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Land Use Map of Changwon Stream and Nam Stream Watershed 

Land Use Map of Changwon Stream and Nam Stream Watershed 

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Recently, due to increase of the impervious layer, the storage of surface layer has been reduced. Otherwise the peak runoff and the total surface runoff have been raised. Because of larger amount of the peak runoff and the rapid time of concentration, the flood damage of the urban watershed was increased. The groundwater level is descended by reduc...

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... 15.74% . 유입되며 , 창 원천 하고 있다 (Fig. 11 ). 115.97 km2 , 15.37 km, 유역 1/1150 ~ 1/51 로서 중 ᆞ 급한 유역이다 (Fig. 12 ). , 2011 1 2011 12 . SWMM . , , GIS , , , . Engman (1986) 의 조도계수 추정 값 을 이용하여 불투수 지역에는 0.013, 투수 지역에는 0.4 를 적용하였다 . 지면 저류 깊 이는 Tholin and Keifer (1960) 의 추정 값 을 이용하여 투수지역에는 6.4 mm, 불투수 지역에 는 1.6 mm 를 입력하였다 . SWMM 모형의 침투모형으로는 Horton, Green-Ampt, Curve Number 가 있으며 본 연구에서는 Green-Ampt 를 이용하였다 . Green-Ampt 식 은 Darcy 의 법 칙 을 기초로 하고 있으며 , 간단하면서도 연 직 침투과정의 기본적인 특성 . (Wallace et al., 1975). Fig. 13 은 창 원천과 남 천 유역의 SWMM 모형 구 축 현 황 을 나 타낸 것이다 . 창 원천 유역을 분할하여 7 개의 소유역으로 구 축 하 였으며 , 남 천 유역은 창 원천을 제외하고 10 개의 소유역으로 구 축 하 였다 . 11 개의 하천 자료는 창 원시에서 구한 CAD 자료와 하천기본 계획보고서를 바 탕 으로 구 축 하였다 (MLTM, 1993, 1994a, 1994b, 1994c, 1995, 1996, 2000, 2005, 2010a, 2010b). SWMM 모형의 5.0 버 전에 포 함 되어 있는 LID 모형은 다양한 빗물관리시설의 수문영향분석이 가능하도록 미국 EPA 에서 기 존 SWMM 모형에 빗물정원 , 습 지 , 침투트 렌 치 , 침투정 , 식 생도 랑 , 투수성 포장 등의 LID 시설 모의가 가능하도록 개발된 모형이다 . 침투 . 저류시설 및 LID 계획요소의 정량적인 수문영향평가가 가능 하다 . Fig. 14 는 LID 모형에서 침투 . 저류시설 여부에 따른 유출개 념 도를 나 타낸 것이다 . 본 연구에서는 LID 모형의 투수성 ...

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