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
January, .737 1,712,198 11,264
February, .796 1,479,878 9,736
March, 1.070 2,237,242 14,719
April, .814 566,861 3,729
May, 1.462 387,974 2,552
June, .964 88,282 581
July, 1.077 51,110 336
August, 1.251 30,202 199
September, 1.015 46,464 305
October, 1.076 989,976 6,572
November, .937 2,176,838 14,321
December, .801 2,604,307 17,133
The city of Brooklyn gathers its supply by intercepting ponds. The
source is the southern slope of Long Island, with a drainage area
of 60.25 square miles. The plain is composed of fine sand, which is
saturated with excellent water, the surface of which rises twelve
feet per mile from the tide level at the shore, and which appears at
the surface of the ground in springs and streams, where depressions
occur in the ground level. The minimum observed flow occurred in
1880, and was equal to 9.4 inches on the water-shed. The available
supply is, at times, quite small.
The city of Lynn uses a driven well partly, of which they say, in
their annual report for 1880:
“The doubtful character of any underground supply of water,
especially when it is drawn from beneath a territory occupied by
a densely settled community, makes frequent examination of its
quality a duty not to be disregarded. We invite attention, however,
to the fact that the chemical examination of the well water has
shown an increasing quantity of foreign matter mingling with it as
pumping proceeded, and that this increase suggests an inflow of
water to the wells from some other source than that from which it
was at first drawn.”
This method of securing water, however, is largely resorted to in the
origin of water-works for small cities.
The Sanitary Engineer (Vol. v, No. 5) refers to a proposed well for
Lincoln, Nebraska, a town of 15,000 inhabitants, that the contractor
proposed to dig for the sum of $10,000. The estimated capacity will
be ten million gallons a day, and the editor of the paper observes:
“If a large well is sunk in a very saturated and porous soil, it
will probably furnish the amount required for the city (one million
gallons) at first, possibly a great deal more. But in five years’
time it is not hazardous to predict that such a well will not yield
enough water for Lincoln. As for furnishing ten million gallons a
day for any length of time, there is no well in the world, which
we know of, of such a capacity, and all experience is against the
probability of such an one being discovered.”
GRAVITATION
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account