Page:Scientific Papers of Josiah Willard Gibbs.djvu/457

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421

where denotes the number of molecules of the form (). Hence we have for the solution

[6]

If is constant, and also ,—a condition realized in equilibrium, when the solution is separated from the pure solvent by a diaphragm permeable to the solvent but not to the solutum, the equation reduces to

Whence [7]

being the pressure where , i.e., in the pure solvent. Here is the so-called osmotic pressure, and is the pressure as calculated[1] by the laws of Boyle, Charles, and Avogadro for the solutum in the space occupied by the solution. The equation manifestly expresses van't HofF's law.

For a coexistent solid phase of the solvent, with constant pressure, the general equation gives

for the solution, and

for the solid coexistent phase. Here and have necessarily the same values in the two equations, and we may suppose the quantity of one of the phases to be so chosen as to make the values of equal in the two equations. This gives

[8]

In integrating from to any small value of , we may treat the coefficients of and as having the same constant values as when . This gives

If we write for (the latent heat of melting for the unit of weight of the solvent), we get

or [9]
  1. Not experimentally found.