Compressibility and phase transitions of potassium carbonate at pressures below 30 kbar


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The compressibility of γ-K2CO3 within the pressure range of 0.001-23.3 kbar and room temperature was determined by in situ synchrotron powder diffraction measurements in diamond anvil cell. The modification of the diffraction pattern was fixed at P > 23.3 kbar. This modification can be explained by a reconstructive phase transition. The amorphization of the high pressure phase was fixed on decompression.

作者简介

P. Gavryushkin

Sobolev Institute of Geology and Mineralogy, Siberian Branch; Novosibirsk National Research State University

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Email: gavryushkin@igm.nsc.ru
俄罗斯联邦, Novosibirsk; Novosibirsk

S. Rashenko

Sobolev Institute of Geology and Mineralogy, Siberian Branch; Novosibirsk National Research State University

Email: gavryushkin@igm.nsc.ru
俄罗斯联邦, Novosibirsk; Novosibirsk

A. Shatskiy

Sobolev Institute of Geology and Mineralogy, Siberian Branch; Novosibirsk National Research State University

Email: gavryushkin@igm.nsc.ru
俄罗斯联邦, Novosibirsk; Novosibirsk

K. Litasov

Sobolev Institute of Geology and Mineralogy, Siberian Branch; Novosibirsk National Research State University

Email: gavryushkin@igm.nsc.ru
俄罗斯联邦, Novosibirsk; Novosibirsk

A. Ancharov

Budker Institute of Nuclear Physics, Siberian Branch

Email: gavryushkin@igm.nsc.ru
俄罗斯联邦, Novosibirsk

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