Modeling the Isotopic Fractionation of Magnesium and Calcium in High Temperature Thermal Gradients from First Principles

Details Modeling the Isotopic Fractionation of Magnesium and Calcium in High Temperature Thermal Gradients from First Principles Modeling the Isotopic Fractionation of Magnesium and Calcium in High Temperature Thermal Gradients from First Principles

Mar 2010

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2010lpi....41.2123d&link_type=abstract

41st Lunar and Planetary Science Conference, held March 1-5, 2010 in The Woodlands, Texas. LPI Contribution No. 1533, p.2123

Physics

Scientific paper

A fundamental model of isotope specific diffusion in high-temperature (T
> 1000°C) systems was developed and tested. We find that
differences in zero point energy of isotopes leads to isotopic
fractionation in high-temperature thermal gradients.

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