Two triple points in the H2O-H2 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 °C and at 3.6 kbar and 1 °C, respectively. Liquid water (L), low-pressure hexagonal ice (I h ) a...
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Published in | High pressure research Vol. 29; no. 2; pp. 250 - 253 |
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Main Authors | , , , , |
Format | Journal Article |
Language | English |
Published |
Taylor & Francis
01.06.2009
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Subjects | |
Online Access | Get full text |
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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 °C and at 3.6 kbar and 1 °C, respectively. Liquid water (L), low-pressure hexagonal ice (I
h
) and high-pressure cubic (sII) and rhombohedral (C
1
) clathrate hydrates were in equilibrium with gaseous hydrogen taken in excess.
†
This paper was presented at the XLVI
th
European High Pressure Research Group (EHPRG 46) Meeting, Valencia (Spain), 7-12 September, 2008. |
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ISSN: | 0895-7959 1477-2299 |
DOI: | 10.1080/08957950902734013 |