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JOURNALS // Mendeleev Communications // Archive

Mendeleev Commun., 1997 Volume 7, Issue 1, Pages 32–34 (Mi mendc4768)

This article is cited in 35 papers

Clathrate formation in the Ar–H2O system under pressures up to 15000 bar

Yu. A. Dyadin, E. G. Larionov, D. S. Mirinskii, T. V. Mikina, L. I. Starostina

A.V. Nikolaev Institute of Inorganic Chemistry, Siberian Branch of the Russian Academy of Sciences, Novosibirsk, Russian Federation

Abstract: Under pressure the decomposition curve of argon hydrate passes through a maximum (33.6 °C at ca. 6.2 kbar) and undergoes two breaks (at 7.2 and 9.6 kbar), indicating that three hydrates form in the Ar–H2O system; at 15 kbar the high pressure hydrate decomposes at 75.1°C.

Language: English

DOI: 10.1070/MC1997v007n01ABEH000650



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