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ISSN Imprimir: 1091-028X
ISSN En Línea: 1934-0508
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Journal of Porous Media
DEPENDENCE ON TEMPERATURE AND SALINITY GRADIENTS AND THE INJECTION RATE OF CO2 STORAGE IN SALINE AQUIFERS WITH AN ANGULAR UNCONFORMITY
Fluid and Complex Systems Research Centre, Coventry University, UK
Seyed M. Shariatipour
Fluid and Complex Systems Research Centre, Coventry University, Coventry, UK
An unconformity surface is a type of interface between an aquifer and a caprock. It refers to a buried erosional or
non-depositional surface that separates two strata of different ages, indicating that sediment deposition has not been continuous. A high- or low-permeability layer may exist just above or below the unconformity surface. The high-permeability layer could be the result of the weathering and erosion of the older layer, or the deposition of coarsegrained sediments on top of the unconformity surface. The effect of this interface on CO2 dissolution in brine was
investigated by running a range of 2D models and considering different injection scenarios. By examining different
injection scenarios using two models for comparative analysis (one with and one without a high-permeability layer), the results provide a good hypothesis of the effects of pressure and migration distance on CO2 dissolution. Although the high-permeability layer creates a pathway for the further migration of CO2, the models without a high-permeability layer have tended to predict a higher CO2 dissolution in almost all the injection scenarios. In addition, the sensitivity of CO2 dissolution to aquifer parameters, such as temperature and salinity gradients, was examined. Models with and without temperature and salinity gradients were compared, and the importance of these parameters on the prediction of CO2 storage was determined. Another significant result is that under higher injection scenarios, the models show significant sensitivity to temperature and salinity gradients. However, for lower injection rates the sensitivity of the dissolved CO2 to temperature and salinity gradients is almost negligible.
Bachu, S. and Adams, J.J., Sequestration of CO2 in Geological Media in Response to Climate Change: Capacity of Deep Saline Aquifers to Sequester CO2 in Solution, Energy Convers. Manage., vol. 44, no. 20, pp. 3151-3175,2003.
Bachu, S. and Bennion, D.B., Interfacial Tension between CO2, Freshwater, and Brine in the Range of Pressure from (2 to 27) Mpa, Temperature from (20 to 125) C, and Water Salinity from (0 to 334 000) mg L-1, J. Chem. Eng. Data, vol. 54, no. 3, pp. 765-775, 2008.
Bachu, S., Gunter, W.D., and Perkins, E.H., Aquifer Disposal of CO2: Hydrodynamic and Mineral Trapping, Energy Convers. Manage, vol. 35, no. 4, pp. 269-279, 1994.
Biddle, K.T. and Wielchowsky, C.C., Hydrocarbon Traps, in The Petroleum System-From Source to Trap, L.B. Magoon and W.G. Dow, Eds., Tulsa, OK: American Association of Petroleum Geologists, pp. 219-235, 1994.
Cao, J., Zhang, Y., Hu, W., Yao, S., Wang, X., Zhang, Y., and Tang, Y., The Permian Hybrid Petroleum System in the Northwest Margin of the Junggar Basin, Northwest China, Marine Petrol. Geol., vol. 22, no. 3, pp. 331-349, 2005.
Davison, J., Freund, P., and Smith, A., Putting Carbon Back into the Ground, Cheltenham, UK: EIA Greenhouse Gas R&D Programme, 2001.
Dickey, P.A., Increasing Concentration of Subsurface Brines with Depth, Chem. Geol., vol. 4,nos. 1-2, pp. 361-370, 1969.
Evans, T.R. and Coleman, N.C., North Sea Geothermal Gradients, Nature, vol. 247, no. 5435, pp. 28-30, 1974.
Fengjun, N., Sitian, L., Hua, W., Xinong, X., Keqiang, W., and Meizhu, J., Lateral Migration Pathways of Petroleum in the Zhu III Subbasin, Pearl River Mouth Basin, South China Sea, Marine Petrol. Geol., vol. 18, no. 5, pp. 561-575, 2001.
Gao, X., Liu, L., Jiang, Z., Shang, X., and Liu, G., A Pre-Paleogene Unconformity Surface of the Sikeshu Sag, Junggar Basin: Lithological, Geophysical and Geochemical Implications for the Transportation of Hydrocarbons, Geosci. Frontiers, vol. 4, no. 6, pp. 779-786,2013.
Goater, A.L., Bijeljic, B., and Blunt, M.J., Dipping Open Aquifers-The Effect of Top-Surface Topography and Heterogeneity on CO2 Storage Efficiency, Int. J. Greenhouse Gas Control, vol. 17, pp. 318-331,2013.
Harper, M.L., Approximate Geothermal Gradients in the North Sea Basin, Nature, vol. 230, no. 5291, pp. 235-236,1971.
Holloway, S., Storage Capacity and Containment Issues of Carbon Dioxide Capture and Geological Storage on the UK Continental Shelf, Proc. Inst. Mech. Eng., Part A: J. Power Energy, vol. 223, no. 3, pp. 239-248,2009.
IPCC (Intergovernmental Panel on Climate Change), IPCC Special Report on Carbon Dioxide Capture and Storage, Prepared by Working Group III of the Intergovernmental Panel on Climate Change, Cambridge, UK: Cambridge University Press, 2005.
Johnson, J.W., Nitao, J.J., and Knauss, K.G., Reactive Transport Modelling of CO2 Storage in Saline Aquifers to Elucidate Fundamental Processes, Trapping Mechanisms and Sequestration Partitioning, Geol. Soc. London, Special Pub., vol. 233, no. 1, pp. 107-128, 2004.
Koide, H., Tazaki, Y., Noguchi, Y., Nakayama, S., Iijima, M., Ito, K., and Shindo, Y., Subterranean Containment and Long-Term Storage of Carbon Dioxide in Unused Aquifers and in Depleted Natural Gas Reservoirs, Energy Convers. Manage., vol. 33, nos. 5-8, pp. 619-626,1992.
Mousavi Nezhad, M., Javadi, A.A., and Rezania, M., Modeling of Contaminant Transport in Soils Considering the Effects of Micro- and Macro-Heterogeneity, J. Hydrol., vol. 404, nos. 3-4, pp. 332-338, 2011.
Nilsen, H.M., Syversveen, A.R., Lie, K., and Nordbotten, J.M., Impact of Top-Surface Morphology on CO2 Storage, Int. J. Greenhouse Gas Control, vol. 11, pp. 221-235, 2012.
Nordbotten, J.M., Celia, M.A., and Bachu, S., Injection and Storage of CO2 in Deep Saline Aquifers: Analytical Solution for CO2 Plume Evolution during Injection, Transp. Porous Media, vol. 58, pp. 339-360,2005.
Oldenburg, C.M., Migration Mechanisms andPotential Impacts of CO2 Leakage and Seepage, in Carbon Capture and Sequestration: Integrating Technology, Monitoring, Regulation, E.J. Wilson and D. Gerard, Eds., Ames, IA: Blackwell Publishing, pp. 127-146, 2006.
Peacock, S.M., Thermal and Petrologic Structure of Subduction Zones, in Subduction Top to Bottom, G.E. Bebout, D.W. Scholl, S.H. Kirby, and J.P. Platt, Eds., Washington, DC: American Geophysical Union, pp. 119-133, 1996.
Rogers, J.N., Kelley, J.T., Belknap, D.F., Gontz, A., and Barnhardt, W.A., Shallow-Water Pockmark Formation in Temperate Estuaries: A Consideration of Origins in the Western Gulf of Maine with Special Focus on Belfast Bay, Marine Geol., vol. 225, nos. 1-4, pp. 45-62,2006.
Saemundsson, K., Geothermal Systems in Global Perspective, Short Course on Exploration for Geothermal Resources, Short Course VIII on Exploration for Geothermal Resources, UNU-GTP, GDC and KenGen, Kenya, Oct. 31-Nov. 22, 2013.
Shariatipour, S.M., Pickup, G.E., and Mackay, E.J., The Effect of Aquifer/Caprock Interface on Geological Storage of CO2, Energy Procedia, vol. 63, pp. 5544-5555, 2014.
Shariatipour, S.M., Pickup, G.E., and Mackay, E.J., Investigation of CO2 Storage in a Saline Formation with an Angular Unconformity at the Caprock Interface, Petrol. Geosci., vol. 22, no. 2, pp. 203-210, 2016a.
Shariatipour, S.M., Pickup, G.E., and Mackay, E.J., Simulations of CO2 Storage in Aquifer Models with Top Surface Morphology and Transition Zones, Int. J. Greenhouse Gas Control, vol. 54, pp. 117-128, 2016b.
Smith, M., Campbell, D., Mackay, E., and Polson, D., CO2 Aquifer Storage Site Evaluation and Monitoring, Edinburgh: Heriot Watt University, 2012.
Spycher, N. and Pruess, K., CO2-H2O Mixtures in the Geological Sequestration of CO2. II. Partitioning in Chloride Brines at 12-100C and Up to 600 Bar, Geochimica et Cosmochimica Acta, vol. 69, no. 13, pp. 3309-3320, 2005.
Spycher, N. and Pruess, K., A Model for Thermophysical Properties of CO2-Brine Mixtures at Elevated Temperatures and Pressures, in Proc. of the 36th Workshop on Geothermal Reservoir Engineering, Stanford, California, January 2011.
Spycher, N., Pruess, K., and Ennis-King, J., CO2-H2O Mixtures in the Geological Sequestration of CO2. I. Assessment and Calculation of Mutual Solubilities from 12 to 100 C and Up to 600 Bar, Geochimica et Cosmochimica Acta, vol. 67, no. 16, pp. 3015-3031,2003.
Song, Z., Song, H., Cao, Y., Killough, J., and Leung, J., Numerical Research on CO2 Storage Efficiency in Saline Aquifer with Low-Velocity Non-Darcy Flow, J. Natural Gas Sci. Eng., vol. 23, pp. 338-345, 2015.
Stern, N.H., The Economics of Climate Change: The Stern Review, Cambridge, UK: Cambridge University Press, 2006.
Swierczek, M., Role of Unconformities in Controlling Clastic Reservoir Properties Insights from Adopting a Multidisciplinary Approach, PhD, Heriot-Watt University, 2012.
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