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
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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
Now, if both the free base and the free acid are very ‹difficultly
soluble›, then the concentrations [MeOH] and [HX], respectively,
in the solution ‹cannot go beyond a certain minute limit›. In
view,[376] then, of the very small value, K_{Base}, of the ratio
[Me^{+}] × [HO^{−}] / [MeOH] and the minute value that the
second term [MeOH] has under these conditions, the first term
[Me^{+}] × [HO^{−}] must have a correspondingly smaller value. It
is clear, therefore, that in such a solution neither the nonionized
base, MeOH, nor its ion, Me^{+}, can exist in more than minute
quantities when the equilibrium constants are satisfied. The same
conclusion is reached regarding the [p186] possibility of the
existence of the difficultly soluble acid HX and its ion X^{−}, in
more than minimal quantities. Since, then, neither the ion Me^{+} nor
the ion X^{−} can be present in more than traces, their salt, MeX,
which is considered readily ionizable, also ‹cannot exist in aqueous
solutions›, except in traces.
The ‹quantitative relations› are evident from the equilibrium
equation (p. 185): [Me^{+}] × [X^{−}] / ([HX] × [MeOH]) =
α^2 [Salt]^2 / ([Acid] × [Base]) = (K_{Acid} × K_{Base}) / K_{HOH} = K.
It is evident that the concentration of the salt, [Salt], which is
capable of existence in aqueous solution, is, in the first place,
‹the smaller the smaller the values› for K_{Acid} and K_{Base}
are, ‹i.e. the weaker the acid and the base are›; and, in the
second place, it is the smaller the smaller the values for [Acid]
and [Base] are, which, in the present instance, represent the
concentrations of the difficultly soluble acid and base in saturated
solution, ‹i.e. their solubilities›.
We reach the conclusion that ‹salts of very weak bases and very weak
acids are very considerably decomposed by water›, and, if both the
acid and the base are difficultly soluble in water, the decomposition
is ‹practically complete›. ‹Conversely, such a very weak, difficultly
soluble base will not combine with a very weak, difficultly soluble
acid to form a salt in the presence of water.› An instance of the
first kind is found in the case of aluminium sulphide, the salt of
a very weak, difficultly soluble base, aluminium hydroxide, with
a rather little soluble, weak acid, hydrogen sulphide (see table,
p. 104). We find that when a piece of aluminium sulphide, prepared
by dry methods, is dropped into water (‹exp.›), a precipitate of
aluminium hydroxide is immediately formed and evolution of hydrogen
sulphide occurs. We have
Al_{2}S_{3} ⇄ 2 Al^{3+} + 3 S^{2−},
«6 HOH» ⇄ 6 HO^{−} + 6 H^{+}
2 Al^{3+} + 6 HO^{−} ⇄ «2 Al(OH)_{3} ↓»
3 S^{2−} + 6 H^{+} ⇄ «3 H_{2}S ↑».
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