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Rock/water reaction. The Cape Fear Formation contains substantial volumes of clays and labile minerals that can potentially react with ground water (Gohn and others, 1977). Miller and others (1986) provided an excellent discussion of sediment/water interaction as a function of ground-water residence time in southeastern U.S. coastal plain aquifers. For the GIS we used information from Miller and others (1986) to characterize rock/water reactions that can be expected 67 in the Cape Fear hydrostratigraphic interval. Immature sands may have moderate potential for interaction with high-CO2 fluids. |
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Rock/water reaction. The Cape Fear Formation contains substantial volumes of clays and labile minerals that can potentially react with ground water (Gohn and others, 1977). Miller and others (1986) provided an excellent discussion of sediment/water interaction as a function of ground-water residence time in southeastern U.S. coastal plain aquifers. For the GIS we used information from Miller and others (1986) to characterize rock/water reactions that can be expected 67 in the Cape Fear hydrostratigraphic interval. Immature sands may have moderate potential for interaction with high-CO2 fluids. |
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Havorka, S., Romero, M., Warne, A., Ambrose, W., Tremblay, T., Trevino, R., and Sasson, D. "Sequestration of Greenhouse Gassesin Brine Formations: CO2 Brine Database. Bureau of Economic Geology Gulf Coast Carbon Center. 2012. https://www.beg.utexas.edu/gccc/research/brine-main |
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Brine chemical composition
Publication Date: 2012
Geographic Extent: South Carolina coastal plain |
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Public access |
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| title:
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Cape Fear Rock/ Water Reaction |
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["United States","South Carolina","South Carolina Coastal Plain","CCS","Cape Fear Rock Water Reaction","Cape Fear","Rock Water Reaction","Rock Reaction","Water Reaction","Rock","Water","Reaction","Groundwater","Geochemistry","Polygon"] |
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en-US |
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150000000 |
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