Dissolution and deformation in fractured carbonates caused by flow of CO2-rich brine under reservoir conditions

Adler, 1999, vol. v.15 Alkattan, 1998, An experimental study of calcite and limestone dissolution rates as a function of pH from −1 to 3 and temperature from 25 to 80°C, Chemical Geology, 150, 199, 10.1016/S0009-2541(98)00080-1 Békri, 1997, Dissolution and deposition in fractures. Eng, Geology, 48, 283 Boadu, 2000, Predicting the transport properties of fractured rocks from seismic information: numerical experiments, Journal of Applied Geophysics, 44, 103, 10.1016/S0926-9851(99)00020-8 Boadu, 1996, Effects of fractures on seismic-wave velocity and attenuation, Geophysical Journal International, 127, 86, 10.1111/j.1365-246X.1996.tb01537.x Brosse, 2005, Modelling fluid–rock interaction induced by the percolation of CO2-enriched solutions in core samples: the role of reactive surface area, Oil & Gas Science and Technology – Revue d’IFP Energies nouvelles, 60, 287, 10.2516/ogst:2005018 Brush, 2003, Fluid flow in synthetic rough-walled fractures: Navier–Stokes, Stokes, and local cubic law simulations, Water Resources Research, 39, 1085, 10.1029/2002WR001346 Daccord, 1993, Chemical dissolution of a porous-medium by a reactive fluid: 1. Model for the Wormholing phenomenon, Chemical Engineering Science, 48, 169, 10.1016/0009-2509(93)80293-Y Detwiler, 2008, Experimental observations of deformation caused by mineral dissolution in variable-aperture fractures, Journal of Geophysical Research, 113, B08202, 10.1029/2008JB005697 Detwiler, 2002, Comparison of an algebraic multigrid algorithm to two iterative solvers used for modeling ground water flow and transport, Ground Water, 40, 267, 10.1111/j.1745-6584.2002.tb02654.x Detwiler, 2007, Predicting dissolution patterns in variable aperture fractures: evaluation of an enhanced depth-averaged computational model, Water Resources Research, 43, W04403, 10.1029/2006WR005147 Dijk, 2002, Measurements and analysis of dissolution patterns in rock fractures, Water Resources Research, 38, 1013, 10.1029/2001WR000246 Durham, 2001, Direct observation of reactive flow in a single fracture, Water Resources Research, 37, 1, 10.1029/2000WR900228 Espinoza, 2011, CO2 geological storage – geotechnical implications, KSCE Journal of Civil Engineering, 15, 707, 10.1007/s12205-011-0011-9 Golfier, 2002, On the ability of a Darcy-scale model to capture wormhole formation during the dissolution of a porous medium, Journal of Fluid Mechanics, 457, 213, 10.1017/S0022112002007735 Hoefner, 1988, Pore evolution and channel formation during flow and reaction in porous-media, AIChE Journal, 34, 45, 10.1002/aic.690340107 Izgec, 2010, Numerical and experimental investigation of acid Wormholing during acidization of vuggy carbonate rocks, Journal of Petroleum Science and Engineering, 74, 51, 10.1016/j.petrol.2010.08.006 Kalia, 2009, Effect of medium heterogeneities on reactive dissolution of carbonates, Chemical Engineering Science, 64, 376, 10.1016/j.ces.2008.10.026 Kays, 1966 Liu, 2006, A fully-coupled hydrological–mechanical–chemical model for fracture sealing and preferential opening, International Journal of Rock Mechanics and Mining Sciences, 43, 23, 10.1016/j.ijrmms.2005.04.012 Moore, 1994, Reduction of permeability in granite at elevated-temperatures, Science, 265, 1558, 10.1126/science.265.5178.1558 Nicholl, 1999, Saturated flow in a single fracture: evaluation of the Reynolds equation in measured aperture fields, Water Resources Research, 35, 3361, 10.1029/1999WR900241 Noiriel, 2005, Hydraulic properties and microgeometry evolution accompanying limestone dissolution by acidic water, Oil & Gas Science and Technology – Revue d’IFP Energies nouvelles, 60, 177, 10.2516/ogst:2005011 Parkhurst, D.L., Appelo, C.A.J., 1999. User's guide to PHREEQC (version 2) – a computer program for speciation, reaction-path, 1D-transport, and inverse geochemical calculations. Tech. Rep. Inv. Rep. 99-4259, US Geol. Surv. Water Resour. Pokrovsky, 2009, Calcite, dolomite and magnesite dissolution kinetics in aqueous solutions at acid to circumneutral pH, 25 to 150°C and 1 to 55atm pCO2: new constraints on CO2 sequestration in sedimentary basins, Chemical Geology, 265, 20, 10.1016/j.chemgeo.2009.01.013 Polak, 2004, Spontaneous switching of permeability changes in a limestone fracture with net dissolution, Water Resources Research, 40, W03502, 10.1029/2003WR002717 Pyrak-Nolte, 2000, Single fractures under normal stress: the relation between fracture specific stiffness and fluid flow, International Journal of Rock Mechanics and Mining Sciences, 37, 245, 10.1016/S1365-1609(99)00104-5 Riding, J.B., Rochelle, C.A., 2005. The IEA Weyburn CO2 monitoring and storage project: final report of the European research team. British Geological Survey. Shukla, 2010, A review of studies on CO2 sequestration and caprock integrity, Fuel, 89, 2651, 10.1016/j.fuel.2010.05.012 Sjoberg, 1976, Fundamental equation for calcite dissolution kinetics, Geochimica et Cosmochimica Acta, 40, 441, 10.1016/0016-7037(76)90009-0 Sjoberg, 1984, Temperature-dependence of calcite dissolution kinetics between 1°C and 62°C at pH 2.7 to 8.4 in aqueous-solutions, Geochimica et Cosmochimica Acta, 48, 485, 10.1016/0016-7037(84)90276-X Szymczak, 2011, The initial stages of cave formation: beyond the one-dimensional paradigm, Earth and Planetary Science Letters, 301, 424, 10.1016/j.epsl.2010.10.026 Taylor, 2006, Anomalous acid reaction rates in carbonate reservoir rocks, SPE Journal, 11, 488, 10.2118/89417-PA Vialle, 2011, Laboratory measurements of elastic properties of carbonate rocks during injection of reactive CO2-saturated water, Geophysical Research Letters, 38, L01302, 10.1029/2010GL045606 Wilson, M., Monea, M. (Eds.), 2004. IEA GHG Weyburn CO2 monitoring and storage project: summary report 2000–2004. Regina, Saskatchewan, Canada. Yasuhara, 2006, A numerical model simulating reactive transport and evolution of fracture permeability, International Journal for Numerical and Analytical Methods in Geomechanics, 30, 1039, 10.1002/nag.513