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Numerical Simulation of Groundwater System Change in a Riverside Area due to the Construction of an Artificial Structure

인공구조물에 의한 하천 주변지역 지하수 시스템 변화의 수치 해석

  • Lee, Jeong-Hwan (Technology Development Center, Korea Radioactive Waste Management Corporation) ;
  • Hamm, Se-Yeong (Division of Earth Environmental System, Pusan National University) ;
  • Lee, Chung-Mo (Division of Earth Environmental System, Pusan National University) ;
  • Lee, Jong-Jin (Water Resources Investigation & Planning Dept., Korea Water Resources Corporation) ;
  • Kim, Hyoung-Soo (Department of Energy Resources Engineering, Jungwon University) ;
  • Kim, Gyoo-Bum (K-Water Institute, Korea Water Resources Corporation)
  • 이정환 (한국방사성폐기물관리공단 기술개발센터) ;
  • 함세영 (부산대학교 지구환경시스템학부) ;
  • 이충모 (부산대학교 지구환경시스템학부) ;
  • 이종진 (한국수자원공사 조사기획처) ;
  • 김형수 (중원대학교 에너지자원공학부) ;
  • 김규범 (한국수자원공사 K-water연구원)
  • Received : 2012.07.11
  • Accepted : 2012.09.06
  • Published : 2012.09.28

Abstract

We performed numerical modeling to estimate the groundwater level around a riverside area following the construction of an artificial structure. The groundwater level of the alluvial deposit responded more rapidly to the river water level than to the rainfall event itself, indicating that the groundwater and river water are directly interrelated through the riverbed. Furthermore, transient modeling showed raised groundwater levels at the southern part of Mt. Dok and the eastern part of Mt. Dummit in an area of low plains. The artificial structure caused a rise in groundwater level of up to approximately 6 m.

본 연구는 지하수 수치 모델링을 통하여 인공 구조물 건설에 따른 하천주변 지역의 지하수 환경 변화를 평가하였다. 하성충적층의 지하수위는 강우 사건보다는 하천수위의 계절적인 변동에 민감하게 반응하며, 이것은 지하수가 하상퇴적층을 통해 하천수와 직접적으로 연결되어 있기 때문이다. 한편, 부정류 모델링 결과, 지하수위는 하성충적층 내부 저지대에 위치하는 독산의 남쪽과 동쪽 지역, 덤밑산 동쪽 지역에서 상승되고 있으며, 지하수위 상승폭은 6 m 이내로 평가되었다.

Keywords

References

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