Site preference of Fe atoms in FeMgSiO4 and FeMg(SiO3)2 studied by density functional calculations

Swastika Chatterjee, Surajit Sengupta, Tanusri Saha-Dasgupta, Koustav Chatterjee, and Nibir Mandal
Phys. Rev. B 79, 115103 – Published 5 March 2009

Abstract

Using first-principles density functional calculation we investigate site preference of Fe in FeMgSiO4 olivine and FeMg(SiO3)2 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 local-densityapproximation+U calculations, and the crystal structures have been optimized by means of total-energy calculations. Our T=0K study in the total-energy-minimized structures indicate a strong preference for Fe to occupy M2 site in case of pyroxene and a preference for Fe to occupy M1 site in case of olivine. We provide the microscopic understanding of our finding in terms of density of states and charge densities.

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  • Received 4 November 2008

DOI:https://doi.org/10.1103/PhysRevB.79.115103

©2009 American Physical Society

Authors & Affiliations

Swastika Chatterjee1, Surajit Sengupta2,*, and Tanusri Saha-Dasgupta1,†

  • 1Department of Material Sciences, S. N. Bose National Center for Basic Sciences, JD-III, Salt Lake City, Kolkata 700 098, India
  • 2Department of Chemical, Biological, and Macro-Molecular Sciences, S. N. Bose National Center for Basic Sciences, JD-III, Salt Lake City, Kolkata 700 098, India

Koustav Chatterjee and Nibir Mandal

  • Indian Institute of Science Education and Research, IIT Kharagpur Extension Centre, Block-HC, Sector-III, Salt Lake City, Kolkata 700106, India

  • *Present address: Centre for Advanced Materials, Indian Association for the Cultivation of Science, Jadavpur, Kolkata 700032, India.
  • Corresponding author: tanusri@bose.res.in

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Issue

Vol. 79, Iss. 11 — 15 March 2009

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