Abstract
Using first-principles density functional calculation we investigate site preference of Fe in olivine and pyroxene, which are the major constituents of the earth’s upper mantle. A combination of state-of-the-art methods has been used for this purpose. The strong correlation effect at Fe site has been taken care of by means of calculations, and the crystal structures have been optimized by means of total-energy calculations. Our study in the total-energy-minimized structures indicate a strong preference for Fe to occupy site in case of pyroxene and a preference for Fe to occupy site in case of olivine. We provide the microscopic understanding of our finding in terms of density of states and charge densities.
- Received 4 November 2008
DOI:https://doi.org/10.1103/PhysRevB.79.115103
©2009 American Physical Society