just enjoyed his hearty meal, as only a worker can, and with feet stretched to the fire — that heats him by direct radiation — and body well clad, inspires the cool, fresh air of the country thdt invigorates body and mind. VENTILATION. 29 Cool air to breathe is as refreshing as cool water to drink, whilst air too warm may be compared with tepid water in its effects. This fact is universally admitted, and yet it has got to be the fashion, at the North especially, to heat houses by puffs of hot air from furnaces that would seem more properly in keeping with a drying house. Let us under- stand clearly the physical differences in the various methods of heating, and we can then form a more intelligent judg- ment as to the merits or demerits of each particular device. The open fire heats solid bodies in front of it, by direct radiation of heat raj's, which pass through the intervening air with scarcely any loss. Tyndall has shown that air, consisting simply of oxygen and nitrogen, intercepls but an extremely small number of heat ra3'S passing through it. The aqueous vapour, found in all air, intercepts 20 to 100 times the heat that pure air does. Carbonic acid, per- fumes, etc., increase the absorption of heat by air. The water gas in the atmosphere, although constituting only, say ^ per cent, of it, yet intercepts nearly all the heat rays of the sun that do not reach the earth ; and again prevents their too rapid radiation at night from the earth. As Tyn- dall says, " Aqueous vapour is a blanket, more necessary to the vegetable life of England than clothing is to man." The amount of heat, however, intercepted by the air be- tween the fire of a room and solid objects in front of it, although small, yet does increase the temperature of the air somewhat, though it is usually neglected altogether. The air of the room is mainly warmed by " convection," from coming in contact with the solid objects that have a higher temperature ; the air next the solid body being heated first, then rises, to be replaced by other air, which operation is repeated indefinitely, or until the whole mass is heated to the same temperature. There is thus a continual circulation of the air in a room heated by an open fire place, and generally an eflBcient draught to keep the air from being too much fouled. 30 SANITAEY ENGINEEEING. If the room is heated by steam or hot-water pipes, the case is different. The direct radiation is small, as any one can test by trying to warm his feet at the pipes without actual contact. The warming is mainly effected, as in the case of STOVES (not over-heated) or hot-air furnaces, by the air being warmed, by the heated pipes, stoves or furnaces, by convection, and this air by its circulation heats the room and its occupants. The air is thus warmer than the furni- ture in the room ; whereas in heating by the open fire-place, the furniture, etc., is ofteji warmer than the air. A person in the room would thus be continually radiating heat, un- less the air was too warm for comfort. In addition to the objection to the warm air, per se, it has been previously ex- plained that heating air causes it to become too dry; so that whilst the " relative humidity" out of doors may be 80, in doors it may be much less — a disproportion that cannot be conducive to health. In fact, asa writer humorously remarks, such drying houses " are drying the very flesh off the bones of the Americans." Still, in large buildings it is generally impracticable to heat by direct radiation, and the inmates have to submit to be dried. Again it is stated that the rigor of the Northern climate. requires that the air, even in dwelling-houses, be heated somewhat before being admitted, If so, then it is still practicable to heat it only to 50° or 70° F., and supple- ment with the open fire-place. Summary of Modes of Heating in the Order of Merit. — We shall conclude this popular exposition of the subject by a condensed summary of the various modes of heating in vogue, in the same order of merit as that given by Prof. Fleming Jenkin, in " Healthy Houses" (Harpers Half Hour Series), a book that every one should have. The open fire-place is best, although most expensive, as it heats by radiation, and secures ventilation. Next follow, in the order of descending merit, hot water pipes, porcelain stoves, hot air pipes, cast iron stoves, and VENTILATION. 31 last and worst gas-stoves with no. chimney. These pipes and stoves heat largely by convection — i. e., by heating the air next to them, which rises and is difFased through the room, the cold air taking its place to be in turn heated, &c. Iron stoves, especially when over-heated, emit a bad smell, supposed to arise from the charring or decomposition of or- ganic substances in the air by their contact with the heated sides of the stove and pipe. Moreover, if the stove is red hot, the poisonous carbonic oxide and other gases will pass through the red hot iron and thus enter the room. The air is charred and dried too much b}' iron stoves. The porce- lain are far preferable. Hot air pipes are better, and more- over distribute the heat more uniformly; though if the fur- nace becomes red hot, poisonous carbonic oxide will pass into the pipes. Some describe the "hot air" as having the " life taken out of it." Hot water pipes are better than hot air pipes; the air is not over-heated, and a uniform temper- ature is preserved for a long time. It is much used in hot- houses, baths, drying-rooms, etc. Exits must be provided for the foul air where the hot-air system, the water pipes or the gas-stoves are used. For comfort and cheerfulness, no device can equal the open fire- place, fed with coal, or oak and hickory wood, not ignoring either the historic pine. The fresh air then comes in through the, walls, tubes, etc., cold, with plenty of oxygen and perhaps ozone in it, and is gradually diffused through the room as it becomes heated, to give up the proper amount of oxygen required for respi- ration and combustion. What excuse can there be for close rooms, that breed debility of various kinds, when pure, fresh air can be obtained by us at such a small cost ? 32 SANITARY ENGINEERING. CHAPTER IV. WATER SUPPLY. All of our supplies of water are derived from rainfall, part of this rainfall evaporating again, part running off into the streams and thence into the ocean to be again distilled and sent back to us as clouds and rain, and part sinking into the earth and forming the small subterranean streams virhich furnish the water of our springs and wells. In run- ning over or through the ground, this water takes up such salts as it meets that are soluble. Some of these, together with the air and carbonic acid dissolved, giving the pleasant taste to our usual potable waters. Other salts and gases, derived from decaying organic mat- ter — dead bodies, manure, filth, etc. — are harmful in the highest degree, and have bred mischief and death in innu- merable cases. The rain as it leaves the clouds is pure water generally ; but in falling to the ground, it not only carries with it me- chanically much organic matter and dust that is floating in the air, but it dissolves various gases, as oxygen, nitrogen, carbonic acid and ammonia (the usual constituents of the atmosphere) besides nitric acid (often formed in the air by the lightning's flash), and in the vicinity of manufacturing towns, the gases evolved in tlie processes used in the partic- ular manufacture. Water readily dissolves certain gases. On simply shaking it up with air, the latter is readily dis- solved. This principle is made use of in aerating the pure water, that has been distilled from the salt water of the ocean, on board ships, thus making it drinkable. The amount of oxygen, nitrogen, carbonic acid and am- monia commonly found in waters is small, particularly the ammonia; which last, it may be observed, water can dis- WATER SUPPLY. 33 solve in large quantities. All of these gases are easily ex- pelled by simply boiling the water. Rain water generally contains far less organic metter than river water. River waters, though, differ greatly in the amount and character of the matter, in solution and sus- pension, as regards potability. Thus, if water drains over an impervious stratum, as a granitic formation, the water is apt to be soft, and to contain but little solid matter in solu- tion. Some waters of this character contain only from three to five grains of solid matter to the gallon ; they possess a high solvent power on lead and iron pipes, but are other- wise of the best character. Where the rocks consist largely of carbonates of lime or magnesia, the waters are apt to be hard, their action on leadi and iron pipes is small, and they require a greater expendi, ture of soap in washing, but are not otherwise objectiona- ble, unless the carbonates are greatly in excess. It is stated that the health and physique of hard water districts is better than in soft water districts ; the water fur- nishing an abundance of material needed in the formation of the bones. Each " degree of hardness " {i. e., each grain of chalk or sulphate of lime, dissolved in a gallon of water) will entail, however, the additional use of two-and-a-half ounces of soap for every 100 gallons of water ; so that it is well to get rid of the carbonates in solution, if possible. This may be partially effected in two ways ; either by boiling the water, or by adding milk of lime. Both methods depend on the fact that water can dissolve only two grains per gallon of. carbonate of lime, unless it contains carbonic acid in solu- tion, when it can dissolve very much more. Boiling expels this acid; thus reducing the amount of carbonate of lime in the water in solution to, at most, two grains per gallon. By the second, called " Clarke's process," the added lime-water combines chemically with all the free carbonic acid, forming carbonate of lime, which thus settles- 8 34 SANITARY ENGINEERING. to the bottom, together with much of the original carbonate of lime, leaving only about two grains per gallon still in solution of carbonate of lime. The milk of lime is made by shaking up a small quan- tity of quick lime in water. Permanent hardness of water is caused hj the presence ■of sulphates of lime and magnesia. Neither boiling nor ■Clarke's process can soften such water. Wells and Springs. — Where wells or springs are used as the source of water supply, great care should be taken that the surface in their vicinity be kept free from organic mat- ier, which by oxidation and putrefaction readily forms solu- ble nitrates, ammonia and chlorides. Such waters are often clear, pleasant to the taste, sparkling from the excess of carbonic acid and cool from the effects of the nitrates. Hence the senses cannot be relied on, without the aid of a .chemical and microscopical analysis to decide whether our well water is fit to drink. Even when all filth, slops, etc., are removed to a distance, we can only infer that there is no probable contamination. The geological structure — stratification, faults, character of the earth, etc. — should be studied in this connection. Thus it was found in a certain locality that wells very near a grave yard gave good water, whereas wells on the oppo- site side, several hundred yards off, in the direction of the ;dip of the strata, were polluted to a dangerous extent. The explanation is simply that water has a tendency to flow along the planes of stratification, where the strata are well defined. Numerous cases of fever, cholera, &c., have been traced to bad water; localities with wells situated on the subter- ranean current that flowed past the diseased refuse, cess pool, etc., being attacked, whilst neighboring localities were free from the epidemic. It is needless to specify particular instances. Let no wells be placed where kitchen refuse, jslops, manure or any kind of fecal matter can drain into WATER SUPPLY. 35 them. Where no stratification exists, tiien, if possible, place the well two or three times its depth from any offend- ing matter. A well can just as properly be dug next to the house as elsewhere, provided slops and kitchen refuse are emptied some distance from it. In one instance soapy water was found by analysis in one well, whose sparkling waters would never have suggested it. The whole of the slops of the establishment were thrown where they drained .directly into the well. It must be carefully borne in mind that the well is the point of least resistance to the numerous little streams en- tering it and that it may induce a flow from a considerable extent of the surrounding earth. Chemical analysis can alone show if some of these little streams have been pol- luted ; in fact, whether a well is the drainage receptacle of the filth on the surface or of the rotten cess pool — the dis- grace of any land where it is found. It is not intended to convey the idea that, before wells are dug, the underground water is necessarily flowing in little streams. On the contrary it is generally otherwise, particularly in very absorptive strata. Very hard rocks, of course, hold but little water, except in the crevices, whilst very porous and absorptive strata, as the London chalk, are fully saturated with water from near the surface downwards and only need tapping to afford it in large quantities. The water thus contained in the ground is known as the " soil " or " ground " water. Where the earth is porous, absorptive and uniform in character, much more of the rain water passes into the ground to flow off along subter- ranean channels to some outlet, to appear at the surface again as ^rings, or to be pumped out of wells — than where the surface is more impervious. The imaginary line connecting the water level of springs and wells (when not used) is called "the line of saturation." It has been found that in uniform earth this line of satura- tion generally rises with the ground, so that generally as 36 SANITARY ElNGlNEERING. we recede from the sea-coast, or a stream, the water level of the well rises, whilst its depth beneath the surface increases. This rule is often true even when there is a want of uni- formity in the strata or in the configuration of the ground> though so much depends upon the inclination the beds have, and their relative permeability, that it is impossible to lay down any precise rules as to where water may be struck in any but the simplest cases. This is still more evident if the rocks are contorted, fis- stired or faulted. Some special eases may be given however. Thus if a porous stratum overlies an impervious one, the water de- scends through the former until it reaches the latter. Now as the lower stratum is level, or slopes towards its outcrops, or is depressed in tlie middle, the water which soaks through the porous stratum will eventually appear in the form of springs near the upper line of the outcrop of the lower stratum, or be mostly stored in the depression mentioned of this stratum. Unless the porous stratum is very shallow, wells may be dug in it, especially in the last case mentioned, with the expectation of getting a good supply of water. Where the porous stratum is covered ^by an impervious one, it holds less water than in the previous case, for it now receives no water except along its outcrop. Where such porous strata, however, are of great extent and have a considerable outcrop (it may be in remote dis- tricts) a good supply of water may he expected. In the latter case, if the porous stratum is again underlaid with an im>pervious one which is depressed in the middle, large quantities of water will collect in this basin under considerable hydrostatatic pressure. If this pressure is sufficient to send water to the surface through a well hole, the result is an artesian well, which wells are much re- sorted to in some couatries. In this State we need have no fearsof a water famine if th& various sources are utilized. In the Quartersary sand Of WATER SUPPLY. 37 the eastern portion of the State, wells only 15 feet deep are common, though the underlying Tertiary marls and older rocks may cause exceptional features. In the middle and western portion of the State, the rocks are sandstones, slates and various crystalline rocks, which are often fissured, faulted, contorted or intersected by trap dykes ; thus caus- ing abnormal features : still, as the dip except in the sand- stone formation is often considerable, there is not generally much difficulty in finding water on digging for it; so that the " diviner " with his witch hazel twig generally finds his predictions verified. Perhaps it would be the same if he did not invoke its mysterious powers to assist him ! In the older rocks, the water often collects in fissures. Instances are known where pumping from one well affects a remote one ; whilst, on the other hand, owing to faults, dykes, change of dip, etc., wells very near together seem to have no connection. As a rule, the wells are deeper in the older rocks ; for, as the latter are more impervious than the sands of the later formations, less water is absorbed by them — more running off into the streams — therefore we should naturally expect to go deeper for a constant supply. Other things being equal, the deeper the well the purer the water, as it has filtered through a greater extent of earth. The earth is thus a vast sponge, ready to afford water when tapped, that is generally of a better quality too than lake or river water in the vicinity. Prof. Nichols (see " Filtration of Potable Waters,") has observed, that even when the well is situated near a stream, that " the water is generally clear and colorless, of a nearly uniform temperature, and differs in chemical character from that of neighboring streams or ponds, generally being some- what harder." On lowering the level of the water in such basing by pumping or otherwise, the ground water level is lowered next the basin to the same extent ; but it is found that as 38 SANITARY ENGINEERING. we proceed from the well or basin, that this level is lowered less and less, until we reach a point which is not aflfected when the level of the water in the basin is kept at a certain minimum height, the friction and capillarity balancing gravity here ; supposing always the rain fall not subject to much variation. In case of drought, of course the whole ground water level would be lowered. As an illustration of the above principle, it was found on the Elbe, that when the water in a well, dug in an alluvial deposit, was kept constanly 8.2 feet below its normal level, that the height of the ground-water was affected in every directinn for 200 feet only. Large basins, near streams, are often used as the source of water supply of whole towns. Now it is evident that if the water level is lowered in such a basin that since the water level in the intervening bank is lowered, that the river water will have a tendency to flow towards the well to make up the deficiency, unless the bottom and sides of the river have become coated with clay to such an extent as to be impervious, which is very apt to be the case unless the stream is very clear, or has a rapid current. Known ex- amples seem to show little or no contamination from the river water when the basins are built 100 to 200 feet from the river. The basin is constructed next a stream, as there is apt to be a greater flow of ground water there ; besides the water in the stream can make up any deficiency by use of proper constructions. Filtration. — This natural filtration of water through the soil, when the latter is good, is more efficient than any sys- tem of ARTIFICIAL FILTRATION, which, when practiced on a large scale, generally consists in passing water through layers of sand and gravel about six feet deep. The finest sand is put at the top, the upper portion of which catches most of the suspended matters, and by the oxygen con- densed in its pores, frees the water of a small portion of its organic matter. WATEK SUPPLY. 39 As the sand becomes clogged, it is scraped off at top ai{d fresh sand added. It is well not to cause the water to flow through the filter at a rate greater than fifty gallons per square foot of surface per day. The water is usually several feet deep on the filter bed. The beds are scraped about a dozen times a year, oftener in summer than in winter. When possible, it is best to construct settling-basins where the water can deposit much of its sediment before passing on to the filter beds. In some rivers, the particles of clay in suspension are so fine as to readily pass through sand and even filter paper. In such cases, charcoal pounded fine is the only resource. The action of a sand filter is two fold, mechanical and chemical: 1st. Mechanical, in that suspended matters too large to pass through the pores of the filter are caught, as in a net ; likewise much sediment that would otherwise pass through sticks to the grains of sand, due to the property of adhesion. 2nd. Chemical, for although sand filters have practically no action on dissolved mineral matter, yet an appreciable quantity of organic matter in solution, particularly certain kinds, are removed by filtration through them. An experiment that any one can perform will illustrate this : Add a few drops of sulphate of indigo solution to some clear water ; the water assumes an intense blue color, Mhich color it retains on filtering through an ordinary filtering paper. But if we strew over the filter paper some powdered charcoal (animal charcoal is best) the water comes through perfectly colorless. If we use earth in place of the charcoal, the water that passes through it ife slightly colored, thus showing that earth is not so powerful an agent as charcoal. Now, evidently, here the earth or the charcoal have exer- cised a different influence from the filter paper alone. The filter paper will catch suspended matter. Thus mudd}' water passed through it may become clear, but it does not alter 40 SANITARY ENGINEERING. chemically the substance in solution. We have just seen, though, that earth or charcoal does, and the usual hypothe- sis to account for this fact is that " porous substances con- dense gases — air, osygen, etc., in proportion to the extent of their interior surface," and this oxygen actually destroys by slow combustion the substance in question. The enormous amount of surface to volume of porous charcoal or piles of earth permits the condensation of a large amount of gas which stands ready to attack any chemical body that can be decomposed or altered by it. Of course this chemical action must diminish the more the longer the filter is in action, as the oxygen is not so readily replaced when the filter is covered with water. If water is really poUuted by sewage matters, it has been shown that it may be improved materially but not perfectly puri- fied by filtration. It is, therefore, pertinent to ask, what amount and kinds of organic matter found in water render it unfit for drinking? Evidently, we must consider the two questions together. Organic matter, per se, cannot always be deleterious, other- wise soup would have to be ranked as poison. It is stated that the waters of the Dismal Swamp, saturated with or- ganic matter, is actually preferred by sea-going vessels to purer waters. Chemistry is perfectly able to determine the mineral salts dissolved in water, and medicine can pro- nounce upon the amounts that may be taken into the sys- tem without injury. Chemistry can likewise determine the amounts and kinds of organic matter in any water, and if the source is known to be bad, or the organic matter (espe- cially the albuminoids) in excess over good potable waters in the vicinity, the chemist is able to form an intelligent opinion, at least as to the " possible amount of germ " or disease producing power of the water. London drinks Thames water principally, though "above the point where the supply is abstracted the river is contami- nated by the excrements of more than 200,000 human beings." WATER SUPPLY. 41 Those who favor this water, claim that a polluted river purifies itself in its onward flow, the noxious matter being oxidized as it is tossed to and fro by the current and thus rendered innocuous, besides being more and more diluted. Again, fish eat fresh fecal matter, and vegetation can ab- stract large quantities of it. Still, it is doubtful if this nat- ural process is continued long enough to thoroughly destroy the hurtful part of the sewage. Now can this Thames water be regarded as a fit source for water supply, having once been contaminated to a cer- tain extent ? " The noxious part of sewage is that which is held in mechanical suspension, and these globules are be- yond the reach of the chemist, and, to a great extent, of the microscopist. There are only two processes by which it can be effectually removed ; the one is boiling for a long time, and the other is by distillation, both impracticable on a large scale." " No process of filtration that has yet been devised will remove choleraic dejections from water." (Hum- ber's Water Supply, p. 19.) The organic matter is not then considered as fatal in itself, but as dangerous, when of certain kinds, as affording a refuge and breeding ground for the poison germs that attend an epidemic. A person may drink even diluted sewage with but slight inconvenience until this germ is once planted in it, when at ohce his beverage changes to a rank poison. Whether we accept the germ theory or not, it is admitted that drinking foul water and breathing impure air debili- tate the system and thus render it less able to withstand epidemics. Let us then follow the natural instincts and avoid polluted air and water, especidly as North Carolina can afford the pure articles in such abundance. Lead Poisoning. — There is one source of poisoning that may be considered by itself — lead poisoning, due to the use of lead cisterns and lead pipes. 42 SANITARY ENGINEERING. Soft waters that contain oxygen oxidize the lead and then dissolve the lead oxide formed. Hard waters, containing free carbonic acid, form, on the contrary, carbonate of lead, which is only soluble to the extent of one part in seven thousand, unless there is much free carbonic acid present. Clarke's softening process lessens the action of water on lead. Peaty matters form a sort of protecting coating on the lead pipe that is very eflScacious in preventing further action on the lead. One-tenth of a grain of lead per gallon of water may produce lead poisoning in time. The presence of lead in water is easily detected by passing a current of sulphuretted hydrogen through a deep column of the acidified water. If the liquid becomes tinged of a brown color, it is due to the formation of lead sulphide. What is the remedy if the water is found to act continuously on the lead ? Simply abolish the lead cisterns for slate, or stone ware, or galvanized iron cisterns, and replace the lead pipes by wrought iron pipes with screw joints. The tin lined lead pipe has not proved satisfactory ; a small flaw exposes the lead, a galvanic action between the two metals is commenced and the water is speedily poisoned. It is of the greatest importance to observe that no cistern or water pipes should be placed where sewer gases may pass either through or over them, in contact with the water, since water is very absorbent of such gases. Cistern Water. — Where rain water is used as the source of supply, it is collected from the house roofs and stored in cisterns of wood or brick in cement. The cistern, if of wood, should have a circular form ; if of brick, any convenient form can be used, provided the earth is well rammed behind the walls, to enable the latter to withstand the outward pres- sure of the water. The cistern should be covered and ven- tilated. The rain water as it descends brings down many impu- rities from the atmosphere, such as soot, acid fumes, oil, etc., particularly in the manufacturing centres; besides if or- WATER SUPPLY. 43 ganic impurities in the shape of dust, such As horse ma- nure, etc., cover the roof, the watter is further contaminated before it reaches the cistern. The character of the roof like- wise, whether lead painted, formed of new shingles or de- cayed ones, etc., must be considered. We thois see that cis- tern water is not necessarily perfect, though it is probably better than well waters, for while it has not had the benefit of the natural filtration of the latter, still it has taken up no new salts from the ground, and has certainly escaped sew- age contamination. Nevertheless, it should be filtered before being used. This is effected in various ways. One plan, when the brick cis- tern is used, is to divide the cistern by a porous wall into two unequal parts. The foul water, let into the larger divi- sion, filters through the porous wall into the smaller divi- sion, from whence it is pumped over the house. The po- rous wall may be made of soft bricks, or of some filtering material, as porous tiles or blocks of animal (bone) charcoal, that may be placed in a frame which can slide in groves and be readily replaced when the filter has become clogged up. The brick wall, although very efiicient at first, becomes clogged up in a few months by solid matter, consisting, amongst other things, of insects, worms, etc.; so that the fil- tration then is rather an injury than a benefit, as chemical analysis has demonstrated. The solid matters that settle at the bottom of cisterns should, of course, be removed when- ever practicable. Domestic Filters. — With regard to domestic filters of any kind whatsoever, it may be observed that the filtering material requires renewal every few months. The following is an extract from the "Sixth Report of the River Pollution Commissioners of England :" " It cannot be too widely known that, as a rule, domestic filters constructed with sand, or sand and wood charcoal. 44 SANITARY ENGINEERING. are nearly useless after the lapse of four months, and posi- tively deleterious after the lapse of a year." " Of all material for domestic filtration, with which we have experimented, we find animal (bone) charcoal and spongy iron to be the most effective in the removal of or- ganic matter from water." " The removal of mineral constituents, and the consequent softening of the water, ceases in about a fortnight, but the withdrawal of organic matter still continues, though to a greatly diminished extent, when the filter is much used, even after the lapse of six months." " We found that myriads of minute worms were develop- ed in the animal charcoal, and passed out with the water when the filters were used for Thames water, and when the charcoal was not renewed at sufficiently short intervals, a serious drawback to its use." The spongy iron is free from this trouble, but the filtered water, especially the first portions filtered, contain iron ; and the softer the water the more iron dissolved. On the whole, it would seem that for hard waters "Bis- chop's Spongy Iron Filter" is best, though the animal char- coal is an admirable material, when renewed every few months. Chemical analysis can alone tell when the filter has ceased action. Both materials (spongy iron and animal charcoal,) remove about the same quantity of "albuminoid ammonia," say one fourth, as a mean of some very careful experiments, (Nichols on Filtration of Potable Water), this substance being taken as the measure of the suspicious organic matter in solution From an analysis by Bischof (Humber's Water Supply) it would seem that the spongy iron (a metallic iron reduced from an oxide without fusion, and hence in a loose spongy state) was a more efficient agent than "magnetic carbide" and "silicated carbon," two other materials that have been used with success. If animal charcoal is used, it should be in lumps in pref- WATER SUPPLY. 46 erence to blocks, though the latter gives good results. An admirable filter, that may be used in any cistern, consists of a metallic vessel with a perforated bottom, filled with an- imal charcoal and having a pipe leading from the top, which must be below the level of the water in the cistern. The water of the cistern passes up through the perforated bot- tom, then filters through the charcoal and is drawn off by the pipe when it is needed. The advantage of this ar- rangement is this: the suspended particles are caught most- ly at the bottom of the filter and may become detached from the filter, especially if water is forced through it from the top in a downward direction at intervals. The filter can of course be taken out at any time and the material aerated or renewed. Many other materials have been used for filters of small size — sponge, sand, cotton, flannel, earthenware, common charcoal, etc. The small size filter acts simply as a strainer in a short time, and requires frequent renewing, otherwise it is worse than useless. Makers of all kinds of filters, however, do not hesitate to aver that they are self- cleansing, perfect, etc., etc., which, we have seen, is opposed to the best and latest scientific research on the subject. Let the householder be guided by the facts. Where nothing better is at hand, water may be filtered through a box perforated at the bottom, containing clean quartz sand, resting on a plate of porous earthenware or on bricks placed on top of the charcoal. Expose the filter to the air from time to time. Public Systems of Water Supply.— It will probably not be long before our cities will demand purer water than can be supplied by the wells and springs now used; many of them being, without doubt, polluted by the many impu- rities thrown on the surface. This involves a public system of water supply, with its attendant system of reservoirs, fil- ter beds, pipes, hydrants, etc. In view of such contingency, it may not be out of place to mention some of the require- ments that fluch a system should fulfill. 46 SANITARY ENGINEERIXCi. The water may be obtained from lakes, rivers and streams, springs and wells, impounding reservoirs often being used to collect that which falls on the hill-sides into one place. This water may be conveyed for distribution (Rawlin- son's Suggestions to Local Sanitary Boards, England, p 20,) — " By means of open conduits (before filtration) ; " " " covered* " (always after filtration) ; " " " cast iron pipes under pressure. A water supply may be gravitating, or the water may be pumped by steam power. The relative economy of one or the other form of works will depend on details of cost and quality of water; as a rule, gravitating works require the largest capital. The annual working expenses of a pump- ing scheme may, however, be greatest. Reservoirs for ser- vice distribution should be covered. If filters are used, the water should not be exposed in open reservoirs and tanks after filtration. Cast iron pipes, properly varnished, should be used for street mains. Lead should not be used with soft water, either in service pipes or in cisterns. Wrought iron tubes with screw joints may be used for home service. Water at and below six degrees of hardness is considered soft water ; above this range, water is termed " hard." These " suggestions " of Mr. Rawlinson, (Chief Engineer- ing Inspector to the local government board, London,) are valuable, especially as they represent the best modern thought on this subject, and may tend to prevent fatal mistakes in designing water supply systems. As he says, " The great modern improvement in water supply is the delivery by constant service, and at high presswe, over the entire area of a town, and into every bouse, cot- tage and tenement, and should be secured where practi- cable." The "constant supply at high pressure" permits con- ♦Covered, to prevent the growth of vegetable organisms. WATER SUPPLY. 47 sumers to draw water from the pipes at any time, and can be made so efficacious in the extinction of fires as to dimin- ish their destructive effects most materially. Fire engines are not needed with such a system. It is said that in Paris, owing to the excellent organization of the fire department, that a destructive fire is almost unknown. The "intermit- tent supply" does not offer these advantages. House cisterns are required to stow the daily allowance of water, which is only supplied at certain hours. The cisterns, if neglected, may not be supplied with water, or they may leak, or absorb foul gases, and finally suffer from want of cleanliness. There is, besides the high pressure due to a sufficient ele- vation of the reservoir above the town, the "Holly System" of maintaining this high pressure in the pipes by steam power. The pumping machinery is placed near the water, which ispumped directly into the mains, the pressure being kept constant, or increased or diminished at will. This system is highly spoken of wherever it has been tried. Source of Supply. Available Rainfall. — In any one of these systems, it is a first requisite that the source of sup- ply shall be constant and unfailing. Where a large stream is used as the source, the amount that can be depended on in the dryest seasons may be estimated with some degree of certainty. Where small lakes, springs, wells and small streams are used as the source, we have to depend, more or less, on the observed rainfalls for the different seasons, in conjunction with the measured flow of the streams if any to form, at best, only an approximate estimate of the yield. Such observations should be conducted over a period of twenty years if possible, to include all fluctuations ; but as a rule, in this State, we have only a few years observations of rain fall, and only one or two of the flow of streams to found an estimate upon of the probable yield of water over a given drainage area. Let us suppose that an embankment is thrown across a 48 SANITARY ENGINEERING. Valley, to form a reservoir, into which shall be stored al the water that drains into the valley from its "catchment ground," whose area can be readily computed, as it is bounded generally by well defined ridge lines and the em- bankment in question. Now the yearly rain fall in diflFer- ent portions of the State varies from 20 to 60 odd inches, the average being high, over 45 inches certainly. If all of this could be collected into reservoirs, the amount would be given by simply multiplying the catchment area by the depth of the rain fall ; thus, if the catchment area was one square mile, 27,878,400 square feet, and the depth of rain fall one foot, we should have 27,878,400 cubic feet in a year or 76,379 cubic feet in one day for the supply. But in practice we are very far from securing the whole rain fall, the reason for which can be made plain by the following considerations. Let us first suppose the catchment ground to be imper- meable and free from vegetation; then any rain that falls all flows into the reservoir, except that lost by evaporation; the latter being less as the surface is steeper, the tempera- ture lower and the drainage area smaller. If, however, the surface of the ground is 'perdous, as is usual, then a portion of the rain fall sinks into the ground, to appear again as springs, and thus drain ultimately into the reservoir, or else to pass off by some subterranean stratum to other outlets. In this case the amount lost by evaporation is less as the ground is more absorbent and better drained, the slopes steeper, and the temperature and area smaller. If now we suppose the earth more or less clothed with vegetation, the latter absorbs and partly evap- orates still more water. The conditions of the problems are thus seen to vary greatly for different localities, with the season of the year, and it may be added, also with the winds and relative humidity of the atmosphere. In England, where observations have been conducted for years over many distinct catchment basins, the loss due to WATER SUPPLY. 49 evaporation and absorption, has been found to range from nine to nineteen inches per annum, and it is the prac- tice to consider as available no more than the mean fall for three consecutive dry years, (which is found to be, as a rule, ^ less than the average rain fall,) after sub- tracting the loss by evaporation. Thus, if the mean fall for three consecutive dry years is about forty inches, and if the loss by evaporation and absorption is put at 20 inches, this would leave 20 inches of rain fall that could be utilized if it was all stored. Observations on Lake Cochituate, Mass., water shed of 12,077 acres, from 1852 to 1 875, gave a yearly rain fall vary- ing from 35 to 69 inches — average 50, and the percentage of this received into the lake 25 to 74 — average about 45. It is nevertheless recommended by some good engineers that not over 12 to 15 inches of rain fall be counted on as avail- ble in the United States, which is less than Humber allows. The evaporation from the surface of the water in the reservoir, in dry seasons, averages about ^ inch daily in England, whilst it is as much as J inch in some localities in India. The annual loss in England is put at 20 to 25 inches. It is, of course, much more in small and shallow ponds, which can be more readily heated, than in extensive reservoirs or lakes. Trautwine says that the daily loss from evaporation in the three warmest months of the year will rarely exceed ^ inch in any part of the United States. This is probably too high, for the same authority found in the tropics over a pond 8 feet deep, a loss of only 2 inches in 16 days, or | inch per day. The thermometer reached 115° to 125° in the sun every day. It is evident from the fore- going the importance of early making observations in each locality for as long a period as possible, in order to ascer- tain the ratio of the " available " to the " total " rainfall. Raukine says that this ratio is about 1 for hard rocks, roof surfaces, paved streets, &c., ^ to ^ for pastures, A to ^ for fiat cultivated country, and for chalk. It follows that a 3 50 SANITARY ENGINEEEIKG. catchment basin is best located in the older formations, con- sisting of hard rocks, whilst wells suit best the more previous and recent deposits. London is even now preparing to give up the Thames water altogetiier and to draw her supply from her underlying chalk beds. It is important to note that the most reliable method of .ascertaining the available rainfall is to measure the actual ■discharge of streams that drain a given water shed. Then by comparison with the total rainfall on the water shed, we find the actual amount lost by evaporation and absorption ■of the ground. No town which contemplates a public water supply should neglect to have such observations made, covering a period as long as possible, to take proper account of droughts, &c. Consumption per Head. — Statistics show that in Eng- land the daily amount of water used in the towns and cities varies from 15 to 50 gallons per head — 30 being regarded as a full allowance. In the United States the daily consumption per head varies from 25 to 120 U. S. liquid gallons of 231 ■cubic inches (1 cubic foot — 7.48052 gallons) ; and it is rec- ■ommended by some to allow 40 to 50 gallons per head for smaller cities, and an increasing amount as the population increases. It is very plain, from the records, that an enormous w.aste occurs in our cities, and special attention is now being -di- rected to it. Where inspections, or water meters have been tried, the amount consumed has often been reduced to half and even one-third the original amount. Humber estimates that 20 to 25 gallons is a liberal allowance. Even if we assume double this, it still behooves us to take every pre- caution to avoid waste by the use of meters or otherwise ; else the large yearly cost of the water supply may be need- lessly doubled or trebled. Reservoir Capacity. — Well, assuming, say 45 gallons .the daily demand on & reservoir is made up of the 45 gallons WATER SUPPLY. 51 X number of population, plus the daily evaporation from the surface of the water, plus any compensation water to mill owners or others. Subtracting from this the dry weather flow of the streams discharging into the reservoir, we get " the excess of the demand over the supply " in dry months; and this multiplied by the number of days storage of the reservoir, gives its available capacity^ or the volume it must contain between its highest and lowest working levels. Some advise that every storage reserVbir should, if possible, contain six months of the excess of the daily demand above the daily supply for the dryest consecutive six months. Some English engineers formulate the following rule, as the result of considerable experience; "The number of days storage of reservoir" equals the number 1,000 divided by the square root of the rainfall in inches for three consecutive dry years. Thus, if this rainfall is 36 inches, the reservoir should contain 1,000 ^ 6 = 166.7 days storage ; that is, 166.7 times the excess of the demand over the dry weather supply. The following table (see " Engineering News," Aug. 23, 1879,) will show the great disparity between the l^ast and greatest flow of streams : Drainage Area Square miles. FLOW IN CUB FT. PER SQ. MILE. Name of River. Greatest Flow. Least Flow. 10,234 4,136 1,800 1,100 981 339 352 84 76 20 20.27 23.40 30.23 20.33 74.87 12.64 41.60 54.43 51 53 Schuvlkill 0.21 23 Tyne, England, Pi