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Influence of Groundwater on the Hydrogeochemistry and the Origin of Oseepchun in Dogye Area, Korea

도계지역 오십천에서의 지하수 영향분석 - 수리지화학적 특성과 기원

Hwang, Jeong Hwan;Song, Min Ho;Cho, Hea Ly;Woo, Nam C
황정환;송민호;조해리;우남칠

  • Received : 2016.04.15
  • Accepted : 2016.06.22
  • Published : 2016.06.28

Abstract

Water quality of Oseepchun, Dogye area, was investigated quantitatively for its origin and hydrogeochemistry in relation to the influence of groundwater. Groundwater appears to be the principal source of Oseepchun from the water-quality monitoring data including redox potentials, composition of dissolved ions and their correlations, hydrogen and oxygen stable isotopic ratios, and the distribution and occurrence of contaminants. Water-quality type of the surface water was grouped by the water-rock interactions as $Ca-HCO_3$ type originated from carbonated bed-rocks in the Joseon Supergroup, (Ca, Mg)-$SO_4$ type related with dissolution of surfide minerals in coal beds of Pyeongan Supergroup, and (Ca, Mg)-($HCO_3$, $SO_4$) type of the mixed one. Locally water pollution occurs by high $SO_4$ from mine drainage and $NO_3$ from waste-treatment facility. Intensive precipitation in summer has no effect on the water type of Oseepchun, but increases the inflow of nitrate and chloride originated from land surface. Results of this study direct that groundwater-surface water interaction is intimate, and thus surface-water resource management should begin with groundwater characterization.

Keywords

Oseepchun;groundwater-surface water interaction;hydrogeochemistry;water-rock interaction;stable isotopes

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  1. Hydrochemical characteristics of groundwater and stream water in a karst area of Samcheok, Korea vol.55, pp.1, 2019, https://doi.org/10.14770/jgsk.2019.55.1.117

Acknowledgement

Supported by : 한국기상산업진흥원