The CO2-H2O system. II. Calculated thermodynamic mixing properties for 400°C, 0-400 MPa

James G. Blencoe, Jeffery C. Seitz, Lawrence M. Anovitz

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Abstract

An excess molar volume (V(ex))-explicit virial equation, and two empirical V(ex) expressions developed from experimentally determined densities, were used to calculate excess Gibbs free energies (G(ex)) and activity-composition (a-X) relations for CO2-H2O fluids at 400°C, 0-400 MPa. Excess Gibbs free energies are continuously positive and asymmetric toward H2O at all pressures up to 400 MPa, rising to peak values of approximately 1300, 1800, 2000 and 2100 J · mol-1 at 50, 100, 200 and 400 MPa, respectively. Calculated activities for H2O and CO2 vary correspondingly, increasing substantially from 0 to 100 MPa, moderately from 100 to 200 MPa, and slightly from 200 to 400 MPa. In addition, because G(ex) is asymmetric toward H2O, a-X relations for H2O are distinctly different from those for CO2. These results indicate that CO2-H2O fluids are strongly nonideal at 400°C and all pressures above ~30 MPa, despite the fact that peak values for V(ex) decrease from ~50 cm3 · mol-1 at 30 MPa to ~1 cm3 · mol-1 at 200 MPa, and remain small to pressures at least as high as 500 MPa. Excess Gibbs free energies and a-X relations for CO2-H2O fluids at 400°C and pressures to 400 MPa calculated from modified Redlich-Kwong and Lee-Kesler equations of state generally suggest significantly smaller positive deviations from ideality.

Original languageEnglish
Pages (from-to)2393-2408
Number of pages16
JournalGeochimica et Cosmochimica Acta
Volume63
Issue number16
DOIs
StatePublished - Aug 1999

Funding

Reviews by J. M. Simonson and three anonymous reviewers are gratefully acknowledged. Regression calculations were performed using a Mathematica program developed by R. H. Wood and R. W. Carter. Thermophysical properties given by the Duan et al. (1992a, b) model were obtained from a computer-executable file provided by Z. Duan. Discussions with T. Chacko led to significant improvements in treating uncertainties. M. S. Gruszkiewicz and S. L. Marshall offered helpful comments concerning the strengths and weaknesses of various approaches to developing equations of state for high-temperature fluids. Funding for the research was provided by the Division of Engineering and Geosciences, Office of Basic Energy Sciences, U.S. Department of Energy, under Contract DE-AC05-96OR22464 with Oak Ridge National Laboratory, managed by Lockheed Martin Energy Research Corporation. Funding for J.C.S. was provided by: (1) the Distinguished Postdoctoral Research Program sponsored by the U.S. Department of Energy, Office of Science and Technical Information, and administered by the Oak Ridge Institute for Science and Education; and (2) the U.S. Department of Energy, Environmental Management Science Program (TTP OR17-SP22), under contract number DE-AC05-96OR22464 with Oak Ridge National Laboratory, managed by Lockheed Martin Energy Research Corporation.

FundersFunder number
Division of Engineering and Geosciences
Lockheed Martin Energy Research Corporation
Office of Science and Technical Information
U.S. Department of Energy, Environmental Management Science ProgramTTP OR17-SP22
U.S. Department of EnergyDE-AC05-96OR22464
Basic Energy Sciences
Oak Ridge National Laboratory
Oak Ridge Institute for Science and Education

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