Startseite New accurate elastic parameters for the forsterite-fayalite solid solution
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New accurate elastic parameters for the forsterite-fayalite solid solution

  • F. Nestola EMAIL logo , D. Pasqual , J.R. Smyth , D. Novella , L. Secco , M.H. Manghnani und A. Dal Negro
Veröffentlicht/Copyright: 2. April 2015
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Abstract

Three natural olivines with Fo80Fa20, Fo71Fa29, and Fo62Fa38 compositions were investigated in situ at high pressure by single-crystal X‑ray diffraction using a diamond-anvil cell up to -8 GPa at room temperature. The bulk modulus, KT0, and its first pressure derivative, K′, do not show any significant variation among the compositions investigated and, using the data on a further sample with Fo92Fa8 composition recently investigated in the same laboratory and using the same experimental technique, we obtain, for the first time, a single equation of state for the entire Fo92Fa8-Fo62Fa38 compositional range. The equation has the following coefficients: KT0 = 124.7(9) GPa and K′ = 5.3(3) and can be used for thermodynamic calculations involving the most common mantle olivine compositions.

Received: 2011-3-11
Accepted: 2011-7-11
Published Online: 2015-4-2
Published in Print: 2011-11-1

© 2015 by Walter de Gruyter Berlin/Boston

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Heruntergeladen am 30.9.2025 von https://www.degruyterbrill.com/document/doi/10.2138/am.2011.3829/html
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