Hygiene: a manual of personal and public health (New Edition)Newsholme, Arthur, Sir
Science
Hygiene: a manual of personal and public health (New Edition)
Newsholme, Arthur, Sir
Hygiene; Public health -- Great Britain; Sanitation
IMPURITIES OF WATER.
=Properties of Water.=—When pure, water =is colourless=, or bluish
when seen in large quantity. It should be quite =inodorous=. If,
after keeping it for some time in a perfectly clean vessel, or if on
heating it a smell is developed, the water is bad. Its =taste= should
be pleasant and sparkling from the atmospheric gases dissolved in it.
Bitterness generally indicates the presence of sulphate of magnesium
(Epsom salts). Saltness is always a suspicious property, except in
water obtained in the neighbourhood of salt mines or brine springs, or
near the sea. It should be soft to the =touch=, and should dissolve
soap easily. It should be bright and =clear=, and contain no suspended
matters. Clear water is not necessarily pure, but turbid water is
always to be rejected; the only exception being the brownish-tinged
water from moors, which is not hurtful. In all other cases, printed
matter should be legible through at least 18 inches of water in a
clear glass cylinder. Thoroughly dissolved organic matter is less
dangerous than suspended; the turbidity of water is therefore of great
importance. But water may be bright and sparkling and apparently
perfectly clear, and yet highly dangerous. The most important of the
physical properties of water in regard to health are the absence of
smell and turbidity, and these can be ascertained by even the most
inexperienced. The chemical tests for the more important impurities are
given (pages 85 to 87).
The impurities of water may be classed under four heads—gaseous,
mineral, vegetable, and animal.
The gases ordinarily present in water cannot properly be regarded as
impurities, inasmuch as they are always present, and greatly increase
its palatableness. The dissolved nitrogen and oxygen bear to each other
the proportion 1·42 to 1; where sewage contamination occurs, the oxygen
will be diminished or disappear, owing to oxidation of the organic
matter.
The amount of carbonic acid gas in water varies greatly. It may be
considerable in chalk waters, and in contaminated well-water.
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