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Дата последнего поиска статьи во внешних источниках: 18 июля 2013 г.
Аннотация:Using a volumetric technique, phase transitions in the H2O-H2 system were investigated in the vicinity of two points of an invariant equilibrium, L+Ih+sII and L+sII+C1, located at 1.07kbar and-10C and at 3.6kbar and 1C, respectively. Liquid water (L), low-pressure hexagonal ice (Ih) and high-pressure cubic (sII) and rhombohedral (C1) clathrate hydrates were in equilibrium with gaseous hydrogen taken in excess.