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• W1990732046 startingPage "1595" @default.
• W1990732046 abstract "Hydrogen isotope fractionation factors were measured for coexisting brines and vapors formed by phase separation of NaCl/H2O fluids at temperatures ranging from 399–450°C and pressures from 277–397 bars. It was found that brines are depleted in D compared to coexisting vapors at all conditions studied. The magnitude of hydrogen isotope fractionation is dependent on the relative amounts of Cl in the two phases and can be empirically correlated to pressure using the following relationship: 1000 In α(vap-brine) = 2.54(±0.83) + 2.87 (±0.69) × log (ΔP), where α(vap-brine) is the fractionation factor and ΔP is a pressure term representing distance from the critical curve in the NaCl/H2O system." @default.
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• W1990732046 date "1996-05-01" @default.
• W1990732046 modified "2023-10-14" @default.
• W1990732046 title "Hydrogen isotope systematics of phase separation in submarine hydrothermal systems: Experimental calibration and theoretical models" @default.
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• W1990732046 doi "https://doi.org/10.1016/0016-7037(96)00033-6" @default.
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