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Published May 1980 | Published
Journal Article Open

Identification of Ice VI on the Hugoniot of Ice I_h

Abstract

Ice VI has been produced by shock compression of ice I_h to about 2 GPa. This is the second high-pressure polymorph of water observed in shock loading. These experiments point out the ease with which high-pressure phases can form when ice I_h is impacted. The new shock data, combined with previous static measurements, provide preliminary equation of state parameters for ice VI.

Additional Information

Copyright 1980 by the American Geophysical Union. (Received January 15, 1980; accepted January 28, 1980.) Paper number 80L0119. Supported under NASA Contract NASW-3224. PacTech report number PT-U79-0408. Contribution no. 3345, Division of Geological and Planetary Sciences, California Institute of Technology. We appreciate the experimental assistance of J. Long, E. Gelle, and M. Long in operating the facilities in the Roland and Helen W. Lindhurst Laboratory of Experimental Geophysics and P. L. Riersgard for his assistance in sample preparation.

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Created:
August 19, 2023
Modified:
October 18, 2023