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• W64490747 abstract "This paper describes the organic carbon cycle of the recharge environment of a shallow, sandy aquifer, with an emphasis on the origin, flux and geochemical evolution of dissolved organic carbon using liquid chromatography, carbon isotopes and GC-MS techniques. The two components of DOC investigated are hydrophobic acids and C 1 -C 10 hydrophilic compounds. The 14 C activity of these components of the DOC was measured using TAMS. 14 C analyses of DOC components may provide an additional tool for groundwater dating. The initial 14 C activity of DOC in a recharge zone, however, depends mainly on the residence times and cycling of DOC sources in the recharge environment. Using 14 C DOC to estimate groundwater residence times between sampling points along a flow path compares well with residence times estimated on the basis of hydraulic parameters and 14 C DIC under closed system conditions." @default.
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• W64490747 date "1989-01-01" @default.
• W64490747 modified "2023-09-26" @default.
• W64490747 title "The Geochemistry and Evolution of Natural Organic Solutes in Groundwater" @default.
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• W64490747 doi "https://doi.org/10.1017/s0033822200012480" @default.
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