Multisite Disordered Structure of Ice VII to 20 GPa

R. J. Nelmes, J. S. Loveday, W. G. Marshall, G. Hamel, J. M. Besson, and S. Klotz
Phys. Rev. Lett. 81, 2719 – Published 28 September 1998
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Abstract

Neutron diffraction measurements on ice VII and ice VIII at pressures up to 20 GPa provide direct evidence of multisite disorder of both oxygen and deuterium atoms in D2O ice VII, and give the magnitudes of the site separations. An O-D distance and D-Ô-D angle closest to those found in ice VIII are obtained with oxygen sites displaced along 111 directions. Such displacements imply an H-bond geometry significantly different from that found in ice VIII, and this may have implications for the centering transition to ice X.

  • Received 5 May 1997

DOI:https://doi.org/10.1103/PhysRevLett.81.2719

©1998 American Physical Society

Authors & Affiliations

R. J. Nelmes, J. S. Loveday, and W. G. Marshall*

  • Department of Physics and Astronomy, The University of Edinburgh, Edinburgh EH9 3JZ, United Kingdom

G. Hamel1, J. M. Besson2, and S. Klotz2

  • 1Département des Hautes Pressions, Université Pierre et Marie Curie, 4 place Jussieu, 75252 Paris, France
  • 2Physique des Milieux Condensés (CNRS UMR 7602), Université Pierre et Marie Curie, 4 place Jussieu, 75252 Paris, France

  • *Now at ISIS Facility, Rutherford Appleton Laboratory, Chilton, Oxon OX11 0QX, U.K.

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Vol. 81, Iss. 13 — 28 September 1998

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