1993
DOI: 10.1007/bf00852521
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Thermodynamic properties and thermal equations of the state of high-pressure ice phases

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Cited by 36 publications
(38 citation statements)
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“…In contrast with "lithostatic" pressure, which is weaker at shallow depth, the order of magnitude of tectonic stresses remains unknown. Despite this uncertainty, melting of pure water ice is impossible below 250 K (Chizhov, 1993). However, mixed compounds decrease the water liquidus temperature ( fig.…”
Section: Discussionmentioning
confidence: 99%
See 1 more Smart Citation
“…In contrast with "lithostatic" pressure, which is weaker at shallow depth, the order of magnitude of tectonic stresses remains unknown. Despite this uncertainty, melting of pure water ice is impossible below 250 K (Chizhov, 1993). However, mixed compounds decrease the water liquidus temperature ( fig.…”
Section: Discussionmentioning
confidence: 99%
“…In this way, crustal recycling zones on Europa would be associated to a warm crustal context rather than a cold region like the Earth subduction zones. (Chizhov, 1993), 15 % NH 3 (Grasset et al, 1995), 32.1 % and 50.25 % NH 3 (Hogenboom et al, 1997)]. L and S on each side of the curves refer to liquid and solid states.…”
Section: Discussionmentioning
confidence: 99%
“…Because the Hugoniot of ice enters the liquid water fields at 9.2 GPa (Stewart and Ahrens, 2005), we applied the parameter of liquid water from 9.2 GPa. The values of C v are 1390 J kg -1 K -1 for ice (Chizhov, 1993) and 3420 J kg -1 K -1 for liquid water (Stewart and Ahrens, 2005). The γ values of ice and liquid water were referred to by Leadbetter (1965) and Stewart and Ahrens (2005), respectively.…”
Section: Calculation Of the Parameters Related To Impact Shock Conditionmentioning
confidence: 99%
“…where F is the vertical heat flow through the shell, and b is the real ice shell thickness corresponding to F. T b obviously corresponds to the melting point of water ice, which is a function of pressure (Chizhov, 1993):…”
Section: Methodsmentioning
confidence: 99%