How should I generally try to express ΔV for calculations using the Clausius-Clapeyron equation?
Example problem:
CH
4·6H
2O decomposes to produce solid water, ice. The enthalpy of this process equals 17.47 kJ·mol
–1. Assume that the enthalpies do not depend on temperature and pressure, the volume change upon decomposition of hydrate is equal to the volume of released methane, and methane is an ideal gas. At what external pressure does decomposition of methane hydrate into methane and ice take place at –5°C?
The reaction equation is CH
4·6H
2O (s)
CH
4 (g) + H
2O (s).
The solution notes that
[tex]\frac{dp}{dT} = \frac{\Delta H}{T \cdot \Delta V}[/tex]
Just as I expected. But now ΔV is given as something much more complicated than what I have seen before:
[tex]\Delta V = \frac{RT}{p} + \frac{6 \cdot M_{H2O}}{\rho_{H2O}} - \frac{M_{CH4.6H2O}}{\rho_{CH4.6H2O}}[/tex]
Why on earth is ΔV like this? And that raises the question, for a general reaction, including solid phases (after all H2O and the methane hydrate are both solid here) as well as gaseous phases, how can I write ΔV, this accurately?