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Formation-water salinity. Several researchers have reported that salinity in the Cape Fear aquifer is moderately high but below 10,000 mg/L (Manheim and Horn, 1968; Brown and others, 1979; Lee, 1985; Miller and others, 1986; Miller, 1990). However, there has not been a systematic study of water chemistry in southeastern South Carolina because of low prospect for use. We used the map of Lee (1985) for the GIS, who referred to the Cape Fear hydrostratigraphic interval as the middle water-bearing zone of the A4 regional aquifer. We chose this map to grid (c12capefear) because it shows the regional distribution of dissolved solids. |
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Formation-water salinity. Several researchers have reported that salinity in the Cape Fear aquifer is moderately high but below 10,000 mg/L (Manheim and Horn, 1968; Brown and others, 1979; Lee, 1985; Miller and others, 1986; Miller, 1990). However, there has not been a systematic study of water chemistry in southeastern South Carolina because of low prospect for use. We used the map of Lee (1985) for the GIS, who referred to the Cape Fear hydrostratigraphic interval as the middle water-bearing zone of the A4 regional aquifer. We chose this map to grid (c12capefear) because it shows the regional distribution of dissolved solids. |
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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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5000 |
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[] |
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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 Salinity |
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["United States","South Carolina","South Carolina Coastal Plain","CCS","Cape Fear Salinity","Cape Fear","Salinity","Polyline"] |
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en-US |
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150000000 |
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