Compressibility of phase A, Mg 7Si 2H 6O i4 up to 11.2 GPa

Takahiro Kuribayashi, Yasuhiro Kudoh, Hiroyuki Kagi

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12 Citations (Scopus)

Abstract

A single crystal high-pressure X-ray diffraction study of phase A was performed using a diamond anvil cell up to 11.2 GPa at ambient temperature. The chemical formula of this sample, determined by EPMA from an average of 8 data points, was Mg 66.9Si 1.99H 6.06O 14 Axial linear compressibilities of phase A wereβ a=2.92(2) andβ c= 2.17(3) (xlO -3/GPa). The isothermal bulk modulus, calculated using the Birch-Murnaghan equation of state, was K T0=105(4) GPa with a pressure derivative k'=3.9(8) and V 0=512.2(6) A 3. The bulk modulus correlates with the summation of the filling factor of the tetrahedral site and the octahedral site, as shown for the minerals on the forsterite-brucite join in the system MgO-Si0 2-H 20.

Original languageEnglish
Pages (from-to)215-234
Number of pages20
JournalJournal of Mineralogical and Petrological Sciences
Volume98
Issue number6
DOIs
Publication statusPublished - 2003

ASJC Scopus subject areas

  • Geophysics
  • Geology

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