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
Boyle's law, the ‹osmotic pressure of the solution increases›.
Similarly, when a solution is cooled until freezing occurs,
provided the solute does not crystallize out with the solvent, the
concentration of the solute is again increased, and therefore the
‹osmotic pressure› of the solution is also increased. Van 't Hoff
recognized the relations existing between the freezing, boiling
and vaporization of solutions, on the one hand, and the changes of
their osmotic pressures on the other. By developing rigorously the
‹relations between the lowering of the vapor tension, the raising of
the boiling-point, the lowering of the freezing-point› of a solvent
by a solute ‹and the osmotic pressure of the solution›, he made it
possible[21] to use [p018] extensive experimental material,[22] on
the elevation of boiling-points and the lowering of freezing-points
and of vapor tensions, to determine the osmotic pressures of
solutions. The theory of the relation of osmotic pressure to gas
pressure is fully confirmed by these measurements, for those cases
to which it may properly be applied, namely, to sufficiently dilute
solutions and such as have only negligible heats of dilution, ‹i.e.›
in which dilution does not involve chemical changes.
«Apparent Exceptions.»—Instead of discussing the vast amount of
material of this kind, which agrees with van 't Hoff's theory,
we may consider, more profitably, typical cases of ‹apparent
exceptions›. The most important instance of this kind, the case of
solutions of compounds which undergo ‹electrolytic dissociation or
ionization›, will be separately discussed in the next chapter, and
we shall find that van 't Hoff's great generalization is a vital
element in the evidence of this important form of dissociation. Of
other apparent exceptions, we may note the fact that some solutes
seem to give "abnormally" ‹low› osmotic pressures[23] in certain
solutions. For instance, benzoic acid, in benzene solutions, gives
only a little more than half as great an osmotic pressure as it does
in aqueous solutions of the same concentration and temperature, and
as would be calculated on the basis of the Avogadro-van 't Hoff
Hypothesis for a compound of the formula C_{6}H_{5}COOH and the
molecular weight 122. But a rigorous study[24] of the distribution
of benzoic acid between water and benzene, when solutions of the
acid in the two solvents are shaken together until equilibrium
is established (Chapter VIII), has proved that the distribution
is strictly in accord with the assumption that benzoic acid, in
aqueous solution, has the molecular weight 122 and the composition
C_{6}H_{5}COOH, and that, in benzene solution, it has the molecular
weight 244 and the composition (C_{6}H_{5}COOH)_{2}; only a
‹small part› of the acid (C_{6}H_{5}COOH)_{2} is decomposed in
benzene solution into the simpler molecules, of the composition
C_{6}H_{5}COOH. In other words, the simpler molecules C_{6}H_{5}COOH
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