Isotopic fractionation by isotope-exchange reactions as a function of temperature: (2)H and (18)O in OH(-) + H sub 2 O and H sub 3 O(+) + H sub 2 O and (15)N in N sub 2 H(+) + N sub 2
A simple model is used to predict the fractionation of isotopes as a function of temperature via ion-molecule reactions. It is developed for reactions proceeding via a single intermediate, where the isotopic mixing is completed within the lifetime of the intermediate such that the reaction is under thermodynamic control. The fractionation efficiency is K/(K + 1) where K is the equilibrium constant of the isotope-exchange reaction. The model is applied to deuterium and Oxygen 18 fractionation via the prototypical reactions OH(-)+H2O and H3O(+)+H2O; satisfactory agreement is found with the data available for 300 K. The model is also applied tomore »