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Figure 5 | Progress in Earth and Planetary Science

Figure 5

From: Water-melt interaction in hydrous magmatic systems at high temperature and pressure

Figure 5

H 2 O solubility in silicate melts at low and high pressures as a function of fugacity of H 2 O, f H 2 O . (A) Solubility in SiO2 melt at and below ambient pressure from Moulson and Roberts (1961). (B) Solubility in SiO2 melt at high pressure as a function of f H 2 O from Kennedy et al. (1962). (C) Solubility in various silicate melts as a function of f H 2 O as compiled by McMillan (1994).

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