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Science 7 August 1998: Vol. 281. no. 5378, pp. 809 - 812 DOI: 10.1126/science.281.5378.809
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Reports
In Situ Observations of a High-Pressure Phase of H2O Ice
I-Ming Chou,
*
Jennifer G. Blank,
Alexander F. Goncharov,
Ho-kwang Mao,
Russell J. Hemley
A previously unknown solid phase of H2O has been
identified by its peculiar growth patterns, distinct
pressure-temperature melting relations, and vibrational Raman spectra.
Morphologies of ice crystals and their pressure-temperature melting
relations were directly observed in a hydrothermal diamond-anvil cell
for H2O bulk densities between 1203 and 1257 kilograms per
cubic meter at temperatures between -10° and 50°C. Under these
conditions, four different ice forms were observed to melt: two stable
phases, ice V and ice VI, and two metastable phases, ice IV and the new ice phase. The Raman spectra and crystal morphology are consistent with
a disordered anisotropic structure with some similarities to ice VI.
I. Chou, 955 National Center, U.S. Geological Survey, Reston, VA
20192, USA. J. G. Blank, A. F. Goncharov, H. Mao, R. J. Hemley,
Geophysical Laboratory and Center for High Pressure Research, Carnegie
Institution of Washington, 5251 Broad Branch Road, NW, Washington, DC
20015, USA.
*
To whom correspondence should be addressed.
Present address: Department of Geology and Geophysics,
University of California, Berkeley, CA 94720, USA.
Read the Full Text
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