Isotope effect on the thermodynamic quantities of gaseous uranium hexafluoride
For gaseous UF6 changes in the thermodynamic quantifies ΔG (= ΔA), ΔH (= ΔU), ΔCp (= ΔCv), and ΔS upon isotopic substitution can be determined by using the spectroscopically determined geometry and force field. The differences ΔG etc. are defined as (G238 – Gx), where 238 and x (x = 235, 234, 233, and 232) are the masses of the central uranium atom. The changes in the thermodynamic quantities are related to the logarithm of the partition function ratio of the UF6 species compared. The logarithm of the partition function ratio can be conveniently expressed as a series in temperature and hence, by using statistical mechanical relationships, the changes in thermodynamic quantities can be expressed as a series in temperature.Since these changes form examples of heavy isotope effects the validity and utility of the first quantum correction can be investigated. Uncertainties and trends in the magnitudes of the differences in the thermodynamic quantities due to uncertainties or changes in spectroscopic parameters are discussed by means of the first quantum correction. It has been found that the first quantum correction has little quantitative value in the lower temperature region, but it can be used in that range to explain some observed trends in the isotope effects. Some of the conclusions can also be applied to kinetic and equilibrium heavy isotope effects.