CO2-H2O MIXTURES IN THE GEOLOGICAL SEQUESTRATION OF CO2. II. PARTITIONING IN CHLORIDE BRINES AT 12-100°C AND UP TO 600 BAR

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dc.contributor.author Spycher N.
dc.contributor.author Pruess K.
dc.date.accessioned 2023-11-18T10:28:17Z
dc.date.available 2023-11-18T10:28:17Z
dc.date.issued 2005
dc.identifier https://www.elibrary.ru/item.asp?id=12092171
dc.identifier.citation Geochimica et Cosmochimica Acta, 2005, 69, 13, 3309-3320
dc.identifier.issn 0016-7037
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/41867
dc.description.abstract Correlations presented by Spycher et al. (2003) to compute the mutual solubilities of CO2 and H2O are extended to include the effect of chloride salts in the aqueous phase. This is accomplished by including, in the original formulation, activity coefficients for aqueous CO2 derived from several literature sources, primarily for NaCl solutions. Best results are obtained when combining the solubility correlations of Spycher et al. (2003) with the activity coefficient formulation of Rumpf et al. (1994) and Duan and Sun (2003), which can be extended to chloride solutions other than NaCl. This approach allows computing mutual solubilities in a noniterative manner with an accuracy typically within experimental uncertainty for solutions up to 6 molal NaCl and 4 molal CaCl2.
dc.title CO2-H2O MIXTURES IN THE GEOLOGICAL SEQUESTRATION OF CO2. II. PARTITIONING IN CHLORIDE BRINES AT 12-100°C AND UP TO 600 BAR
dc.type Статья
dc.identifier.doi 10.1016/j.gca.2005.01.015


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