History of the Water Supply of the World: arranged in a comprehensive form from eminent authorities, containing a description of the various methods of water supply, pollution and purification of waters, and sanitary effects, with analyses of potable waters, also geology and water strata of Hamilton county, Ohio, statistics of the Ohio river, proposed water supply of Cincinnati.Bell, Thomas J. (Thomas Jefferson)
History
History of the Water Supply of the World: arranged in a comprehensive form from eminent authorities, containing a description of the various methods of water supply, pollution and purification of waters, and sanitary effects, with analyses of potable waters, also geology and water strata of Hamilton county, Ohio, statistics of the Ohio river, proposed water supply of Cincinnati.
Bell, Thomas J. (Thomas Jefferson)
Water-supply -- History; Water-supply -- Ohio -- Hamilton County
As the contents of the water-hole or well are pumped out, they are
immediately replenished from the surrounding disgusting mixture, and
it is not therefore very surprising to be assured that such wells
do not become dry even in summer. Unfortunately, excrementitious
liquids, especially after they have soaked through a few feet of
porous soil, do not impair the palatability of water; and this
polluted liquid is consumed from year to year without a suspicion of
its character.
Our acquaintance with a very large portion of this class of potable
waters, has been in consequence of the occurrence of severe outbreaks
of typhoid fever amongst consumers of this character of water.
“The samples of water from deep unpolluted wells were obtained
from wells or bore-holes of a depth rarely less than 100 feet,
and reaching in one case 1,285 feet. In many cases these wells
were partly or wholly supplied by surface-polluted water. Such
water, when it penetrates only to shallow wells still retains a
considerable proportion of its polluting organic matter in an
unoxidized condition: but when it descends through one hundred
feet or upwards of porous soil or rock, the exhausted filtration
to which it has been subjected in passing downwards through so
great a thickness of material, and the rapid oxidation of the
dissolved organic matters in a porous and aerated medium, afford
a considerable guarantee that all noxious constituents have been
removed.”--(Rivers Pollution Commission, 1874.)
“Deep wells may become polluted, either by admission of soakage
from the superficial strata into the shaft of the well, or by
access of polluted water through open fissures in the rock in which
the well is sunk.”--(Rivers Pollution Commission, 1874.)
“Even where wells are sunk to great distance (one was sunk at
Bondy, near Paris, to a depth of 247 feet), the surrounding soil is
not free from danger of pollution by the soaking of the foul liquid
into the side of the well.”--(Fifth report Massachusetts State
Board of Health.)
The following table shows the average analysis of ten worst examples
of well water (parts in 100,000 parts):
AV. CARBON NITROGEN
DEPTH. ORGANIC. ORGANIC. CHLORINE. HARDNESS.
Shallow wells, -- 1.560 .241 16.56 63.24
Deep wells polluted, -- .363 .092 9.45 36.27
Deep wells unpolluted, 380 .151 .032 14.14 27.4
ARTESIAN WELLS.
Artesian is the name applied to water-springs rising above the
surface of the ground by natural hydrostatic pressure, or boring a
small hole down through a series of strata to a water-bearing bed
inclosed between two layers. It was first practiced in 1100, in
province of Artois, France, whence it derives its name.
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