The prediction of methane solubility in natural waters to high ionic strength from 0 to 250C and from 0 to 1,600 bar

A model for the solubility of methane in brines (0-6 m) for temperatures from 0 to 250C and for pressures from 0 to 1,600 bar (or slightly above) is presented. The model is based on Pitzer phenomenology for the liquid phase and a highly accurate equation of state recently developed for the vapor pha...

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Veröffentlicht in:	Geochimica et cosmochimica acta 1992-04, Vol.56:4
Hauptverfasser:	Zhenhao Duan, Moeller, N., Greenberg, J., Weare, J.H.
Format:	Artikel
Sprache:	eng
Schlagworte:	152003 - Geothermal Data & Theory- Rock-Water-Gas Interactions 580000 - Geosciences ALKANES BRINES CALIFORNIA CHEMICAL COMPOSITION CHEMISTRY DEVELOPED COUNTRIES DISSOLVED GASES EQUATIONS EQUATIONS OF STATE FLUIDS GASES GEOCHEMISTRY GEOSCIENCES GEOTHERMAL ENERGY GEOTHERMAL FIELDS HYDROCARBONS HYDROGEN COMPOUNDS MATHEMATICAL MODELS METHANE NORTH AMERICA ORGANIC COMPOUNDS OXYGEN COMPOUNDS PARTIAL PRESSURE PHASE STUDIES PHASE TRANSFORMATIONS SALTON SEA GEOTHERMAL FIELD SEAWATER SOLUBILITY SOLUTES THERMODYNAMICS USA WATER
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