CHAP. 6: THERMODYNAMICS OF HOMOGENEOUS MIXTURES [CONTENTS] 145
∆GE = ∆GM−RT
∑k
i=1
xilnxi, (6.34)
∆FE = ∆FM−RT
∑k
i=1
xilnxi. (6.35)
6.2.3 Heat of solution (integral)
The heat of solution is defined by the relation
∆solHi=
Q
ni
, [T, p], (6.36)
whereQis the heat exchanged with the surroundings, which accompanies the solution ofni
moles of a substanceiinnsolvmoles of a solvent at specified temperature and pressure.
Note: The heat of solution defined in this way is sometimes termed the integral heat of
solution in order to prevent confusion with the differential heat of solution of a component
[see6.3.5].
∆solHi depends on temperatureT, pressurep, and on the composition of the resulting
mixture.
Dependence of the integral heat of solution on composition can be expressed in two ways:
a) using a relative amount of solvent
nrel=
nsolv
ni
(6.37)
in which case the heat of solution ∆solHiis defined as the amount of heat accompanying
solution of 1 mole of a substance innrelmoles of a solvent;
b) using molalitymiof the dissolved substance in the resulting mixture.
Example
During the dissolution of 0.2 mol NH 3 (g) in 54.045 g H 2 O(`)at 25◦C and pressure 101.325 kPa,
it was found out that a heat of 6870 J passed to the surroundings. Calculate the heat of solution
of ammonia andnrel.