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)
28 may, therefore, be regarded either as the solubility curve of
silver nitrate in water, or as the freezing point curve for silver nitrate
in contact with a solution consisting of that salt and water.
As the temperature of the saturated solution falls, silver nitrate is
deposited, and on lowering the temperature sufficiently a point will at
last be reached at which ice also begins to separate out. Since there are
now four phases co-existing, viz. silver nitrate, ice, solution, vapour,
the system is invariant, and the point is a _quadruple point_. This
quadruple point, therefore, forms the lower limit of the solubility curve
of silver nitrate. Below this point the solution becomes metastable.
Ice as Solid Phase.--Ice melts or is in equilibrium with water at a
temperature of 0°. The melting point, will, however, be lowered by the
solution of silver nitrate in the water; and the greater the concentration
of the salt in the solution the greater will be the depression of the
temperature of equilibrium. On continuing the addition of silver nitrate, a
point will at length be reached at which the salt is no longer dissolved,
but remains in the solid form along with the ice. We again obtain,
therefore, the invariant system ice--salt--solution--vapour. The
temperature at which this invariant system can exist has been found by
Middelberg[193] to be -7.3°, the solution at this point containing 47.1 per
cent. of silver nitrate.
The same general behaviour will be found in the case of all other systems
of two components belonging to this class; that is, in the case of systems
from which the components crystallise out in the pure state, and in which
the fused components are miscible in all proportions. In all such cases,
therefore, the solubility curves (curves of equilibrium) can be represented
diagrammatically as in Fig. 29. In this figure OA represents the solubility
curve of the salt, and OB the freezing {117} point curve of ice. O is the
quadruple point at which the invariant system exists, and may be regarded
as the point of intersection of the solubility curve with the
freezing-point curve. Since this point is fixed, the condition of the
system as regards temperature, vapour pressure, and concentration of the
components (or composition of the solution), is perfectly definite. From
the way, also, in which the condition is attained, it is evident that the
quadruple point is the lowest temperature that can be obtained with
mixtures of the two components in presence of vapour. It is known as the
_cryohydric point_, or, generally, the _eutectic point_.[194]
[Illustration: FIG. 29.]
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