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Geochemical Study on the Mobility of Dissolved Elements by Rocks-$CO_2$-rich waters Interaction in the Kangwon Province  

최현수 (고려대학교 지구환경과학과)
고용권 (한국원자력연구소)
윤성택 (고려대학교 지구환경과학과)
김천수 (한국원자력연구소)
Publication Information
Economic and Environmental Geology / v.35, no.6, 2002 , pp. 533-544 More about this Journal
Abstract
In order to investigate the relative mobility (RM) of dissolved elements during processes controlling major and trace element content, the concentrations of major, minor and trace elements were reviewed from the previous data of $CO_2$-rich waters and granites from Kangwon Province. The relative mobility of elements dissolved in $CO_2$-rich waters is calculated from $CO_2$-rich water/granite ratio with normalizing by sodium. The results show that gaseous input of magmatic volatile metals into the aquifer is negligible in this study area, being limited by cooling of the rising fluids. Granite leaching by weakly acidic, $CO_2$-charged water is the overwhelming source of metals. Poorly mobile element (Al) is preferentially retained in the solid residue of weathering, while alkalis, alkaline earth and oxo-hydroxo anion forming elements (especially As and U) are mobile and released to the aqueous system. Transition metals display an intermediate behavior and are strongly dependent on either the redox conditions (Fe and Mn) or solid surface-related processes (adsorption or precipitation) (V, Zn and Cu).
Keywords
mobility; geochemistry; $_2$-rich water; water-rock interaction;
Citations & Related Records
Times Cited By KSCI : 6  (Citation Analysis)
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