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Acta Geotechnica

, Volume 11, Issue 5, pp 1167–1188 | Cite as

Impacts of mineralogical compositions on different trapping mechanisms during long-term CO2 storage in deep saline aquifers

  • Kairan Wang
  • Tianfu Xu
  • Hailong TianEmail author
  • Fugang Wang
Research Paper

Abstract

Deep saline aquifers in sedimentary basins are considered to have the greatest potential for CO2 geological storage in order to reduce carbon emissions. CO2 injected into a saline sandstone aquifer tends to migrate upwards toward the caprock because the density of the supercritical CO2 phase is lower than that of formation water. The accumulated CO2 in the upper portions of the reservoir gradually dissolves into brine, lowers pH and changes the aqueous complexation, whereby induces mineral alteration. In turn, the mineralogical composition could impose significant effects on the evolution of solution, further on the mineralized CO2. The high density of aqueous phase will then move downward due to gravity, give rise to “convective mixing,” which facilitate the transformation of CO2 from the supercritical phase to the aqueous phase and then to the solid phase. In order to determine the impacts of mineralogical compositions on trapping amounts in different mechanisms for CO2 geological storage, a 2D radial model was developed. The mineralogical composition for the base case was taken from a deep saline formation of the Ordos Basin, China. Three additional models with varying mineralogical compositions were carried out. Results indicate that the mineralogical composition had very obvious effects on different CO2 trapping mechanisms. Specific to our cases, the dissolution of chlorite provided Mg2+ and Fe2+ for the formation of secondary carbonate minerals (ankerite, siderite and magnesite). When chlorite was absent in the saline aquifer, the dominant secondary carbon sequestration mineral was dawsonite, and the amount of CO2 mineral trapping increased with an increase in the concentration of chlorite. After 3000 years, 69.08, 76.93, 83.52 and 87.24 % of the injected CO2 can be trapped in the solid (mineral) phase, 16.05, 11.86, 8.82 and 6.99 % in the aqueous phase, and 14.87, 11.21, 7.66 and 5.77 % in the gas phase for Case 1 through 4, respectively.

Keywords

CO2 storage Mineralogical compositions Numerical simulation Saline aquifers Trapping mechanisms 

Notes

Acknowledgments

This work was supported by the China Geological Survey working project (Grant No. 12120113006300) and the China Postdoctoral Science Foundation project (Grant No. 2015M571369). The paper also benefited from Jilin University’s Groundwater Resources and Environments Key Laboratory of Ministry of Education (China).

References

  1. 1.
    Andersen G, Probst A, Murray L, Butler S (1992) An accurate PVT model for geothermal fluids as represented by H2O-NaCl-CO2 mixtures. In: Proceedings 17th workshop on geothermal reservoir engineering, Stanford, California, USA, pp 239–248Google Scholar
  2. 2.
    Bachu S, Shaw J (2003) Evaluation of the CO2 sequestration capacity in Albertas oil and gas reservoirs at depletion and the effect of underlying aquifers. Pet Technol 42(9):51–61Google Scholar
  3. 3.
    Baker JC, Bai GP, Hamilton PJ, Golding SD, Keene JB (1995) Continental-scale magmatic carbon dioxide seepage recorded by dawsonite in the Bowen-Gunnedah-Sydney Basin system, eastern Australia. J Sediment Res A 65(3):522–530Google Scholar
  4. 4.
    Berger A, Gier S, Krois P (2009) Porosity-preserving chlorite cements in shallow-marine volcaniclastic sandstones: evidence from Cretaceous sandstones of the Sawan gas field, Pakistan. AAPG Bull 93(5):595–615CrossRefGoogle Scholar
  5. 5.
    Bertier P, Swennen R (2006) Experimental identification of CO2-water-rock interactions caused by sequestration of CO2 in Westphalian and Buntsandstein sandstones of the Campine Basin (NE-Belgium). J Geochem Explor 89(1):10–14CrossRefGoogle Scholar
  6. 6.
    Corey AT (1954) The interrelation between gas and oil relative permeabilities. Producers Mon 19(1):38–41Google Scholar
  7. 7.
    Coveney RM, Kelly WC (1971) Dawsonite as a daughter mineral in hydrothermal fluid inclusions. Contrib Miner Petrol 32(4):334–342CrossRefGoogle Scholar
  8. 8.
    Dalkhaa C, Shevalier M, Nightingale M, Mayer B (2013) 2-D reactive transport modeling of the fate of CO2 injected into a saline aquifer in the Wabamun Lake Area, Alberta, Canada. Appl Geochem 38:10–23CrossRefGoogle Scholar
  9. 9.
    Dixon SA, Summers DM, Surdam RC (1989) Diagenesis and preservation of porosity in Norphlet Formation (Upper Jurassic), southern Alabama. AAPG Bull 73(6):707–728Google Scholar
  10. 10.
    Du YH (1982) Secondary dawsonite in ShengLi oil field, China. Sci Geol Sin 4:434–438 (in Chinese with English abstract) Google Scholar
  11. 11.
    Ehrenberg SN (1993) Preservation of anomalously high porosity in deep buried sandstones by grain-coating: example from the Norwegian Continental Shelf. AAPG Bull 77:1260–1286Google Scholar
  12. 12.
    Ennis-King J, Paterson L (2007) Coupling of geochemical reactions and convective mixing in the long-term geological storage of carbon dioxide. Int J Greenhouse Gas Control 1:86–93CrossRefGoogle Scholar
  13. 13.
    Farajzadeh R, Hamidreza Salimi H, Zitha PL, Bruining H (2007) Numerical simulation of density-driven natural convection in porous media with application for CO2 injection projects. Int J Heat Mass Transf 50(25–26):5054–5064zbMATHCrossRefGoogle Scholar
  14. 14.
    Gao YQ, Liu L, Qu XY (2005) Gemesis of dawsonite and its indication significance of CO2 migration and accumulation. Adv Earth Sci 20(10):1083–1088 (in Chinese with English abstract) Google Scholar
  15. 15.
    Gunter WD, Bachu S, Benson S (2004) The role of hydrogeological and geochemical trapping in sedimentary basins for secure geological storage of carbon dioxide, in geological storage of carbon dioxide. Geol Soc Lond Spec Publ 233(1):129–145CrossRefGoogle Scholar
  16. 16.
    Gunter WD, Perkins EH, Mccann TJ (1993) Aquifer disposal of CO2-rich gases: reaction design for added capacity. Energy Convers Manag 34(9–11):941–948CrossRefGoogle Scholar
  17. 17.
    Haas Jr JL (1976) Thermodynamics properties of the coexisting phases and thermochemical properties of the H2O component in boiling NaCl solutions, USGS Bulletin, 1421-A, Washington, DC, 73 ppGoogle Scholar
  18. 18.
    Hay RL (1963) Zeolite weathering in Olduvai Gorge, Tanganyika. Bull Geol Soc Am 74(10):1281–1286CrossRefGoogle Scholar
  19. 19.
    Heald MT, Larese RE (1974) Influence of coatings on quartz cementation. J Sediment Petrol 44(4):1269–1274Google Scholar
  20. 20.
    Heritsch H (1975) Dawsonite as a product of low-hydrothermal transformation of a volcanic breccia froma borehole in eastern Styria (Austria). Neus Jahrbuch fur Mineralogie, Monatshefte 8:360–368Google Scholar
  21. 21.
    Holloway S (2005) Underground sequestration of carbon dioxide-a viable greenhouse gas mitigation option. Energy Convers Manag 30(11–12):231–333Google Scholar
  22. 22.
    Hou Z, Xie H, Were P (2014) The special issue “Underground storage of CO2 and energy” in the framework of the 3rd Sino-German conference in May 2013. Acta Geotech 9(1):1–5CrossRefGoogle Scholar
  23. 23.
    Huang SJ, Xie LW, Zhang M, Wu WH, Shen LC, Liu J (2004) Formation mechanism of authigenic chlorite and relation to preservation of porosity in nonmarine Triassic reservoir sandstones, Ordos Basin and Sichuan Basin, China. J Chengdu Univ Technol 3:273–281 (in Chinese with English abstract) Google Scholar
  24. 24.
    IEA GHG R&D Programme (2005) Capture and storage of CO2. http://www.ieagreen.org.uk/ccs.html
  25. 25.
    IPCC (2005) Carbon dioxide capture and storage. Cambridge University Press, UKGoogle Scholar
  26. 26.
    Kaszuba JP, Janecky DR, Snow MG (2003) Carbon dioxide reaction processes in a model brine aquifer at 200 °C and 200 bars: implications for geologic sequestration of carbon. Appl Geochem 18(7):1065–1080CrossRefGoogle Scholar
  27. 27.
    Kharaka YK, Thordsen JJ, Hovorka SD, Seay Nance H, Cole DR, Phelps TJ, Knauss KG (2009) Potential environmental issues of CO2 storage in deep saline aquifers: geochemical results from the Frio-I Brine Pilot test, Texas, USA. Appl Geochem 24(6):1106–1112CrossRefGoogle Scholar
  28. 28.
    Kihm JH, Kim JM, Wang S (2009) Numerical simulation of impacts of mineralogical compositions on efficiency and safety of geologic storage of carbon dioxide in deep sandstone aquifers. J Geol Soc Korea 45(5):493–516 (in Korean with English abstract) Google Scholar
  29. 29.
    Kihm JH, Kim JM, Wang S, Xu T (2012) Hydrogeochemical numerical simulation of impacts of mineralogical compositions and convective fluid flow on trapping mechanisms and efficiency of carbon dioxide injected into deep saline sandstone aquifers. J Geophys Res Solid Earth (1978–2012):117(B6)Google Scholar
  30. 30.
    Kneafsey TJ, Pruess K (2009) Laboratory flow experiments for visualizing carbon dioxide-induced, density-driven brine convection. Transp Porous Media 82(1):123–139CrossRefGoogle Scholar
  31. 31.
    Kulik DA, Aja SU (1997) Hydrothermal stability of illite: implications of empirical correlations and Gibbs Energy minimization. In: Proceedings on the fifth international symposium on hydrothermal reactions. Gatlinburg, Tennessee, July 20–24, pp. 228–292Google Scholar
  32. 32.
    Lasaga AC (1984) Chemical kinetics of water–rock interactions. J Geophys Res 89(B6):4009–4025CrossRefGoogle Scholar
  33. 33.
    Li D, Bauer S, Benisch K, Graupner B, Beyer C (2014) OpenGeoSys-ChemApp: a coupled simulator for reactive transport in multiphase systems and application to CO2 storage formation in Northern Germany. Acta Geotech 9(1):67–79CrossRefGoogle Scholar
  34. 34.
    Liu L, Gao YQ, Qu XY, Meng QA, Gao FH, Ren YG, Zhu DF (2006) Petrology and carbon-oxygen isotope of inorganic CO2 gas reservoir in Wuerxun depression, Hailaer basin. Acta Petrol Sin 22(8):2229–2236 (in Chinese with English abstract) Google Scholar
  35. 35.
    Liu L, Liu N, Zhou B, Zhao S, Meng FQ, Jiang L (2009) Petrological recording of mantle-magmatic CO2 leakage on a large-scale in Honggang anticline, Southern Songliao Basin. J Jilin Univ (Earth Sci Ed) 39(1):411–420 (in Chinese with English abstract) Google Scholar
  36. 36.
    Liu LH, Suto Y, Bignall G, Yamasaki N, Hashida T (2003) CO2 injection to granite and sandstone in experiment rock/hot water systems. Energy Convers Manag 44(9):1399–1410CrossRefGoogle Scholar
  37. 37.
    Liu L, Zhu DF, Qu XY, Jin ZL, Wang XQ, Dong LS (2009) Impacts of mantle-genetic CO2 influx on the reservoir quality of Lower Cretaceous sandstone from Wuerxun depression, Hailaer basin. Acta Petrol Sin 25(10):2311–2319 (in Chinese with English abstract) Google Scholar
  38. 38.
    Loughnan FC, Goldbery R (1972) Dawsonite and analcite in the singleton coal measures of the sydney basin. Am Mineral 57(9–10):1437–1447Google Scholar
  39. 39.
    Lu C, Lichtner PC (2007) High resolution numerical investigation on the effect of convective instability on long term CO2 storage in saline aquifers. J Phys: Conf Ser 78(1):012042Google Scholar
  40. 40.
    MacMinn CW, Szulczewski ML, Juanes R (2011) CO2 migration in saline aquifers: regimes in migration with dissolution. Energy Proc 4:3904–3910zbMATHCrossRefGoogle Scholar
  41. 41.
    Marini L (2006) Geological sequestration of carbon dioxide: thermodynamics, kinetics and reaction path modeling. Developments in Geochemistry, vol 11. Elsevier, New York, p 453Google Scholar
  42. 42.
    Monnin C (1994) Density calculation and concentration scale conversion for natural waters. Comput Geosci 20(10):1435–1445CrossRefGoogle Scholar
  43. 43.
    Moore J, Adams M, Allis R, Lutz S, Rauzi S (2005) Mineralogical and geochemical consequences of the long-term presence of CO2 in natural reservoirs: an example from the Springerville-St. Johns Field, Arizona, and New Mexico, USA. Chem Geol 217(3):365–385CrossRefGoogle Scholar
  44. 44.
    Neufeld JA, Hesse MA, Riaz A, Hallworth MA, Tchelepi HA, Huppert HE (2010) Convective dissolution of carbon dioxide in saline aquifers. Geophys Res Lett 37(22):L22404CrossRefGoogle Scholar
  45. 45.
    Pang ZH, Li YM (2012) Geochemistry of a continental saline aquifer for CO2 sequestration: the Guantao formation in the Bohai Bay Basin, North China. Appl Geochem 27:1821–1828CrossRefGoogle Scholar
  46. 46.
    Pau GS, Bell JB, Pruess K, Almgren AS, Lijewski MJ, Zhang K (2010) High resolution simulation and characterization of density driven flow in CO2 storage in saline aquifers. Adv Water Resour 33(4):443–455CrossRefGoogle Scholar
  47. 47.
    Pittman ED, Larese RE, Heald MT (1992) Clay coats: occurrence and relevance to preservation of porosity in sandstones. SEPM Special Publication 47:241–264Google Scholar
  48. 48.
    Pittman ED, Lumsden DN (1968) Relationship between chlorite coatings on quartz grains and porsity, Spiro Sand, Oklahoma. J Sediment Petrol 38(2):668–670CrossRefGoogle Scholar
  49. 49.
    Pruess K, Spycher N (2007) ECO2 N-A fluid property module for the TOUGH2 code for studies of CO2 storage in saline aquifers. Energy Convers Manag 48(6):1761–1767CrossRefGoogle Scholar
  50. 50.
    Pruess K, Nordbotten J (2011) Numerical simulation studies of the long-term evolution of a CO2 plume in a saline aquifer with a sloping caprock. Transp Porous Media 90(1):135–151CrossRefGoogle Scholar
  51. 51.
    Pruess K, Zhang K (2008) Numerical modeling studies of the dissolution-diffusion-convection process during CO2 storage in saline aquifers. Lawrence Berkeley National Laboratory. Paper LBNL-1243E, 2008Google Scholar
  52. 52.
    Robert HG, Carlos R (2002) Recrystallization in quartz overgrowths. J Sediment Res 72(3):432–440CrossRefGoogle Scholar
  53. 53.
    Rosenbauer RJ, Koksalan T, Palandri JL (2005) Experimental investigation of CO2-brine-rock interactions at elevated temperature and pressure: implications for CO2 sequestration in deep-saline aquifers. Fuel Process Technol 86(14):1581–1597CrossRefGoogle Scholar
  54. 54.
    Smith MM, Wolery TJ, Carroll SA (2013) Kinetics of chlorite dissolution at elevated temperatures and CO2 conditions. Chemical Geology 347:1–8CrossRefGoogle Scholar
  55. 55.
    Spycher N, Pruess K (2005) CO2-H2O mixtures in the geological sequestration of CO2, II. Partitioning in chloride brines at 12–100 °C and up to 600 bar. Geochim Cosmochim Acta 69(13):3309–3320CrossRefGoogle Scholar
  56. 56.
    Steefel CI, Lasaga AC (1994) A coupled model for transport of multiple chemical species and kinetic precipitation/dissolution reactions with applications to reactive flow in single phase hydrothermal system. Am J Sci 294(5):529–592CrossRefGoogle Scholar
  57. 57.
    Stevenson JS, Stevenson LS (1965) The petrology of dawsonite at the type locality, Montreal. Can Mineral 8(2):249–252Google Scholar
  58. 58.
    Stevenson JS, Stevenson LS (1978) Contrasting dawsonite occurrences from Mount St-Bruno, Quebec. Can Mineral 16:471–474Google Scholar
  59. 59.
    Tian H, Xu T, Wang F, Patil VV, Sun Y, Yue G (2014) A numerical study of mineral alteration and self-sealing efficiency of a caprock for CO2 geological storage. Acta Geotech 9(1):87–100CrossRefGoogle Scholar
  60. 60.
    Tian HL, Feng P, Xu TF, McPherson BJ, Yue GF, Prashanth M (2014) Impacts of hydrological heterogeneities on caprock mineral alteration and containment of CO2 in geological storage sites. Int J Greenhouse Gas Control 24:30–42CrossRefGoogle Scholar
  61. 61.
    Van Genuchten MT (1980) A closed-form equation for predicting the hydraulic conductivity of unsaturated soils. Soil Sci Soc Am J 44(5):892–898CrossRefGoogle Scholar
  62. 62.
    Weir GJ, White SP, Kissling WM (1996) Reservoir storage and containment of greenhouse gases. Transp Porous Media 23(1):37–60Google Scholar
  63. 63.
    White SP, Weir GJ, Kissling WM (2001) Numerical simulation of CO2 sequestration in natural CO2 reservoirs on the Colorado Plateau. In: Proceedings of first national conference on carbon sequestration, Washington, DCGoogle Scholar
  64. 64.
    Wilkinson M, Haszelding RS, Fallick AE, Odling N, Stoker SJ, Gatliff RW (2009) CO2-mineral reaction in a natural analogue for CO2 storage-implications for modeling. J Sediment Res 79(7):486–494CrossRefGoogle Scholar
  65. 65.
    Winter EM, Bergman PD (1993) Availability of depleted oil and gas reservoirs for disposal of carbon dioxide in the United States. Energy Convers Manag 34(6):1177–1187CrossRefGoogle Scholar
  66. 66.
    Wolery TJ (1992) EQ3/6: software package for geochemical modeling of aqueous systems: Package overview and installation guide (version 7.0). Lawrence Livermore National Laboratory Report UCRL-MA-110662 PT I, Livermore, CaliforniaGoogle Scholar
  67. 67.
    Worden RH (2006) Dawsonite cement in the Triassic Lam Formation, Shabwa Basin, Yemen: a natural analogue for a potential mineral product of subsurface CO2 storage for greenhouse gas reduction. Mar Pet Geol 23(1):61–77CrossRefGoogle Scholar
  68. 68.
    Xie H, Li X, Fang Z, Wang Y, Li Q, Shi L, Bai B, Wei N, Hou Z (2014) Carbon geological utilization and storage in China: current status and perspectives. Acta Geotech 9(1):7–27CrossRefGoogle Scholar
  69. 69.
    Xu T, Apps JA, Pruess K (2003) Reactive geochemical transport simulation to study mineral trapping for CO2 disposal in deep arenaceous formations. J Geophys Res Solid Earth 108(B2):2071CrossRefGoogle Scholar
  70. 70.
    Xu T, Apps JA, Pruess K (2004) Numerical simulation of CO2 disposal by mineral trapping in deep aquifers. Appl Geochem 19(6):917–936CrossRefGoogle Scholar
  71. 71.
    Xu T, Apps JA, Pruess K (2005) Mineral sequestration of carbon dioxide in a sandstone-shale system. Chem Geol 217(3):295–318CrossRefGoogle Scholar
  72. 72.
    Xu T, Apps JA, Pruess K, Yamamoto H (2007) Numerical modeling of injection and mineral trapping of CO2 with H2S and SO2 in a sandstone formation. Chem Geol 242(3–4):319–346CrossRefGoogle Scholar
  73. 73.
    Xu T, Kharaka YK, Doughty C, Freifeld BM, Daley TM (2010) Reactive transport modeling to study changes in water chemistry induced by CO2 injection at the Frio-I Brine Pilot. Chem Geol 271(3):153–164CrossRefGoogle Scholar
  74. 74.
    Xu T, Pruess K (2001) On fluid flow and mineral alteration in fractured caprock of magmatic hydrothermal systems. J Geophys Res 106(B2):2121–2138CrossRefGoogle Scholar
  75. 75.
    Xu T, Sonnenthal E, Spycher N, Pruess K (2006) TOUGHREACT-a simulation program for non-isothermal multiphase reactive geochemical transport in variably saturated geologic media: applications to geothermal injectivity and CO2 geological sequestration. Comput Geosci 32(2):145–165CrossRefGoogle Scholar
  76. 76.
    Xu T, Spycher N, Sonnenthal E, Zheng LG, Pruess K (2012) TOUGHREACT user’s guide: A simulation program for non-isothermal multiphase reactive geochemical transport in variable saturated geologic media, V1.2.1. Lawrence Berkeley National LaboratoryGoogle Scholar
  77. 77.
    Yang C, Gu Y (2006) Accelerated mass transfer of CO2 in reservoir brine due to density-driven natural convection at high pressures and elevated temperatures. Ind Eng Chem Res 45(8):2430–2436CrossRefGoogle Scholar
  78. 78.
    Zhang G, Spycher N, Sonnenthal E, Steefel C, Xu T (2008) Implementation of a Pitzer Activity Model into TOUGHREACT for modeling concentrated solutions. Nucl Technol 164:180–195Google Scholar
  79. 79.
    Zhang W, Li Y, Xu T, Cheng H, Zheng Y, Xiong P (2009) Long-term variations of CO2 trapped in different mechanisms in deep saline formations: a case study of the Songliao Basin, China. Int J Greenhouse Gas Control 3(2):161–180CrossRefGoogle Scholar
  80. 80.
    Zhao C (2009) Dynamic and transient infinite elements: theory and geophysical, geotechnical and geoenvironmental applications. Springer, HeidelbergGoogle Scholar
  81. 81.
    Zhao C (2010) Computational simulation of wave propagation problems in infinite domains. Sci China, Ser G 53(8):1397–1407CrossRefGoogle Scholar
  82. 82.
    Zhao C (2010) Coupled method of finite and dynamic infinite elements for simulating wave propagation in elastic solids involving infinite domains. Sci China Ser E: Technol Sci 53(6):1678–1687zbMATHCrossRefGoogle Scholar
  83. 83.
    Zhao C (2014) Physical and chemical dissolution front instability in porous media: theoretical analyses and computational simulations. Springer, HeidelbergCrossRefGoogle Scholar
  84. 84.
    Zhao C (2015) Advances in numerical algorithms and methods in computational geosciences with modeling characteristics of multiple physical and chemical processes. Sci China Ser E: Technol Sci 58(5):783–795CrossRefGoogle Scholar
  85. 85.
    Zhao C, Hobbs BE, Hornby P, Ord A, Peng S, Liu L (2008) Theoretical and numerical analyses of chemical-dissolution front instability in fluid-saturated porous rocks. Int J Numer Anal Meth Geomech 32(9):1107–1130zbMATHCrossRefGoogle Scholar
  86. 86.
    Zhao C, Hobbs BE, Mühlhaus HB (1998) Finite element modelling of temperature gradient driven rock alteration and mineralization in porous rock masses. Comput Methods Appl Mech Eng 165(1):175–187zbMATHCrossRefGoogle Scholar
  87. 87.
    Zhao C, Hobbs BE, Ord A (2008) Convective and advective heat transfer in geological systems. Springer, Berlin, HeidelbergGoogle Scholar
  88. 88.
    Zhao C, Hobbs BE, Ord A (2008) Investigating dynamic mechanisms of geological phenomena using methodology of computational geosciences: an example of equal-distant mineralization in a fault. Sci China, Ser D Earth Sci 51(7):947–954CrossRefGoogle Scholar
  89. 89.
    Zhao C, Hobbs BE, Ord A (2009) Fundamentals of computational geoscience: numerical methods and algorithms. Springer, Berlin, HeidelbergGoogle Scholar
  90. 90.
    Zhao C, Hobbs BE, Ord A (2010) Theoretical analyses of nonaqueous-phase-liquid dissolution induced instability in two-dimensional fluid-saturated porous media. Int J Numer Anal Meth Geomech 34(17):1767–1796zbMATHCrossRefGoogle Scholar
  91. 91.
    Zhao C, Hobbs BE, Ord A (2010) Theoretical and numerical investigation into roles of geofluid flow in ore forming systems: integrated mass conservation and generic model approach. J Geochem Explor 106(1):251–260CrossRefGoogle Scholar
  92. 92.
    Zhao C, Hobbs BE, Ord A (2010) Theoretical analyses of the effects of solute dispersion on chemical-dissolution front instability in fluid-saturated porous rocks. Transp Porous Media 84(3):629–653MathSciNetCrossRefGoogle Scholar
  93. 93.
    Zhao C, Hobbs BE, Ord A (2012) Effects of domain shapes on the morphological evolution of nonaqueous-phase-liquid dissolution fronts in fluid-saturated porous media. J Contam Hydrol 138:123–140CrossRefGoogle Scholar
  94. 94.
    Zhao C, Hobbs BE, Ord A (2012) Effects of medium and pore-fluid compressibility on chemical-dissolution front instability in fluid-saturated porous media. Int J Numer Anal Meth Geomech 36(8):1077–1100CrossRefGoogle Scholar
  95. 95.
    Zhao C, Hobbs BE, Ord A (2013) Analytical solutions of nonaqueous-phase-liquid dissolution problems associated with radial flow in fluid-saturated porous media. J Hydrol 494:96–106CrossRefGoogle Scholar
  96. 96.
    Zhao C, Hobbs BE, Ord A (2013) Effects of medium permeability anisotropy on chemical-dissolution front instability in fluid-saturated porous rocks. Transp Porous Media 99(1):119–143MathSciNetCrossRefGoogle Scholar
  97. 97.
    Zhao C, Hobbs BE, Ord A (2015) Theoretical analyses of chemical dissolution-front instability in fluid-saturated porous media under non-isothermal conditions. Int J Numer Anal Meth Geomech 39(8):799–820CrossRefGoogle Scholar
  98. 98.
    Zhao C, Hobbs BE, Ord A (2015) Computational simulation of chemical dissolution-front instability in fluid-saturated porous media under non-isothermal conditions. Int J Numer Meth Eng 102(2):135–156MathSciNetCrossRefGoogle Scholar
  99. 99.
    Zhao C, Hobbs BE, Ord A, Hornby P, Peng S (2008) Morphological evolution of three-dimensional chemical dissolution front in fluid-saturated porous media: a numerical simulation approach. Geofluids 8(2):113–127CrossRefGoogle Scholar
  100. 100.
    Zhao C, Hobbs BE, Ord A, Hornby P, Peng S (2008) Effect of reactive surface areas associated with different particle shapes on chemical-dissolution front instability in fluid-saturated porous rocks. Transp Porous Media 73(1):75–94MathSciNetCrossRefGoogle Scholar
  101. 101.
    Zhao C, Hobbs BE, Ord A, Hornby P, Peng S, Liu L (2006) Theoretical and numerical analyses of pore-fluid flow patterns around and within inclined large cracks and faults. Geophys J Int 166(2):970–988CrossRefGoogle Scholar
  102. 102.
    Zhao C, Hobbs BE, Ord A, Hornby P, Peng S, Liu L (2007) Mineral precipitation associated with vertical fault zones: the interaction of solute advection, diffusion and chemical kinetics. Geofluids 7(1):3–18CrossRefGoogle Scholar
  103. 103.
    Zhao C, Hobbs BE, Ord A, Kuhn M, Mühlhaus HB, Peng S (2006) Numerical simulation of double-diffusion driven convective flow and rock alteration in three-dimensional fluid-saturated geological fault zones. Comput Methods Appl Mech Eng 195(19):2816–2840zbMATHCrossRefGoogle Scholar
  104. 104.
    Zhao C, Hobbs BE, Ord A, Peng S, Liu L (2008) Inversely-mapped analytical solutions for flow patterns around and within inclined elliptic inclusions in fluid-saturated rocks. Math Geosci 40(2):179–197zbMATHCrossRefGoogle Scholar
  105. 105.
    Zhao C, Hobbs BE, Ord A, Peng S (2008) Particle simulation of spontaneous crack generation associated with the laccolithic type of magma intrusion processes. Int J Numer Meth Eng 75(10):1172–1193zbMATHCrossRefGoogle Scholar
  106. 106.
    Zhao C, Hobbs BE, Ord A, Peng S (2010) Effects of mineral dissolution ratios on chemical-dissolution front instability in fluid-saturated porous media. Transp Porous Media 82(2):317–335CrossRefGoogle Scholar
  107. 107.
    Zhao C, Hobbs BE, Ord A, Peng S, Mühlhaus HB, Liu L (2004) Theoretical investigation of convective instability in inclined and fluid-saturated three-dimensional fault zones. Tectonophysics 387(1):47–64CrossRefGoogle Scholar
  108. 108.
    Zhao C, Hobbs BE, Regenauer-Lieb K, Ord A (2011) Computational simulation for the morphological evolution of nonaqueous-phase-liquid dissolution fronts in two-dimensional fluid-saturated porous media. Comput Geosci 15(1):167–183zbMATHCrossRefGoogle Scholar
  109. 109.
    Zhao C, Mühlhaus HB, Hobbs BE (1997) Finite element analysis of steady-state natural convection problems in fluid-saturated porous media heated from below. Int J Numer Anal Meth Geomech 21(12):863–881CrossRefGoogle Scholar
  110. 110.
    Zhao C, Poulet T, Regenauer-Lieb K, Hobbs BE (2013) Computational modeling of moving interfaces between fluid and porous medium domains. Comput Geosci 17(1):151–166MathSciNetCrossRefGoogle Scholar
  111. 111.
    Zhao C, Reid LB, Regenauer-Lieb K (2012) Some fundamental issues in computational hydrodynamics of mineralization. J Geochem Explor 112:21–34CrossRefGoogle Scholar
  112. 112.
    Zhao C, Reid LB, Regenauer-Lieb K, Poulet T (2012) A porosity-gradient replacement approach for computational simulation of chemical-dissolution front propagation in fluid-saturated porous media including pore-fluid compressibility. Comput Geosci 16(3):735–755CrossRefGoogle Scholar
  113. 113.
    Zhao C, Valliappan S (1993) A dynamic infinite element for three-dimensional infinite-domain wave problems. Int J Numer Meth Eng 36(15):2567–2580zbMATHCrossRefGoogle Scholar
  114. 114.
    Zhao C, Valliappan S (1993) Transient infinite elements for seepage problems in infinite media. Int J Numer Anal Meth Geomech 17(5):324–341zbMATHCrossRefGoogle Scholar
  115. 115.
    Zhao C, Valliappan S (1993) Mapped transient infinite elements for heat transfer problems in infinite media. Comput Methods Appl Mech Eng 108(1):119–131zbMATHCrossRefGoogle Scholar
  116. 116.
    Zhao C, Valliappan S (1994) Transient infinite elements for contaminant transport problems. Int J Numer Meth Eng 37(7):1143–1158zbMATHCrossRefGoogle Scholar
  117. 117.
    Zwingmann N, Mito S, Sorai M, Ohsumi T (2005) Preinjection characterization and evaluation of CO2 sequestration potential in the Haizume Formation, Niigata Basin, Japan. Oil Gas Sci Technol 60(2):249–258CrossRefGoogle Scholar

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Authors and Affiliations

  • Kairan Wang
    • 1
  • Tianfu Xu
    • 1
  • Hailong Tian
    • 1
    Email author
  • Fugang Wang
    • 1
  1. 1.Key Laboratory of Groundwater Resources and Environment, Ministry of EducationJilin UniversityChangchunChina

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