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The P - V - T equation of state of D 2 O ice VI determined by neutron powder diffraction in the range 0 < P < 2.6 GPa and 120 < T < 330 K, and the isothermal equation of state of D 2 O ice VII from 2 to 7 GPa at room temperature (2012)

First Author: Fortes A

Attributed to: EXPERIMENTAL AND COMPUTATIONAL STUDIES OF PLANETARY ICES AND THEIR ROLE IN THE THERMAL EVOLUTION OF ICY MOONS funded by STFC

Abstract

No abstract provided

Bibliographic Information

Digital Object Identifier: http://dx.doi.org/10.1107/s0021889812014847

Publication URI: http://dx.doi.org/10.1107/s0021889812014847

Type: Journal Article/Review

Parent Publication: Journal of Applied Crystallography

Issue: 3