The People's Common Sense Medical Adviser in Plain English: or, Medicine Simplified, 54th ed., One Million, Six Hundred; and Fifty Thousand
John Stuart Mill · en
THE NATURAL DRINK OF MAN. Water constitutes the natural drink of man. No
other liquid can supply its place. Its presence, however, in the body is
not permanent. It is discharged from the body in different ways; by the
urine, the feces, the breath, and the perspiration. In the first two, it
is in a liquid form, in the others in a vaporous form. It is estimated
that about forty-eight per cent. is discharged in the liquid, and
fifty-two per cent. in the vaporous form; but the absolute as well as
the relative amount discharged depends upon a variety of circumstances.
Water is never found perfectly pure, since it holds in solution more or
less of almost every substance with, which it comes in contact. Rain
falling in the country remote from habitations is the purest water that
nature furnishes, for it is then only charged with the natural gases of
the atmosphere. In cities it absorbs organic and gaseous impurities, as
it falls through the air, and flowing over roofs of houses carries with
it soot and dust. Water from melted snow is purer than rain-water, since
it descends in a solid form, and is therefore incapable of absorbing
gases. Rain-water is not adapted to drinking purposes, unless well
filtered. All water, except that which has been distilled, contains air,
and it is due to this fact, that aquatic animals can live in it; for
example, put a fish in distilled water and it will soon die.
MINERAL IMPURITIES. Rain-water, which has filtered through the soil and
strata of the earth, dissolves the soluble materials, and carries them
down to lower levels, until they finally collect in the sea. Common
well, spring, and mineral waters contain from 5 to 60 grains to the
gallon; sea-water contains 2,000 grains while in some parts of the Dead
Sea there are 20,000 grams to the gallon. The principal mineral
impurities of well and spring water are lime, magnesia, soda, and oxide
of iron, combined with carbonic and sulphuric acids, forming carbonates,
sulphates, and chloride of sodium, or common salt. The most general,
however, are carbonate and sulphate of lime.