Reactive transport modelling of CO2 storage in saline aquifers to elucidate fundamental processes, trapping mechanisms and sequestration partitioning
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[1] A. Blum,et al. Chapter 7. FELDSPAR DISSOLUTION KINETICS , 1995 .
[2] J. Nitao,et al. Reactive Transport Modeling of Geologic CO2 Sequestration at Sleipner , 2003 .
[3] P. Bergmo,et al. The Long-Term Fate of CO2 Injected into an Aquifer , 2003 .
[4] W. Wakeham,et al. The Viscosity of Carbon Dioxide , 1998 .
[5] J. C. Baker,et al. Continental-scale magmatic carbon-dioxide seepage recorded by Dawsonite in the Bowen-Gunnedah-Sydney Basin System, eastern Australia , 1995 .
[6] Lincoln Paterson,et al. Rate of Dissolution Due to Convective Mixing in the Underground Storage of Carbon Dioxide , 2003 .
[7] K. Knauss,et al. The effect of malonate on the dissolution kinetics of albite, quartz, and microcline as a function of pH at 70°C , 1995 .
[8] H. Barnes,et al. Precipitation and dissolution rate constants for cristobalite from 150 to 300°C , 1995 .
[9] R. Garrels,et al. Solutions, Minerals and Equilibria , 1965 .
[10] Jack C. Parker,et al. A parametric model for constitutive properties governing multiphase flow in porous media , 1987 .
[11] K. Knauss,et al. The dissolution kinetics of quartz as a function of pH and time at 70°C , 1988 .
[12] A. Blum,et al. Feldspar dissolution kinetics , 1995 .
[13] R. A. Robie,et al. Thermodynamic properties of minerals and related substances at 298.15 K and 1 bar (10[5] pascals) pressure and at higher temperatures , 1995 .
[14] Guntram Jordan,et al. Dissolution Rates of Calcite (104) Obtained by Scanning Force Microscopy: Microtopography-Based Dissolution Kinetics on Surfaces with Anisotropic Step Velocities , 1998 .
[15] S. Brantley,et al. Chemical weathering rates of silicate minerals , 1995 .
[16] E. Oelkers,et al. Calculation of the thermodynamic properties of aqueous species at high pressures and temperatures. Effective electrostatic radii, dissociation constants and standard partial molal properties to 1000 °C and 5 kbar , 1992 .
[17] H. Helgeson,et al. Thermodynamics of hydrothermal systems at elevated temperatures and pressures , 1969 .
[18] N. P. Fofonoff,et al. Algorithms for Computation of Fundamental Properties of Seawater. Endorsed by Unesco/SCOR/ICES/IAPSO Joint Panel on Oceanographic Tables and Standards and SCOR Working Group 51. Unesco Technical Papers in Marine Science, No. 44. , 1983 .
[19] Ola Eiken,et al. Seismic Monitoring of CO2 Injected Into a Marine Acquifer , 2000 .
[20] Oleg S. Pokrovsky,et al. Processes at the magnesium-bearing carbonates/solution interface. II. kinetics and mechanism of magnesite dissolution. , 1999 .
[21] Carl I. Steefel,et al. Reactive Transport Modeling of Geologic CO{sub 2} Sequestration in Saline Aquifers: The Influence of Intra-Aquifer Shales and the Relative Effectiveness of Structural, Solubility, and Mineral Trapping During Prograde and Retrograde Sequestration , 2001 .
[22] J. Tester,et al. Correlating quartz dissolution kinetics in pure water from 25 to 625°C , 1994 .
[23] Maxwell N. Watson,et al. The Ladbroke Grove-Katnook carbon dioxide natural laboratory: A recent CO2 accumulation in a lithic sandstone reservoir , 2004 .
[24] J. Drever,et al. rates of feldspar dissolution at pH 3–7 with 0–8 m M oxalic acid , 1996 .
[25] K. L. Nagy,et al. Chapter 5. DISSOLUTION AND PRECIPITATION KINETICS OF SHEET SILICATES , 1995 .
[26] E. C. Beutner. Slaty cleavage and related strain in Martinsburg Slate, Delaware Water Gap, New Jersey , 1978 .
[27] Denis Norton,et al. Theory of Hydrothermal Systems , 1984 .
[28] James W. Johnson,et al. Critical phenomena in hydrothermal systems; state, thermodynamic, electrostatic, and transport properties of H 2 O in the critical region , 1991 .
[29] Susan D. Hovorka,et al. Frio brine sequestration pilot in the Texas Gulf Coast , 2003 .
[30] Kevin G. Knauss,et al. Reactive transport modeling of plug-flow reactor experiments: quartz and tuff dissolution at 240°C , 1998 .
[31] W. Wagner,et al. A New Equation of State for Carbon Dioxide Covering the Fluid Region from the Triple‐Point Temperature to 1100 K at Pressures up to 800 MPa , 1996 .
[32] H. Helgeson,et al. Calculation of the thermodynamic and transport properties of aqueous species at high pressures and temperatures; revised equations of state for the standard partial molal properties of ions and electrolytes , 1988 .
[33] Adrian E. Scheidegger,et al. The physics of flow through porous media , 1957 .
[34] E. Oelkers,et al. SUPCRT92: a software package for calculating the standard molal thermodynamic properties of minerals, gases, aqueous species, and reactions from 1 to 5000 bar and 0 to 1000 ° C , 1992 .
[35] H. Helgeson,et al. Summary and critique of the thermodynamic properties of rock forming minerals , 1978 .
[36] J. H. Stewart. Origin of Sedimentary Rocks , 1974 .
[37] K. Knauss,et al. Muscovite dissolution kinetics as a function of pH and time at 70°C , 1989 .
[38] Mark H. Holtz,et al. Residual Gas Saturation to Aquifer Influx: A Calculation Method for 3-D Computer Reservoir Model Construction , 2002 .
[39] Lincoln Paterson,et al. Role of Convective Mixing in the Long-Term Storage of Carbon Dioxide in Deep Saline Formations , 2005 .
[40] B. Fritz,et al. Hydrothermal experiments and thermo-kinetic modelling of water-sandstone interactions☆ , 1994 .
[41] K. Knauss,et al. Dependence of albite dissolution kinetics on ph and time at 25°c and 70°c , 1986 .
[42] A. Lasaga. Kinetic theory in the earth sciences , 1998 .
[43] Kathryn L. Nagy,et al. Dissolution and precipitation kinetics of sheet silicates , 1995 .