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• W757963652 abstract "Groundwater samples were collected from the bedrock aquifers related with Okcheon metasedimentary rocks. Arsenic (As) concentrations in the samples varied between 0.0051 and 0.887 mg/L, with an average of 0.0248. Cations and anions of groundwaters had no relationship with As contents as well as with spatial distribution of geology in the area. Pyrite, chalcopyrite and arsenopyrite in the core samples of the monitoring wells were identified in thin section, X-ray diffraction (XRD) and electron probe microscope analysis (EPMA). It was suggested that these minerals are responsible for the As in groundwater. The groundwater showed saturations with respect to calcite , dolomite (CaMg) and Magnesite . activities in the groundwater samples were close to and solubility isotherms, indicating that the maximum As contents in groundwater are secondly controlled by the precipitation and dissolution of carbonate minerals due to alkaline and oxic nature of the groundwater (pe+pH>10)." @default.
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• W757963652 date "2009-01-01" @default.
• W757963652 modified "2023-09-28" @default.
• W757963652 title "Arsenic Distribution and Solubility in Groundwater of Okcheon Area" @default.
• W757963652 hasPublicationYear "2009" @default.
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