The Phase Rule and Its ApplicationsFindlay, Alexander
Science
The Phase Rule and Its Applications
Findlay, Alexander
Chemistry, Physical and theoretical; Phase rule and equilibrium; Solution (Chemistry)
This, at first sight, strange fact will be readily understood when we
consider that since ice and solution are together in equilibrium with the
same vapour, they must have the same vapour pressure. For suppose at any
given temperature equilibrium to have been established in the system
ice--solution--vapour, removal of the ice will not alter this equilibrium.
Suppose, now, the ice and the solution placed under a bell-jar so that they
have a common vapour, but are not themselves in contact; then, if they do
not have the same vapour pressure, distillation must take place and the
solution will become more dilute or more concentrated. Since, at the
completion of this process, the ice and solution are now in equilibrium
when they are not in contact, they must also be in equilibrium when they
are in contact (p. 32). But if distillation has taken place the
concentration of the solution must have altered, so that the ice will now
be in equilibrium with a solution of a different concentration from before.
But according to the Phase Rule ice cannot at one and the same temperature
be in equilibrium with two solutions of different concentration, for the
system ice--solution--vapour is univariant, and at any given temperature,
therefore, not only the pressure but also the _concentration of the
components in the solution must be constant_. Distillation could not,
therefore, take place from the ice to the solution or _vice versâ_; that is
to say, the solution and the ice must have the same vapour pressure--the
sublimation pressure of ice. The reason of the coincidence is the
non-volatility of the salt: had {129} the salt a measurable vapour pressure
itself, the sublimation curve of ice and the curve for
ice--solution--vapour would no longer fall together.
The curve AO represents the pressures of the system ice--salt--vapour. This
curve will also be coincident with the sublimation curve of ice, on account
of the non-volatility of the salt.
The equilibria of the fourth univariant system ice--salt--solution are
represented by AE. Since this is a condensed system, the effect of a small
change of temperature will be to cause a large change of pressure, as in
the case of the fusion point of a pure substance. The direction of this
curve will depend on whether there is an increase or diminution of volume
on solidification; but the effect in any given case can be predicted with
the help of the theorem of Le Chatelier.
Public-domain text, read in full here on John Shaqi.
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