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Establishing the structure of GeS2 at high pressures and temperatures: a combined approach using x-ray and neutron diffraction

Anita Zeidler et al 2009 J. Phys.: Condens. Matter 21 474217 (22pp)   doi: 10.1088/0953-8984/21/47/474217  Help

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Anita Zeidler1, James W E Drewitt1, Philip S Salmon1, Adrian C Barnes2, Wilson A Crichton3, Stefan Klotz4, Henry E Fischer5, Chris J Benmore6, Silvia Ramos7 and Alex C Hannon8
1 Department of Physics, University of Bath, Bath BA2 7AY, UK
2 H H Wills Physics Laboratory, Royal Fort, Tyndall Avenue, Bristol BS8 1TL, UK
3 European Synchrotron Radiation Facility, 6 rue Jules Horowitz, BP 220, Grenoble Cedex, F-38043, France
4 IMPMC, Université Pierre et Marie Curie F-75252 Paris, France
5 Institut Laue-Langevin, 6 rue Jules Horowitz, BP 156, Grenoble Cedex 9, F-38042, France
6 Argonne National Laboratory, 9700 South Cass Avenue, Argonne, IL 60439, USA
7 Diamond Light Source Ltd, Diamond House, Harwell Science and Innovation Campus, Didcot, Oxon OX11 0DE, UK
8 ISIS Facility, Rutherford Appleton Laboratory, Chilton, Didcot, Oxon OX11 0QX, UK

Abstract. The change in structure of glassy GeS2 with pressure increasing to {\simeq }5~\mathrm {GPa} at ambient temperature was explored by using in situ neutron and x-ray diffraction. Under ambient conditions, the glass structure is made from a mixture of corner- and edge-sharing Ge(S1/2)4 tetrahedra where 47(5)% of the Ge atoms are involved in edge-sharing configurations. The network formed by these tetrahedra orders on an intermediate range as manifested by the appearance of a pronounced first sharp diffraction peak in the measured total structure factors at a scattering vector k = 1.02(2) Å−1 which has a large contribution from Ge–Ge correlations. The intermediate range order breaks down when the pressure on the glass increases above ≈2 GPa but there does not appear to be a significant alteration of the Ge–S coordination number or corresponding bond length with increasing density. The results for the glass are consistent with a densification mechanism in which there is a replacement of edge-sharing by corner-sharing Ge centred tetrahedral motifs and/or a reduction in the Ge–\hat {\mathrm
{S}} –Ge bond angle between corner-sharing tetrahedral motifs with increasing pressure. The change in structure with increasing temperature at a pressure of {\simeq }5~\mathrm
{GPa} was also investigated by means of in situ x-ray diffraction as the glass crystallized and then liquefied. At 5.2(1) GPa and 828(50) K the system forms a tetragonal crystal, with space group I\bar {4}2d and cell parameters a = b = 4.97704(12) and c = 9.5355(4) Å, wherein corner-sharing Ge(S1/2)4 tetrahedra pack to form a dense three-dimensional network. A method is described for correcting x-ray diffraction data taken in situ under high pressure, high temperature conditions for a cylindrical sample, container and gasket geometry with a parallel incident beam and with a scattered beam that is defined using an oscillating radial collimator. A method is also outlined for obtaining coordination numbers from direct integration of the peaks in measured x-ray total pair distribution functions.

Print publication: Issue 47 (25 November 2009)
Received 17 April 2009, in final form 4 August 2009
Published 5 November 2009

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