A Handbook of Health by Woods Hutchinson (readnow TXT) π
CHAPTER II
WHY WE HAVE A STOMACH
WHAT KEEPS US ALIVE
The Energy in Food and Fuel. The first question that arises in our mind on looking at an engine or machine of any sort is, What makes it go? If we can succeed in getting an answer to the question, What makes the human automobile go? we shall have the key to half its secrets at once. It is fuel, of course; but what kind of fuel? How does the body take it in, how does it burn it, and how does it use the energy or power stored up in it to run the body-engine?
Man is a bread-and-butter-motor. The fuel of the automobile is gasoline, and the fuel of the man-motor we call food. The two kinds of fuel do not taste or smell much alike; but they are alike in that they both have what we call energy, or power, stored up
Read free book Β«A Handbook of Health by Woods Hutchinson (readnow TXT) πΒ» - read online or download for free at americanlibrarybooks.com
- Author: Woods Hutchinson
- Performer: -
Read book online Β«A Handbook of Health by Woods Hutchinson (readnow TXT) πΒ». Author - Woods Hutchinson
Here the farmhouse is set above the barn, pens, and cattle yard, and at some distance from them. The drainage from these is into the lower fields, so that a well driven into the high ground not far from the house is presumably safe.
The Danger from Outbuildings. This danger is further increased by the fact that for the same reasonβthe vital need of plenty of water for all living creaturesβthe hen coop, the pig pen, the cow stable, and the horse barn are all likely to be built clustering around this same well. If the fertilizer from these places is, as it should be in all intelligent farming, protected from the rain so as not to have all its strength washed out of it, and removed and spread on the soil at frequent intervals, the well may even yet escape contamination; but the chances are very strongly against it. If you will figure out that a well drains the surface soil in every direction for a distance from ten to thirty times its own depth, and that the average well is about twenty-five feet deep, you can readily see what a risk of contaminating the well is caused by every barn, outhouse, or pen within from sixty to a hundred and fifty yards from its mouth.
Every well from which drinking water is taken should be at least fifty, and better, a hundred and fifty, yards away from any stable, outhouse, or barn; or set well up-hill from it, so that all drainage runs away from its basin. This, of course, is possible only in the country, or in villages or small towns, where houses have plenty of ground about them. Consequently, the health laws of most cities and states forbid the use of shallow wells for drinking purposes in cities of over 10,000 population.
Causes which Produce Pure Well Water. Occasionally a well will be driven through a layer of rock or hard water-proof clay, before the water-bearing layer of soil, or sand, is struck, so that its water will be drawn, not from the rain that falls on the surface of the ground immediately about it, but from that which has fallen somewhere at a considerable distance and filtered down through the soil. This water, on account of the many, many layers of soil through which it has filtered, and the long distance it has come, is usually fairly pure, so far as animal or vegetable impurities are concerned, though it is apt to have become too strong in certain salty and mineral substances, which give it a taste of salt, or iron, or sulphur. If, however, it is free from these salty substances, it makes a very pure and wholesome drinking water; and if the upper part of the well shaft be lined with bricks and cement, so that the surface water cannot leak into it, it may be used with safety for drinking purposes even in the heart of a city.
The milk inspector on visiting this dairy farm found that the well was receiving the drainage of both house and privy. The well water was used for drinking and for washing the milk pails (seen behind the fence).
The Greatest Single Danger to Well Water. The greatest single danger to the purity of well water is the privy vault. This is doubly dangerous, first, because it is dug below the level at which the bacteria in the soil are most abundant and active, so that they cannot attack and break up its contents; and the impurities, therefore, are gradually washed down by the rain water into the soil, unchanged, and seep directly into the well. The other reason is that its contents may contain the germs of serious diseases, particularly typhoid fever and other bowel troubles. These germs and their poisons would usually be destroyed by the bacteria of the soil, if not poured out in too large quantities; but in the privy vault they escape their attack, and so are carried on with the slow leakage of water into the well; then those who use that water are very liable to have typhoid fever and other serious diseases.
Early Methods of Prevention. On account of these filth-dangers, it began, a century or so ago, to be the custom in cleanly and thoughtful households to provide, first, ditches, and then, lines of pipes, made out of hollow wood or baked clay, and later of iron, called drains, through which all the watery parts of household wastes could be carried away and poured out at some distance from the house. Then toilets, or flush-closets, were built, and this kind of waste was carried completely away from the house, and beyond danger of contaminating the wells.
How Streams were Contaminated. For a time this seemed to end the danger, as the waste was soaked up by the soil, and eaten by its hungry bacteria and drunk up again by the roots of plants. But when ten or a dozen houses began to combine and run their drain-pipes together into a large drain called a sewer, then this could not open upon the surface of the ground, but had to be run into some stream, or brook, in order to be carried away. As cities and towns, which had been obliged to give up their wells, were beginning to collect the water from these same brooks and streams in reservoirs and deliver it in pipes to all their houses, it can be easily seen that we had simply exchanged one danger for another.
The Loss of Life from Typhoid Fever. For a time, indeed, it looked as if the new danger were the greater of the two, because, when the typhoid germs were washed into a well, they poisoned or infected only one, or at most two or three, families who used the water from that well. But when they were carried into a stream which was dammed to form a reservoir to supply a town with water, then the whole population of the town might become infected. A great many epidemics of typhoid fever occurred in just this way, before people realized how great this danger was. Simply from the pouring of the wastes from one or two typhoid fever cases into the streams leading into the water reservoir used by a town, five hundred, a thousand, or even three or four thousand cases of typhoid have developed within a few weeks, with from one hundred to five hundred deaths.
TYPHOID EPIDEMIC IN THE MOHAWK-HUDSON VALLEY, 1891-92
In 1891-92 typhoid fever broke out in Schenectady on the Mohawk River. Following this, Cohoes and West Troy, which drew their water supply from the Mohawk below Schenectady, and Albany, which drew its supply from the Hudson below the mouth of the Mohawk, suffered from typhoid epidemics; while Waterford and Troy, which drew their supplies from the Hudson above the mouth of the Mohawk, and the river towns that, like Lansingburgh, drew from other sources, entirely escaped the infection.
In fact, even to-day, when these dangers are better understood, and while most of our big cities are getting fairly clear of typhoid, so ignorant and careless are the smaller towns, villages, and private houses all over the United States, that over 35,000 deaths[14] from typhoid fever occur every year in a country which prides itself upon its cleanliness and its intelligence. This means, too, that there are at least half a million people sick of the disease, and in bed or utterly prevented from working, for from five to fifteen weeks each. All of which frightful loss of human life and human labor, to say nothing of the grief, bereavement, and anxiety of the two million or more families and relatives of these typhoid victims, is due to eating dirt and drinking filth. Dirt is surely the most expensive thing there is, instead of the cheapest.
METHODS OF OBTAINING PURE WATERWise Planning and Spending of Money is Necessary. If our city wells are defiled by manure heaps and vault-privies, and our streams by sewage, where are we to turn for pure water? All that is required is foresight and a little intelligent planning and wise spending of money. Of course the community must take hold of the problem, through a Board of Health, or Health Officer, appointed for the purpose; and this is why questions of health are coming to play such an important part in legislation, and even in politics. No matter how fast a city is growing or how much money its inhabitants are making, if it has an impure water supply or a bad sewage system, there will be disease and death, suffering and unhappiness among its people, which no amount of money can make up for. Cleanliness is not only next to godliness, but one of the most useful forms of it; and a city can afford to spend money liberally to secure itβin fact, it is the best investment a city can make.
Artesian and Deep Wells. The earliest, and still the most eagerly sought-for, source of pure water supply is springs or deep wells, such as we have referred to. Both of these are fed by rain water which has fallen somewhere upon the surface of the earth. As the layers of earth or rock, of which the crust of the earth is made up, do not run level, or horizontal, but are tilted and tipped in all directions, this rain water soaks down until it reaches one of these sloping layers that is so hard, or tough, as to be waterproof, and then runs along over its surface in a sort of underground stream. If anywhere in the course of this stream a very deep well shaft is driven right down through the soil until it strikes the surface of this sloping layer of rock, then the water will rise in this shaft to the level of the highest point from which it is running.
The sketch shows a wide section from northern Illinois to central Wisconsin, in which the cities have rejected the water supplies afforded by the rivers, choosing instead to bore down almost to hard rock to insure the purity of the supply.
If this highest point of the waterproof layer be many miles away, up in the hills above the surface of the ground where the well is dug, then the
Comments (0)