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This article is cited in 40 scientific papers (total in 40 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.
Citation:
Yu. A. Dyadin, E. G. Larionov, D. S. Mirinskii, T. V. Mikina, L. I. Starostina, “Clathrate formation in the Ar–H2O system under pressures up to 15000 bar”, Mendeleev Commun., 7:1 (1997), 32–34
Linking options:
https://www.mathnet.ru/eng/mendc4768 https://www.mathnet.ru/eng/mendc/v7/i1/p32
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