KSCE Journal of Civil and Environmental Engineering Research (대한토목학회논문집)

Korean Society of Civil Engeneers (대한토목학회)
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Estimation of Interception in Cheonmi Watershed, Jeju Island

제주 천미천 유역의 차단량 추정

  • Chung, Il-Moon (Korea Institute of Civil Engineering and Building Technology) ;
  • Lee, Jeongwoo (Korea Institute of Civil Engineering and Building Technology) ;
  • Kim, Nam Won (Korea Institute of Civil Engineering and Building Technology)
  • 정일문 (한국건설기술연구원 수자원.하천연구소) ;
  • 이정우 (한국건설기술연구원 수자원.하천연구소) ;
  • 김남원 (한국건설기술연구원 수자원.하천연구소)
  • Received : 2015.01.23
  • Accepted : 2015.04.06
  • Published : 2015.08.01
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Abstract

For the establishment of effective water resources management platform for Jeju-Island, the characteristics, including surface runoff, evapotranspiration, groundwater recharge and discharge are to be properly quantified. Among these hydrologic components, interception due to vegetation is very important factor but it is hard to be quantified. After Von Hoyningen-Huene (1981) found the relationship between LAI (Leaf Area Index) and interception storage, LAI has been used for key factor to estimate interception and transpiration. In this study the equation suggested by Kozak et al. (2007) is implemented in SWAT-K (Soil and Water Assessment Tool - Korea) model and is tested at the Cheonmicheon watershed in Jeju-Island. The evaporation due to interception was estimated as 85~104mm, 8~11% of whole evaporation. Therefore it is necessary to consider the evaporation due to interception as a controlling factor to water budget of this watershed.

제주도의 효율적 수자원 관리 기반을 구축하기 위해서는 지표수의 유출 특성과 증발산량, 지하수 함양량, 지하수 유출량의 상호관계를 정확하게 제시할 필요가 있다. 이 중 식생에 의한 차단(interception)효과는 증발산량에 직결되는 영향 인자임에도 정량적 분석의 어려움 때문에 유역단위로 정량화된 사례는 드물다. Von Hoyningen-Huene (1981)이 엽면적지수와 차단저류량의 관계를 밝혔고, LAI는 차단, 증산의 핵심요소로 다양한 수문모형에 활용되고 있다. 본 연구에서는 Kozak et al. (2007)이 제시한 엽면적 지수(LAI: Leaf Area Index)에 따른 차단저류량의 관계식을 이용하여 한국형 유역수문모형 SWAT-K (Soil and Water Assessment Tool-Korea)내에 식생에 의한 차단량 산정모듈을 개선하였다. 제주도 천미천 유역을 대상으로 적용한 결과 천미천 유역의 차단증발량은 85~104mm로서 전체 증발산량(993~1062mm)의 약 8~11% 만큼 차지하는 것으로 분석되어 전체 물수지 성분에 영향인자로 고려되어야 할 것이다.

Keywords

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