Two triple points in the H(2)O-H(2) system

Using a volumetric technique, phase transitions in the H(2)O-H(2) system were investigated in the vicinity of two points of an invariant equilibrium, L + I(h)+ sII and L + sII + C(1), located at 1.07 kbar and -10 deg C and at 3.6 kbar and 1 deg C, respectively. Liquid water (L), low-pressure hexagon...

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Published inHigh pressure research Vol. 29; no. 2; pp. 250 - 253
Main Authors Efimchenko, V S, Antonov, V E, Barkalov, O I, Klyamkin, S N, Tkacz, M
Format Journal Article
LanguageEnglish
Published 01.06.2009
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Summary:Using a volumetric technique, phase transitions in the H(2)O-H(2) system were investigated in the vicinity of two points of an invariant equilibrium, L + I(h)+ sII and L + sII + C(1), located at 1.07 kbar and -10 deg C and at 3.6 kbar and 1 deg C, respectively. Liquid water (L), low-pressure hexagonal ice (ft) and high-pressure cubic (sII) and rhombohedral (C(1)) clathrate hydrates were in equilibrium with gaseous hydrogen taken in excess.
Bibliography:ObjectType-Article-2
SourceType-Scholarly Journals-1
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ISSN:0895-7959
DOI:10.1080/08957950902734013