Pressure-Induced Crossover between Diffusive and Displacive Mechanisms of Phase Transitions in Single-Crystalline αGeO2

V. V. Brazhkin, A. G. Lyapin, R. N. Voloshin, S. V. Popova, E. V. Tat’yanin, N. F. Borovikov, S. C. Bayliss, and A. V. Sapelkin
Phys. Rev. Lett. 90, 145503 – Published 11 April 2003

Abstract

We present the first example of the phase transition occurring via the different kinetic mechanisms, displacive or diffusive, competing with each other in quartzlike αGeO2 single crystals. Upon room-pressure heating, αGeO2 transforms to the rutile-type phase (the αr transition) via the diffusive mechanism. With increase of the treatment pressure the diffusive mode of the temperature-induced αr transition is substituted at 4GPa by a displacivelike mode, and then at 6GPa the transition type changes from the αr sequence to a displacive martensiticlike transition to a distorted rutilelike phase (αr. A crossover between diffusive and displacive transition modes suggests a new way to control the meso- and nanometer-scale morphology of high-pressure phases.

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  • Received 15 August 2002

DOI:https://doi.org/10.1103/PhysRevLett.90.145503

©2003 American Physical Society

Authors & Affiliations

V. V. Brazhkin, A. G. Lyapin*, R. N. Voloshin, S. V. Popova, E. V. Tat’yanin, and N. F. Borovikov

  • Institute for High Pressure Physics, Russian Academy of Sciences, Troitsk, Moscow region, 142190, Russia

S. C. Bayliss and A. V. Sapelkin

  • Department of Chemistry, School of Applied Sciences, De Montfort University, The Gateway, Leicester, LE1 9BH, United Kingdom

  • *Electronic address: alyapin@hppi.troitsk.ru

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Vol. 90, Iss. 14 — 11 April 2003

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