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Pressure-Induced Distortive Phase Transition in Chromite-Spinel at 29 GPa

Published online by Cambridge University Press:  26 February 2011

Jinfu Shu
Affiliation:
[email protected], Carnegie Institution of Washington, Geophysical Laboratory, 5251 Broad Branch Road, NW, Washington, DC, 20015, United States
Wendy L. Mao
Affiliation:
[email protected], Los Alamos National Laboratory, LANSCE, Los Almos, NM, 87545, United States
Russell J Hemley
Affiliation:
[email protected], Carnegie Institution of Washington, Geophysical Laboratory, 5251 Broad Branch Road, NW, Washington, DC, 20015, United States
Hokwang Mao
Affiliation:
[email protected], Carnegie Institution of Washington, Geophysical Laboratory, 5251 Broad Branch Road, NW, Washington, DC, 20015, United States
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Abstract

A natural chromite single crystal was compressed in a helium pressure medium to just above 35 GPa at ambient temperature and studied with energy-dispersive x-ray diffraction. The volume compression of the cubic, spinel-type structure was fit to a third-order Birch-Murnaghan equation of state with parameters a0 = 8.338(4) Å, V0 = 579.6(9) Å3, K0 =179(10) GPa, and K' = 3.9(9) up to 29 GPa. A distortive phase transition was discovered at higher pressures to a CaAl2O4-type orthorhombic structure, with two cubic unit-cell axes increasing and the third decreasing with increasing pressure. The transition can be fit to a Landau-type strain-order formulism with approximately 5% volume decrease from the cubic phase at 35 GPa. The transition may be triggered by electronic or magnetic transitions in the 3d elements Fe and Cr cations.

Type
Research Article
Copyright
Copyright © Materials Research Society 2007

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References

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