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Title: Thermoelasticity of olivine to 8 GPa 1073K

Journal Article · · Physics of the Earth and Planetary Interiors

In situ synchrotron X-ray diffraction measurements have been carried out on San Carlos olivine (Mg0.9Fe0.1)2SiO4 up to 8 GPa and 1073 K. Data analysis using the high-temperature Birch-Murnaghan (HTBM) equation of state (EoS) yields the temperature derivative of the bulk modulus ({partial_derivative}KT/{partial_derivative}T)P = -0.019 {+-} 0.002 GPa K-1. The thermal pressure (TH) approach gives aKT = 4.08 {+-} 0.10 x 10-3 GPa K-1, from which ({partial_derivative}KT/{partial_derivative}T)P = -0.019 {+-} 0.001 GPa K-1 is derived. Fitting the present data to the Mie-Grueneisen-Debye (MGD) formalism, the Grueneisen parameter at ambient conditions 0 is constrained to be 1.14 {+-} 0.02 with fixed volume dependence q = 1. Combining the present data with previous results on iron-bearing olivine and fitting to MGD EoS, we obtain 0 = 1.11 {+-} 0.01 and q = 0.54 {+-} 0.36. In this study the thermoelastic parameters obtained from various approaches are in good agreement with one another and previous results.

Research Organization:
Brookhaven National Lab. (BNL), Upton, NY (United States). National Synchrotron Light Source
Sponsoring Organization:
Doe - Office Of Science
DOE Contract Number:
DE-AC02-98CH10886
OSTI ID:
959950
Report Number(s):
BNL-82936-2009-JA; PEPIAM; TRN: US1005849
Journal Information:
Physics of the Earth and Planetary Interiors, Vol. 157; ISSN 0031-9201
Country of Publication:
United States
Language:
English

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