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Pressure-volume-temperature behavior of fayalite based on static compression measurements at 400° C

Physics and Chemistry of Minerals volume 17, pages 212–219 (1990)Cite this article

Abstract

Twenty-one energy-dispersive X-ray diffraction spectra for fayalite at 400° C constitute the basis for an elevated-temperature static compression isotherm for this important silicate mineral. A Murnaghan regression of the resulting molar volumes yields 103.8 GPa and 7.1 for the 400° C, room-pressure values of the isothermal bulk modulus (K 0) and its first pressure derivative (K′0), respectively. When compared to the room-temperature static compression isotherm of Yagi et al. (1975), our 400° C value for K 0 yields 5.4 ×10−2 GPa/deg for (∂K/∂T)00. When combined with literature volume data, our measurements indicate that the fayalite isochores are strongly concave toward the pressure axis [(∂ 2 T/∂P 2) v <0].

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Author notes

  1. Thomas G. Plymate

    Present address: Department of Geosciences, Southwest Missouri State University, 65804, Springfield, MO, USA

Authors and Affiliations

  1. Department of Geology and Geophysics, University of Minnesota, 55455, Minneapolis, MN, USA

    Thomas G. Plymate & James H. Stout

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  1. Thomas G. Plymate
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  2. James H. Stout
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This is publication number 1125 of the School of Earth Sciences, Department of Geology and Geophysics, University of Minnesota, Minneapolis, MN 55455, USA

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Plymate, T.G., Stout, J.H. Pressure-volume-temperature behavior of fayalite based on static compression measurements at 400° C. Phys Chem Minerals 17, 212–219 (1990). https://doi.org/10.1007/BF00201452

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  • DOI: https://doi.org/10.1007/BF00201452

Keywords

  • Silicate
  • Mineral Resource
  • Molar Volume
  • Material Processing
  • Bulk Modulus