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Published September 10, 1984 | Published
Journal Article Open

Shock wave equations of state using mixed-phase regime data

Abstract

A method is given that uses Hugoniot data in the mixed-phase regime to constrain further equation of state (EOS) parameters of low- and high-pressure phases of materials under-going phase transformations on shock loading. We compute the relative proportion of low- and high-pressure phases present in the mixed-phase region and apply additional tests to the EOS parameters of the separate low- and high-pressure phases by invoking two simple requirements: the fraction of high-pressure phase (1) must increase with increasing shock pressure, and (2) must approach one at the high-pressure end of the mixed-phase regime. We apply our analysis to previously published data for potassium thioferrite, KfeS_2, and pyrrhotite, Fe_(0.9)S. We find that including the mixed-phase regime data in the KfeS_2 analysis requires no change in the published high-pressure EOS parameters. For Fe_(0.9)S we must modify the high-pressure phase EOS parameters to account for both the mixed-phase and high-pressure phase Hugoniot data. Our values of zero-pressure density, bulk modulus and first pressure derivative of the bulk modulus of the high-pressure phase of Fe_(0.9)S are 5.3 Mg/m^3, 106 GPa, and 4.9, respectively.

Additional Information

© 1984 by the American Geophysical Union. Paper number 4B0741. Received September 13, 1982; revised May 2, 1984; accepted May 15, 1984. We appreciate discussions with M. B. Boslough and J. M. Vizgirda as well as a helpful review from J. M. Brown, Computing support was provided by the Office of Computer Services and the Department of Geology, Rensselaer Polytechnic Institute. Supported by NSF grant EAR 79-26384. Contribution 3733, Division of Geological and Planetary Sciences, California Institute of Technology.

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August 19, 2023
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