• Title/Summary/Keyword: Funoff characteristics

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A Comparative Study of Storm Runoff Characteristics far Irrigated Paddy Fields and forest Watershed (관개논과 산림유역의 홍수유출 특성 비교)

  • 임상준;박승우;강문성
    • Magazine of the Korean Society of Agricultural Engineers
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    • v.44 no.3
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    • pp.65-72
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    • 2002
  • Rainfall and runoff data from a forested watershed and irrigated rice paddies at the Bal-an experimental watershed were monitored and analyzed to investigate the variations of runoff characteristics with different land use. The comparisons were conducted fourteen storm events ranging 21.8∼190.2 mm of rainfall. Field data showed that direct runoff from paddies and forested watershed are not significantly different in volume. The peak discharge from forest watershed was less than that from paddies far lighter storms, but became greater fur heavier storms. The peak runoff from the forest watershed was 39 percent greater than from the paddies. The results demonstrate that paddies play an important role to reduce peak discharge from heavy storms as compared to forest.

Estimation of Watershed Parameters and Runoff Computation Using GIS (GIS를 이용한 유역매개변수의 추정 및 유출량 산정)

  • Lee, Im-Keun;Ahn, Kyung-Soo
    • Journal of Korea Water Resources Association
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    • v.40 no.1 s.174
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    • pp.11-24
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    • 2007
  • There exist various difficulties in runoff analysis due to many ungauged basins in Korea and the runoff phenomena is also more and more complicated by the change of geologic characteristics due to the urbanization. So, we use GIS technique which is widely used in hydrologic field and cell runoff concept for the fast and effective runoff simulation. This study uses the observations of 6 stage stations in Wi-Cheon watershed and simulates the watershed parameters by using WMS model. We construct DEM by the grids which are consisted based on the criteria of minimum area according to land use. The cell runoff is estimated by an average weighted method using mean annual streamflow and mean maximum daily streamflow obtained from six stage stations. The runoff ratio at arbitrary site is estimated by conducting the direction analysis of streamflow and by removing sinkhole. We compare the simulated and observed runoffs and know that the simulated runoff shows the valid results. So, we could use the geographical information and cell runoff concept for more fast and effective runoff simulation studies.