On the Temperature Dependence of the Kinetic Isotope Fractionation of Type B CAI-like Melts During Evaporation

Physics

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Scientific paper

The kinetic isotope fractionation factor for Mg evaporating from
CAI-like melts is significantly different from the commonly assumed
value of (24/25)^0.5. It varies with temperature and for typical natural
conditions, 5 permil per amu implies 36%, not 22% Mg loss.

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