메뉴 건너뛰기




Volumn 38, Issue 4, 2009, Pages 101-110

Kinetics of anorthite dissolution process on CO2 geological sequestration

Author keywords

Anorthite; CO2 geological sequestration; Dissolution rate; Feldspar; Gibbs free energy; Phase shift interferometry

Indexed keywords

ANORTHITE; CARBON DIOXIDE; CARBON SEQUESTRATION; COMPUTER SIMULATION; DISSOLUTION; FELDSPAR; FORMATION WATER; GIBBS FREE ENERGY; INTERFEROMETRY; NUMERICAL MODEL; PERMEABILITY; POROSITY; PRECIPITATION (CHEMISTRY); REACTION KINETICS; REACTION RATE; RESERVOIR ROCK;

EID: 69449092893     PISSN: 1345630X     EISSN: 13497979     Source Type: Journal    
DOI: 10.2465/gkk.38.101     Document Type: Article
Times cited : (2)

References (47)
  • 1
    • 0024258238 scopus 로고
    • The use of a surface complexation madel to describe the kinetics of ligand-promoted dissolution of anorthite
    • Amrhein, C. and Suarez, D.L. (1988): The use of a surface complexation madel to describe the kinetics of ligand-promoted dissolution of anorthite. Geochim. Cosmochim. Acta, 52, 2785-2793.
    • (1988) Geochim. Cosmochim. Acta , vol.52 , pp. 2785-2793
    • Amrhein, C.1    Suarez, D.L.2
  • 2
    • 30944462303 scopus 로고    scopus 로고
    • Albite dissolution kinetics as a function of distance from equilibrium: Implications for natural feldspar weathering
    • Beig, M.S. and Lüttge, A. (2006): Albite dissolution kinetics as a function of distance from equilibrium: Implications for natural feldspar weathering. Geochim. Cosmochim. Acta, 70, 1402-1420.
    • (2006) Geochim. Cosmochim. Acta , vol.70 , pp. 1402-1420
    • Beig, M.S.1    Lüttge, A.2
  • 3
    • 0034006745 scopus 로고    scopus 로고
    • Carbon dioxide mediated dissolution of Ca-feldspar: Implications for silicate weathering
    • Berg, A. and Banwart, S.A. (2000): Carbon dioxide mediated dissolution of Ca-feldspar: implications for silicate weathering. Chem. Geol., 163, 25-42.
    • (2000) Chem. Geol , vol.163 , pp. 25-42
    • Berg, A.1    Banwart, S.A.2
  • 4
    • 0033452481 scopus 로고    scopus 로고
    • Kinetics of feldspar and quartz dissolution at 70-80°C and near-neutral pH: Effects of organic acids-and NaCl
    • Blake, R.E. and Walter, L.M. (1999): Kinetics of feldspar and quartz dissolution at 70-80°C and near-neutral pH: Effects of organic acids-and NaCl. Geochim. Cosmochim. Acta, 63, 2043-2059.
    • (1999) Geochim. Cosmochim. Acta , vol.63 , pp. 2043-2059
    • Blake, R.E.1    Walter, L.M.2
  • 5
    • 0001470940 scopus 로고    scopus 로고
    • Feldspar dissolution at 25°C and low pH
    • Brantley, S.L. and Stillings, L. (1996): Feldspar dissolution at 25°C and low pH. Amer. J. Science, 296, 101-127.
    • (1996) Amer. J. Science , vol.296 , pp. 101-127
    • Brantley, S.L.1    Stillings, L.2
  • 6
    • 0027510808 scopus 로고
    • Free energy dependence of albite dissolution kinetics at 80°C and pH 8.8
    • Burch, T.E., Nagy, K.L. and Lasaga, A.C. (1993): Free energy dependence of albite dissolution kinetics at 80°C and pH 8.8. Chem. Geol. 105, 137-162.
    • (1993) Chem. Geol , vol.105 , pp. 137-162
    • Burch, T.E.1    Nagy, K.L.2    Lasaga, A.C.3
  • 7
    • 84996222466 scopus 로고
    • On the dislocation theory of evaporation of crystals
    • Cabrera, N. and Levine, M.M. (1956); On the dislocation theory of evaporation of crystals, Philosoph. Mag., 1, 450-458.
    • (1956) Philosoph. Mag , vol.1 , pp. 450-458
    • Cabrera, N.1    Levine, M.M.2
  • 9
    • 0030745231 scopus 로고    scopus 로고
    • Temperature- and pH-dependence of albite dissolution rate at acid pH
    • Chen, Y. and Brantley, S.L. (1997): Temperature- and pH-dependence of albite dissolution rate at acid pH. Chem. Geol, 135, 275-290.
    • (1997) Chem. Geol , vol.135 , pp. 275-290
    • Chen, Y.1    Brantley, S.L.2
  • 10
    • 0022264795 scopus 로고
    • Steady-state kinetics and dissolution mechanisms of albite
    • Chou, L. and Wollast, R. (1985): Steady-state kinetics and dissolution mechanisms of albite. Amer. J. Sci., 285, 963-993.
    • (1985) Amer. J. Sci , vol.285 , pp. 963-993
    • Chou, L.1    Wollast, R.2
  • 12
    • 0028583442 scopus 로고
    • Experimental study of K-feldspar dissolution rates as a function of chemical affinity at 150 °C and pH 9
    • Gautier, J.-M., Oelkers, E.H. and Schott, J. (1994): Experimental study of K-feldspar dissolution rates as a function of chemical affinity at 150 °C and pH 9. Geochim. Cosmochim. Acta, 58, 4549-4560.
    • (1994) Geochim. Cosmochim. Acta , vol.58 , pp. 4549-4560
    • Gautier, J.-M.1    Oelkers, E.H.2    Schott, J.3
  • 13
    • 0028315168 scopus 로고
    • The albite-water system, Part 1. The kinetics of dissolution as a function of pH at 100, 200, and 300 °C
    • Hellmann, R. (1994): The albite-water system, Part 1. The kinetics of dissolution as a function of pH at 100, 200, and 300 °C. Geochim. Cosmochim. Acta, 58, 595-611.
    • (1994) Geochim. Cosmochim. Acta , vol.58 , pp. 595-611
    • Hellmann, R.1
  • 14
    • 0028830558 scopus 로고
    • The albite-water system: Part 11. The time-evolution of the stoichiometry of dissolution as a function of pH at 100, 200, and 300 °C
    • Hellmann, R. (1995): The albite-water system: Part 11. The time-evolution of the stoichiometry of dissolution as a function of pH at 100, 200, and 300 °C. Geochim. Cosmochim. Acta, 59, 1669-1697.
    • (1995) Geochim. Cosmochim. Acta , vol.59 , pp. 1669-1697
    • Hellmann, R.1
  • 15
    • 30944469827 scopus 로고    scopus 로고
    • Dissolution kinetics as a function of the Gibbs free energy of reaction: An experimental study based on albite feldspar
    • Hellmann, R. and Tisserand, D. (2006): Dissolution kinetics as a function of the Gibbs free energy of reaction: An experimental study based on albite feldspar. Geochim. Cosmochim. Acta, 70, 364-383.
    • (2006) Geochim. Cosmochim. Acta , vol.70 , pp. 364-383
    • Hellmann, R.1    Tisserand, D.2
  • 16
    • 33644970107 scopus 로고    scopus 로고
    • Does reactive surfaee area depend on grain size- Results from pH 3, 25 °C far-from-equilibrium flow-through dissolution experiments on anorthite and biotite
    • Hodson, M.E. (2006): Does reactive surfaee area depend on grain size- Results from pH 3, 25 °C far-from-equilibrium flow-through dissolution experiments on anorthite and biotite. Geochim. Cosmochim. Acta, 70, 1655-1667.
    • (2006) Geochim. Cosmochim. Acta , vol.70 , pp. 1655-1667
    • Hodson, M.E.1
  • 17
    • 0022264793 scopus 로고
    • pH dependent changes in the rates and stoichiometry of dissolution of an alkali feldspar at room temperature
    • Holdren, Jr.,G.R. and Speyer, P.M. (1985a): pH dependent changes in the rates and stoichiometry of dissolution of an alkali feldspar at room temperature. Amer. J. Sci., 285, 994-1026.
    • (1985) Amer. J. Sci , vol.285 , pp. 994-1026
    • Holdren Jr., G.R.1    Speyer, P.M.2
  • 18
    • 0021890368 scopus 로고    scopus 로고
    • (1085b): Reaction rate-surface area relationships during the early stages of weathering - I. Initial observations
    • Holdren, Jr.,G.R. and Speyer; P.M. (1085b): Reaction rate-surface area relationships during the early stages of weathering - I. Initial observations. Geochim. Cosmochim, Acta, 49, 675-681.
    • Geochim. Cosmochim, Acta , vol.49 , pp. 675-681
    • Holdren Jr., G.R.1    Speyer, P.M.2
  • 19
    • 0023525275 scopus 로고
    • Reaction rate-surface area relationships during the early stages of weathering - II. Data on eight additional feldspars
    • Holdren, Jr.,G.R. and Speyer, P.M. (1987): Reaction rate-surface area relationships during the early stages of weathering - II. Data on eight additional feldspars. Geochim. Cosmochim. Acta, 51, 2311-2318.
    • (1987) Geochim. Cosmochim. Acta , vol.51 , pp. 2311-2318
    • Holdren Jr., G.R.1    Speyer, P.M.2
  • 20
    • 69449089280 scopus 로고    scopus 로고
    • IPCC (2005): Beason, S., Cook, P. (Coordinating lead authors), Underground geological storage. In IPCC Special Report on Carbon Dioxide Capture and Storage (Metz, B., Davidson, O., Coninck, H., Loos, M. and Meyer, L. Eds.). Cambridge University Press, 195-276.
    • IPCC (2005): Beason, S., Cook, P. (Coordinating lead authors), Underground geological storage. In IPCC Special Report on Carbon Dioxide Capture and Storage (Metz, B., Davidson, O., Coninck, H., Loos, M. and Meyer, L. Eds.). Cambridge University Press, 195-276.
  • 22
    • 0022899342 scopus 로고
    • Dependence of albite dissolution kinetics on pH and time at 25 °C and 70 °C
    • Knauss, K.G. and Wolery, T.J. (1986): Dependence of albite dissolution kinetics on pH and time at 25 °C and 70 °C. Geochim. Cosmochim. Acta, 50, 2481-2497.
    • (1986) Geochim. Cosmochim. Acta , vol.50 , pp. 2481-2497
    • Knauss, K.G.1    Wolery, T.J.2
  • 23
    • 33746231473 scopus 로고    scopus 로고
    • Theory of crystal growth and dissolution
    • Princeton
    • Lasaga, A.C. (1998): Theory of crystal growth and dissolution. In Kinetic theory in the Earth sciences. Princeton, 581-712.
    • (1998) Kinetic theory in the Earth sciences , pp. 581-712
    • Lasaga, A.C.1
  • 24
    • 0035937547 scopus 로고    scopus 로고
    • Variation of crystal dissolution rate based on a dissolution stepwave model
    • Lasaga, A.C. and Lüttge, A. (2001): Variation of crystal dissolution rate based on a dissolution stepwave model. Science, 291, 2400-2404.
    • (2001) Science , vol.291 , pp. 2400-2404
    • Lasaga, A.C.1    Lüttge, A.2
  • 25
    • 28444454825 scopus 로고    scopus 로고
    • Crystal dissolution kinetics and Gibbs free energy
    • Lüttge, A. (2006): Crystal dissolution kinetics and Gibbs free energy. J. Elect. Spectro. Related Phenomena, 150, 248-259.
    • (2006) J. Elect. Spectro. Related Phenomena , vol.150 , pp. 248-259
    • Lüttge, A.1
  • 26
    • 0040531893 scopus 로고    scopus 로고
    • An interferometric study of the dissolution kinetics of anorthite: The role of reactive surface area
    • Lüttge, A., Bolton, E.W. and Lasaga, A.C. (1999): An interferometric study of the dissolution kinetics of anorthite: the role of reactive surface area. Amer. J. Sci., 299, 652-678.
    • (1999) Amer. J. Sci , vol.299 , pp. 652-678
    • Lüttge, A.1    Bolton, E.W.2    Lasaga, A.C.3
  • 27
    • 0027042006 scopus 로고
    • Dissolution and precipitation kinetics of gibbsite at 80 °C and pH 3: The dependence on solution saturation state
    • Nagy, K.L. and Lasaga, A.C. (1992): Dissolution and precipitation kinetics of gibbsite at 80 °C and pH 3: The dependence on solution saturation state. Geochim. Cosmochim. Acta, 56, 3093-3111.
    • (1992) Geochim. Cosmochim. Acta , vol.56 , pp. 3093-3111
    • Nagy, K.L.1    Lasaga, A.C.2
  • 28
    • 0028254135 scopus 로고
    • The effect of aluminum, pH, and chemical affinity on the rates of aluminosilicate dissolution reactions
    • Oelkers, E.H., Schott, J. and Devidal, J.-L. (1994): The effect of aluminum, pH, and chemical affinity on the rates of aluminosilicate dissolution reactions. Geochim. Cosmochim. Acta, 58, 2011-2024.
    • (1994) Geochim. Cosmochim. Acta , vol.58 , pp. 2011-2024
    • Oelkers, E.H.1    Schott, J.2    Devidal, J.-L.3
  • 29
    • 0029479427 scopus 로고
    • Experimental study of anorthite dissolution and the relative mechanism of feldspar hydrolysis
    • Oelkers, E.H. and Schott, J. (1995): Experimental study of anorthite dissolution and the relative mechanism of feldspar hydrolysis. Geochim. Cosmochim. Acta, 59, 5039-5053.
    • (1995) Geochim. Cosmochim. Acta , vol.59 , pp. 5039-5053
    • Oelkers, E.H.1    Schott, J.2
  • 30
    • 0003396170 scopus 로고    scopus 로고
    • User's guide to PHREEQC (Version 2) - A computer program for speciation, batch-reaction, one-dimensional transport, and inverse geochemical calculations: U.S
    • 99-4259, pp
    • Parkhurst, D.L. and Appelo, C.A.J. (1999): User's guide to PHREEQC (Version 2) - A computer program for speciation, batch-reaction, one-dimensional transport, and inverse geochemical calculations: U.S. Geological Survey Water-Resources Investigations Report 99-4259, pp. 312.
    • (1999) Geological Survey Water-Resources Investigations Report , pp. 312
    • Parkhurst, D.L.1    Appelo, C.A.J.2
  • 31
    • 69449089846 scopus 로고    scopus 로고
    • Palandri, J.L. and Kharaka, Y.K. (2004): A compilation of rate parameters of water-mineral interaction kinetics for application to geochemical modeling, U.S. Geological Survey, Open file report 2004-1068.
    • Palandri, J.L. and Kharaka, Y.K. (2004): A compilation of rate parameters of water-mineral interaction kinetics for application to geochemical modeling, U.S. Geological Survey, Open file report 2004-1068.
  • 34
    • 0025591789 scopus 로고
    • A new kinetic approach to modeling water-rock interaction: The role of nucleation, precursors, and Ostwald ripening
    • Steefel, C.I. and Van Cappellen, P. (1990): A new kinetic approach to modeling water-rock interaction: The role of nucleation, precursors, and Ostwald ripening. Geochim. Cosmochim. Acta, 54, 2657-2677.
    • (1990) Geochim. Cosmochim. Acta , vol.54 , pp. 2657-2677
    • Steefel, C.I.1    Van Cappellen, P.2
  • 35
    • 0028826799 scopus 로고    scopus 로고
    • (199-5): Feldspar dissolution at 25 °C and pH 3: Reaction steichiometry and the effect of cations
    • Stillings, L.L. and Brantley, S.L. (199-5): Feldspar dissolution at 25 °C and pH 3: Reaction steichiometry and the effect of cations. Geochim. Cosmochim. Acta, 59, 1483-1496.
    • Geochim. Cosmochim. Acta , vol.59 , pp. 1483-1496
    • Stillings, L.L.1    Brantley, S.L.2
  • 36
    • 0030423865 scopus 로고    scopus 로고
    • Rates of feldspar dissolution at pH 3-7 with 0-8 mM oxalic acid
    • Stillings, L.L., Drever, J.I., Brantley, S.L., Sun. Y. and Oxburgh, R. (1996): Rates of feldspar dissolution at pH 3-7 with 0-8 mM oxalic acid. Chem. Geol., 132, 79-89.
    • (1996) Chem. Geol , vol.132 , pp. 79-89
    • Stillings, L.L.1    Drever, J.I.2    Brantley, S.L.3    Sun, Y.4    Oxburgh, R.5
  • 37
    • 0033940757 scopus 로고    scopus 로고
    • The dependence of labradorite dissolution and Sr isotope release rates on solution saturation state
    • Taylor, A.S., Blum, J.D. and Lasaga, A.C. (2000): The dependence of labradorite dissolution and Sr isotope release rates on solution saturation state. Geochim. Cosmochim. Acta, 64, 2389-2400.
    • (2000) Geochim. Cosmochim. Acta , vol.64 , pp. 2389-2400
    • Taylor, A.S.1    Blum, J.D.2    Lasaga, A.C.3
  • 38
    • 0035209797 scopus 로고    scopus 로고
    • Resolving orthoclase dissolution processes with atomic force microscopy and X-ray reflectivity
    • Teng, H.H., Fenter, P., Cheng, L. and Sturchio, N.C. (2001): Resolving orthoclase dissolution processes with atomic force microscopy and X-ray reflectivity. Geochim. Cosmochim. Acta, 65, 3459-3474.
    • (2001) Geochim. Cosmochim. Acta , vol.65 , pp. 3459-3474
    • Teng, H.H.1    Fenter, P.2    Cheng, L.3    Sturchio, N.C.4
  • 39
    • 0942299935 scopus 로고    scopus 로고
    • Controls by saturation state on etch pit formation during calcite dissolution
    • Teng, H.H. (2004): Controls by saturation state on etch pit formation during calcite dissolution. Geochim. Cosmochim. Acta, 68, 253-262.
    • (2004) Geochim. Cosmochim. Acta , vol.68 , pp. 253-262
    • Teng, H.H.1
  • 40
    • 69449095719 scopus 로고    scopus 로고
    • Tullis, J. (1983): Deformation of feldspars. In Feldspar Mineralogy (Ribbe, P.H., Ed.). Mineral. Soc. Amer., Rev. Mineral., 2, 297-323.
    • Tullis, J. (1983): Deformation of feldspars. In Feldspar Mineralogy (Ribbe, P.H., Ed.). Mineral. Soc. Amer., Rev. Mineral., 2, 297-323.
  • 41
    • 0005550495 scopus 로고    scopus 로고
    • The effect of partial pressure. of carbon dioxide on anorthite dissolution
    • Utsunomiya, S., Murakami, T., Kadohara, H. and Tsukimura, K. (1999): The effect of partial pressure. of carbon dioxide on anorthite dissolution. Mineral. J., 21, 1-8.
    • (1999) Mineral. J , vol.21 , pp. 1-8
    • Utsunomiya, S.1    Murakami, T.2    Kadohara, H.3    Tsukimura, K.4
  • 42
    • 0030517823 scopus 로고    scopus 로고
    • Feldspar dissolution in acidic and organic solutions: Compositional and pH dependence of dissolution rate
    • Welch, S.A. and Ullman, W.J. (1996): Feldspar dissolution in acidic and organic solutions: Compositional and pH dependence of dissolution rate. Geochim. Cosmochim. Acta, 60, 2939-2948.
    • (1996) Geochim. Cosmochim. Acta , vol.60 , pp. 2939-2948
    • Welch, S.A.1    Ullman, W.J.2
  • 43
    • 0034113449 scopus 로고    scopus 로고
    • The temperature dependence of bytownite feldspar dissolution in neutral aqueous solutions of inorganic and organic ligands at low temperature (5-35 °C)
    • Welch, S.A. and Ullman, W.J. (2000): The temperature dependence of bytownite feldspar dissolution in neutral aqueous solutions of inorganic and organic ligands at low temperature (5-35 °C). Chem. Geol., 167, 337-354.
    • (2000) Chem. Geol , vol.167 , pp. 337-354
    • Welch, S.A.1    Ullman, W.J.2
  • 44
    • 0003596807 scopus 로고    scopus 로고
    • Coupled modeling of non-isothermal multiphase flow, solute transport and reactive chemistry in porous and fractured media: 1. Model development and validation
    • LBNL-42050, Berkeley, California
    • Xu, T. and Pruess, K. (1998): Coupled modeling of non-isothermal multiphase flow, solute transport and reactive chemistry in porous and fractured media: 1. Model development and validation. Lawrence Berkeley National Laboratory Report LBNL-42050, Berkeley, California.
    • (1998) Lawrence Berkeley National Laboratory Report
    • Xu, T.1    Pruess, K.2
  • 45
    • 0035073183 scopus 로고    scopus 로고
    • On fluid flow and mineral alteration in fractured caprock of magmatic hydrothermal systems
    • Xu, T. and Pruess, K. (2001): On fluid flow and mineral alteration in fractured caprock of magmatic hydrothermal systems. J. Geophys. Res., 106, 2121-2138.
    • (2001) J. Geophys. Res , vol.106 , pp. 2121-2138
    • Xu, T.1    Pruess, K.2
  • 46
    • 18444364508 scopus 로고    scopus 로고
    • Mineral sequestration of carbon dioxide in a sandstone - hale system
    • Xu, T., Apps, J.A. and Pruess, K. (2005): Mineral sequestration of carbon dioxide in a sandstone - hale system. Chem. Geol., 217, 295-318.
    • (2005) Chem. Geol , vol.217 , pp. 295-318
    • Xu, T.1    Apps, J.A.2    Pruess, K.3
  • 47
    • 20744444271 scopus 로고    scopus 로고
    • 2 sequestration potential in the Haizume Formation, Niigata Basin, Japan. Oil Gas Sci. Tech., 60, 249-258.
    • 2 sequestration potential in the Haizume Formation, Niigata Basin, Japan. Oil Gas Sci. Tech., 60, 249-258.


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.