The Elements of Qualitative Chemical Analysis, vol. 1, parts 1 and 2.: With Special Consideration of the Application of the Laws of Equilibrium and of the Modern Theories of Solution.Stieglitz, Julius
Science
The Elements of Qualitative Chemical Analysis, vol. 1, parts 1 and 2.: With Special Consideration of the Application of the Laws of Equilibrium and of the Modern Theories of Solution.
Stieglitz, Julius
Chemistry, Analytic -- Qualitative
«Self-Neutralization of Amphoteric Substances.»[360]—We may turn now
to the third question raised in connection with aluminium hydroxide,
to the inquiry (p. 171), why aluminium hydroxide, the acid, does not
neutralize aluminium hydroxide, the base. In fact, the base must
and does form a salt with the acid. But the salt is formed only to
a minimal extent, as the result of the fact that the base is a very
weak base, the acid an exceedingly weak acid. Such exceedingly weak
bases and acids show little tendency to combine with each other to
form salts ‹in the presence of water, especially if one or both
are difficultly soluble in water›, as in the present instance. The
behavior of aluminium hydroxide, in this respect, is part of a much
larger and more general question, growing out of the fact that water
is a very weak acid and base, as has been seen, and, to a greater
or lesser extent, reacts as such with salts, which are dissolved in
it. This action of water plays an important rôle in many analytical
reactions, and especially, also, in the reactions of aluminium salts.
We shall, first, discuss this larger question of the action of water,
as an ionogen, on salts, and then return (p. 187) to the problem of
the self-neutralization of an amphoteric hydroxide.
HYDROLYSIS OF SALTS
«Ionization of Water.»—We may first consider, very briefly, the
evidence that water is ionized even to the extent indicated by the
ionization constants given in our tables. It may be said that the
purest water ever prepared[361] shows a minimal conductivity, from
which the concentrations of its hydrogen and hydroxide ions and
the value of the ionization constant may be calculated. For the
ionization of water we have
[H^{+}] × [HO^{−}] / [Nonionized water] = K_{Ion}.
As the concentration of pure water, or of the water in dilute
solutions, may be considered nearly a constant, we may put
[H^{+}] × [HO^{−}] = K_{H_{2}O}.
This is the relation most commonly, and most conveniently, used.
It is free from all assumptions as to the molecular weight of the
nonionized water, the calculation of the concentrations [p177]
[H^{+}] and [OH^{−}] being independent of any such assumption. The
value of K_{H_{2}O} increases decidedly with an increase in the
temperature,[362] whereas the ionization constant of an ordinary
acid, such as acetic acid, is affected very little by changes in
temperature. This peculiar increase of the ionization of water at
higher temperatures is undoubtedly due to the increasing dissociation
of the complex water molecules into hydrol molecules (see p. 66),
which, presumably, are most easily ionized. Now, the value of
the constant K_{H_{2}O}, at any temperature, may be determined
in some half a dozen different and independent ways, including
the conductivity method mentioned, and one of the most remarkable
developments of the theory of ionization is that all of these methods
lead to concordant results.[363]
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