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물 수지 방법과 라돈 물질수지 방법을 이용한 일광유역의 해저용출수 평가

Estimation of Submarine Groundwater Discharge in Il-Gwang Watershed Using Water Budget Analysis and Rn Mass Balance

  • 곽용석 (부산대학교 환경공학과) ;
  • 김상현 (부산대학교 환경공학과) ;
  • 이용우 (부산대학교 해양시스템과학과) ;
  • 함세영 (부산대학교 지질환경과학과) ;
  • 김인수 (부산대학교 지질환경과학과) ;
  • 김부근 (부산대학교 환경공학과)
  • Gwak, Yong-Seok (Department of Environmental Engineering, Pusan National University) ;
  • Kim, Sang-Hyun (Department of Environmental Engineering, Pusan National University) ;
  • Lee, Yong-Woo (Department of Oceanography, Pusan National University) ;
  • Hamm, Se-Yeung (Department of Geological Sciences, Pusan National University) ;
  • Kim, In-Soo (Department of Geological Sciences, Pusan National University) ;
  • Khim, Boo-Keun (Department of Oceanography, Pusan National University)
  • 투고 : 2011.06.30
  • 심사 : 2011.08.11
  • 발행 : 2011.09.30

초록

The evaluation of potential submarine groundwater is an important research topic for exploring an alternative water resource. Two different approaches, water budget analysis and Rn mass balance method, were employed to investigate the annual variation of submarine groundwater discharge in 2010 at a marine watershed located at the south-eastern part of Korean Peninsula. In order to obtain reliable hydrological data during study period, temporal and spatial variations of rainfall and soil moisture had been collected and hydro-meterological data such as temperature, humidity and wind speed were collected The runoff response was simulated using SCS-CN method with spatial distributions of landuse and soil texture from GIS analysis. Six different methods were used to estimate the monthly variation of evapotranspiration and field measurements of soil moisture were used to account for the infiltration. Comparisons of infiltration and surface runoff between simulation and water balance with measurements showed coincidence. The water budget analysis and Rn mass balance method provide mean daily submarine groundwater as 5.35 and 4.07 $m^3/m/day$ in 2010, respectively.

키워드

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