• 제목/요약/키워드: watershed scale

검색결과 306건 처리시간 0.027초

Watershed Scale Flood Simulation in Upper Citarum Watershed, West Java-Indonesia using RRI Model

  • Nastiti, Kania Dewi;Kim, Yeonsu;Jung, Kwansue;An, Hyunuk
    • 한국수자원학회:학술대회논문집
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    • 한국수자원학회 2015년도 학술발표회
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    • pp.179-179
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    • 2015
  • Citarum River is one of the important river in West Java, Indonesia. During the rainy season, flood happens almost every year in Upper Citarum Watershed, hence, it is necessary to establish the countermeasure in order to prevent and mitigate flood damages. Since the lack of hydrological data for the modelling is common problem in this area, it is difficult to prepare the countermeasures. Therefore, we used Rainfall-Runoff-Inundation (RRI) Model developed by Sayama et al. (2010) as the hydrological and inundation modelling for evaluating the inundation case happened in Upper Citarum Watershed, West Java, Indonesia and the satellite based information such as rainfall (GSMaP), landuse and so on instead of the limited hydrological data. In addition, 3 arc-second HydroSHEDS Digital Elevation Model (DEM) is used. To verify the model, the observed data of Nanjung water stage gauging station and the daily observation data are used. Simulated inundation areas are compared with the flood extent figure from Upper Citarum Basin Flood Management Project (UCBFM).

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감수곡선을 이용한 산림소유역 유출특성의 시계열 변화 평가 (Analysis of Secular Changes in the Hydrological Characteristics of a Small Forested Watershed using a Baseflow Recession Curve)

  • 이익수;이헌호
    • 한국산림과학회지
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    • 제103권3호
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    • pp.383-391
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    • 2014
  • 본 연구는 주지하수 감수곡선을 이용하여 산림소유역의 유출특성을 밝히기 위하여 수행하였다. 2003년부터 2011년까지 9년간 관측한 강우-유출량 자료를 이용하여 수문곡선 감수부의 시계열 변화를 분석하였다. 그 결과 산림소유역에서는 직접유출 감수계수가 기저유출의 감수계수 값보다 작았다. 또한 산림소유역에서의 직접유출량은 대유역에 비해 상당히 적은 양을 보였으며, 기저유출량은 차이가 크지 않았다. 시험유역에서 주지하수 감수곡선의 회귀식과 감수계수는 각각 $y=0.7528e^{-0.022x}$($R^2=0.8938$, 범위는 0.3 mm~0.8 mm), K = 0.978로 산출되었다. 주지하수 감수곡선과 연유출량과는 관련성이 큰 것으로 나타났는데, 유출량이 많으면 주지하수 감수곡선의 기울기가 완만해지고, 유출량이 줄어들면 감수곡선의 기울기가 급해지는 것으로 나타났다. 또한 해를 거듭할수록 주지하수 감수곡선의 기 울기가 완만해지는 경향이 나타나, 점차 기저유출량이 증가하는 것으로 판단하였다. 따라서 시험유역에서는 시간의 경과와 함께 산림의 홍수조절기능 및 수원함양기능이 점진적으로 높아지는 것으로 나타났다.

충남 매곡천 최상류에 있어서 홀로세 구릉사면의 삭박과정과 사면물질이동의 이력 (The Process of Hillslope Denudation and History of Mass-Movement at the Uppermost Stream of Maegokcheon During the Holocene)

  • 박지훈;정혜경
    • 한국지형학회지
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    • 제18권2호
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    • pp.25-37
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    • 2011
  • 본 연구의 목적은 충남 매곡천 최상류 차암골 유역(이하 조사유역)에 있어서 홀로세 동안 유역을 둘러싸고 있는 구릉사면의 삭박에 의해 사면에서 기원한 무기물질이 곡저로 이동하는 현상(이하 사면물질이동)의 이력을 구명하는 것이다. 이를 위하여 조사유역의 곡저에 분포하는 충적층을 대상으로 층상해석·탄소연대측정·입도분석을 실시하고 그리고 조사유역의 지형분석도 병행했다. 그 결과는 다음과 같다. 약 9,100yrBP~최근에 걸쳐서 102~103년의 시간 규모(time scale)로 발생한 수 회의 사면물질이동으로 인하여 다량의 무기물질이 조사유역의 곡저에 형성되어 있는 습지기원의 유기물층에 혼입되었거나 또는 유기물층 사이에 협재되어 있는 것으로 확인되었다. 조사유역에서 홀로세 초기 이후 사면의 불안정시기에 발생했던 사면물질이동은 최소 8회(M1기(期)~M8기(期)) 그리고 사면의 안정기에 형성되는 습지환경은 총 4회(W1기(期)~W4기(期))가 존재했던 것으로 밝혀졌다. 본 분석결과는 향후 매곡천 유역의 홀로세 기후변화와 이에 따른 유역을 구성하고 있는 구릉사면의 삭박과정을 복원하는 데 기초자료로 활용될 것이다.

금강유역 내 도랑유역 분포 및 지형적 특성 분석 (Spatial Distribution and Geomorphological Characteristics of Headwater Stream (Dorang) Catchments in Geum River Basin)

  • 김해정;조홍래;구본경
    • 한국물환경학회지
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    • 제30권3호
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    • pp.319-328
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    • 2014
  • Dorang - the Korean term for headwater streams - occupy a large portion of the total stream length in a basin, and contribute significantly towards the quantitative and qualitative characteristics, and the ecosystem, of the main river. The Ministry of Environment of South Korea has supported the investigation of the status of Dorang in the nation's four major basins, since 2007. Without a widely accepted academic or legal definition of Dorang, however, there are limits to understand the distribution of Dorang at the national scale and to systematically compile a Dorang database. This paper, through a review of the stream classification system and Korean legal system delineating streams, defines Dorang as 1st and 2nd order streams according to the Strahler ordering method, in a 1:25,000 geographical scale. Analysis of the Geum River basin, with this definition, reveals that the total length of Dorang is 20,622.4 km (73.6% of total stream length), and the number of Dorang catchments is 23,639 (71.3% of the basin area). Further analysis of the geomorphological characteristics of Dorang catchments shows that the average total stream length is 1.1 km, average catchment length is 1.2 km, average drainage area is $0.4km^2$, and average drainage density is 3.08/km.

금호강 유역의 환경특성이 하천수질에 미치는 영향 (The Impact of Environmental Characteristics in the Geumho River Watershed on Stream Water Quality)

  • 박경훈
    • 한국지리정보학회지
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    • 제6권4호
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    • pp.85-98
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    • 2003
  • 최근 물환경에 관련된 광범위한 문제들을 해결하기 위한 대안으로 유역관리의 관심이 증대되고있는 시점에서, 본 연구는 금호강 유역을 모니터링하기 위한 환경정보의 구축과 소유역 단위의 환경특성이 하천 수질에 미치는 영향을 분석하였다. 소유역 단위의 환경특성을 분석하기 위한 GIS 데이터베이스는 축척 1:25,000의 지형도, 정밀토양도, 토지이용도, 10m 해상도의 DEM, 도로망도, 수계망도, Landsat TM 영상에서 산출된 식생지수(NDVI), 강우량, 그리고 RUSLE 모형에 의한 토양유실량으로 구성되었다. 소유역 단위의 환경특성과 하천 수질간의 상호관련성을 분석한 결과에 따르면, 유역의 도시화 또는 산업화에 관련된 주거 상업지역, 공업지역, 도로지역에 관련된 변수들은 BOD, COD, SS, T-N, T-P의 수질자료와 음(-)의 상관성을 가지는 것으로 분석되었다. 이와는 달리, 자연환경상태와 관련된 산림피복과 식생상태 변수들은 수질자료와 양(+)의 상관성을 가지는 것으로 분석되었다. 그러나, 농업적 토지이용과 농약 및 비료사용량, 토양유실량은 수질자료와 유의한 상관성을 가지지 않는 것으로 나타났다.

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도시의 자연배수능력 평가를 위한 유역 내 환경특성과 침수피해면적의 관계 (Relationship between Inundated Areas and Environmental Characteristics in Watershed for Natural Drainage Capacity Assessment in Urban Area)

  • 정경진;김민정;김옥수
    • 한국방재학회:학술대회논문집
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    • 한국방재학회 2007년도 정기총회 및 학술발표대회
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    • pp.211-214
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    • 2007
  • The purpose of this study was to establish the basic information for natural drainage capacity assessment in urban area. We sorted midium watershed of Han river and Nak-dong river, and selected 30 rainfall events during 1995 to 2000 according to high level of damage. The inundated area showed high watershed slope about 25% and it indicated the greatest damage around the watershed located in 200-300m of altitude. Besides, the great damage by inundation was occurred in the mountainous agriculture region, where the forest scale was high and the urbanization was being progressed gradually. However, inundated area was small in case of grassland, water tone such as riparian area, bare ground and wetland. Moreover, the inundated area was different according to river shape and characteristics of river distribution such as the density of the stream order, conservation constant of the river system, and the number of undulations in the watershed. Therefore, it showed that land use, river shape and distribution characteristics of stream influence on inundation.

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농촌유역의 산림지 면적 감소에 따른 유역 토양유실량 변화 추정 (Estimation of the Forestry Area Decrease Effect on the Soil Erosion in Rural Watershed)

  • 김상민;임상준;박승우
    • 농촌계획
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    • 제10권1호
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    • pp.19-26
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    • 2004
  • In this paper, forestry area change effect on the soil erosion in Asan lake watershed was estimated. Temporal variations of land use in the study watershed were analyzed from Landsat-5 TM remote sensing images. Geographic Information System (GIS) combined with Universal Soil Loss Equation (USLE) was used to estimate the soil erosion of Asan lake watershed. Spatial data for each USLE factors was obtained from the Landsat-5 TM remote sensing images and 1/25,000 scale digital contour maps. Sediment yield to Asan lake was estimated by sediment delivery ratio and sediment accumulation in lake was estimated by trap efficiency. The estimation methods were validated for sediment accumulation in Asan lake. From the hydrographic survey from 1974 to 2003 for Asan lake, sediment accumulation was measured. The estimated accumulation sediment of 303,569ton/yr showed similar value with observed of 295,888ton/yr. From the validated estimation methods, the increasing amount of soil erosion when 1% of forest area in Asan lake watershed decreases was calculated from 12.91 to 1482.05ton/yr.

Analysis of Land Use Change Impact on Storm Runoff in Anseongcheon Watershed

  • Park, Geun-Ae;Jung, In-Kyun;Lee, Mi-Seon;Shin, Hyung-Jin;Park, Jong-Yoon;Kim, Seong-Joon
    • 대한원격탐사학회지
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    • 제24권1호
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    • pp.35-43
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    • 2008
  • The purpose of this study is to evaluate the hydrological impact due to temporal land cover change by gradual urbanization of upstream watershed of Pyeongtaek gauging station of Anseong-cheon. WMS HEC-1 was adopted, and OEM with 200 m resolution and hydrologic soil group from 1:50,000 scale soil map were prepared. Land covers of 1986, 1990, 1994 and 1999 Landsat TM images were classified by maximum likelihood method. The watershed showed a trend that forest & paddy areas decreased and urban/residential area gradually increased during the four selected years. The model was calibrated at 2 locations (Pyeonglaek and Gongdo) by comparing observed with simulated discharge results for 5 summer storm events from 1998 to 2001. The watershed average CN values varied from 61.7 to 62.3 for the 4 selected years. To identify the impact of streamflow by temporal area change of a target land use, a simple evaluation method that the CN values of areas except the target land use are unified as one representative CN value was suggested. By applying the method, watershed average CN value was affected in the order of paddy, forest and urban/residential, respectively.

Watershed에 의한 형태분할 (Shape Segmentation by Watersheds)

  • 김태진;김주영;고광식
    • 대한전자공학회:학술대회논문집
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    • 대한전자공학회 1999년도 추계종합학술대회 논문집
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    • pp.573-576
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    • 1999
  • This paper presents a new shape segmentation algorithm. The procedure to achieve complete segmentation consists of two steps : the first step is mapping shape into two dimension by the using Distance Transform, the second step is partitioning the region by using the Watershed algorithm. As a application of the proposed algorithm, we perform the matching experiment for several objects by the use of segmented region. Simulation results demonstrate the efficiency of the proposed method, and the method has scale, rotation, and shift invariant properties.

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소규모 축산 유역의 수문/수질 모니터링 (Hydrologic and Water Quality Monitoring from a Small-Scale Livestock Watershed)

  • 이남호;윤광식;김성준;홍성구
    • 농촌계획
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    • 제7권2호
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    • pp.13-25
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    • 2001
  • Runoff and water quality was monitored from a watershed with small-scale livestock production farms. To evaluate pollution potential, land use, population, the size of livestock production of each farm, and livestock management method were surveyed. Climate and stream flow data were measured. Water samples were taken periodically for base flow conditions and some storm events. Pollutant loading was estimated by flow volume and concentrations of constituents. Delivery ratio of pollutant load was determined using estimated pollutant load.

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