Philosophical transactions, Vol. L. Part I. For the year 1757.: Giving some account of the present undertakings, studies, and labours, of the ingenious, in many considerable parts of the world.Various
History
Philosophical transactions, Vol. L. Part I. For the year 1757.: Giving some account of the present undertakings, studies, and labours, of the ingenious, in many considerable parts of the world.
Various
Science -- Periodicals
20. This experiment being also made with a weak solution of alum in
spring-water, its effects upon the milk were not in the least different
from those of the mineral water.
21. And the same trial being again repeated with the water, when
boiled and filtred from its ochrous parts, the milk was in the same
manner coagulated as before elixation.
22. One part of sweet milk being added to four parts of the mineral
water, the milk subsided, and formed a cloud in the bottom of the
glass, leaving the upper parts of the water clear. This mixture being
heartily shaken, the milk mixed so well with the water, that it
appeared to be but a very little curdled.
23. When a larger quantity of milk was added to a smaller quantity of
water, and even when equal parts of the milk and mineral water were
mixed and shaken together, there could be no curdling or coagulation
observed.
24. An equal quantity of the water and milk being boiled together, the
greatest part of the milk was coagulated into a thick white curd; and
the remainder, with the mineral water, turned of a pure white milky
colour, which drank like whey, and was very agreeable.
25. Eight gutts of sweet milk being added to four ounces of the water,
and the mixture boiled, part of the milk was thereby curdled, and swam
upon the top of the water. The ochrous parts of the water were likewise
separated, and falling to the bottom, their colour did not appear of a
clear yellow, as usual, but was something milky.
All these experiments strongly indicate the existence of alum in this
water. It retains its aluminous taste, and coagulates milk, after the
chalybeat parts are almost all expelled by elixation. The coagulation
of the milk demonstrates an acidity in the water, and the other
appearances shew that acidity to be owing to an aluminous salt.
It appears, that the milk requires a large quantity of the water, to
make a sensible coagulation in it: for, in the 22d experiment, one
part of the milk being added to four parts of the mineral water, the
coagulation was scarcely discernible: and in the 23d, when an equal or
larger quantity of milk was added to the water, the coagulation was
not at all observable. I have heard it confidently averred, that this
mineral water did not at all curdle milk; which, I suppose, has been
thro’ a mistake in the experiment, in adding too large a proportion of
milk to the water: for in this way the coagulation cannot be observed.
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