• Title/Summary/Keyword: Upland watershed

검색결과 78건 처리시간 0.019초

농촌 소유역에서의 논과 밭의 지하수 영양물질 농도 비교 (Comparison of the nutrient concentration in ground water between paddy field and upland in a rural watershed)

  • 장훈;김진수;김영현
    • 한국수자원학회:학술대회논문집
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    • 한국수자원학회 2009년도 학술발표회 초록집
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    • pp.1994-1998
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    • 2009
  • Nutrients were investigated for surface water and ground water of paddy field and upland in a rural watershed from May 2008 to January 2009. The cocentrations of TN and $NO_3-N$ in ground water higher than those in surface water due to fertilization on cabbage upland neighboring a river during May to September, but lower than those in surface water during October to January. However, the concentrations TP and $PO_4-P$ in ground water were lower than those in surface water. TP and $PO_4-P$ concentrations in ground water of paddy field were generally lower than those of upland.

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WEPP 모형을 이용한 밭포장과 밭유역의 토양 유실량 추정 (Applications of WEPP Model to a Plot and a Small Upland Watershed)

  • 강민구;박승우;손정호;강문성
    • 한국농공학회논문집
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    • 제46권1호
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    • pp.87-97
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    • 2004
  • The paper presents the results from the applications of the Water Erosion Prediction Project (WEPP) model to a single plot, and also a small watershed in the Mid Korean Peninsula which is comprised of hillslopes and channels along the water courses. Field monitoring was carried out to obtain total runoff, peak runoff and sediment yield data from research sites. For the plot of 0.63 ha in size, cultivated with com, the relative error of the simulated total runoff, peak runoff rates, and sediment yields using WEPP ranged from -16.6 to 22%, from -15.6 to 6.0%, and from 23.9 to 356.4% compared to the observed data, respectively. The relative errors for the upland watershed of 5.1 ha ranged from -0.7 to 11.1 % for the total runoff, from -6.6 to 35.0 % for the sediment yields. The simulation results seem to justify that WEPP is applicable to the Korean dry croplands if the parameters are correctly defined. The results from WEPP applications showed that the major source areas contributing sediment yield most are downstream parts of the watershed where runoff concentrated. It was suggested that cultural practice be managed in such a way that the soil surface could be fully covered by crop during rainy season to minimize sediment yield. And also, best management practices were recommended based on WEPP simulations.

비점원오염 저감효과 분석을 위한 시단위 SWAT 유역 모델링 (Hourly SWAT Watershed Modeling for Analyzing Reduction Effect of Nonpoint Source Pollution Discharge Loads)

  • 장선숙;안소라;최중대;김성준
    • 한국농공학회논문집
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    • 제57권1호
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    • pp.89-97
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    • 2015
  • This study is to assess the effect of non-point source pollution discharge loads between tillage and no-tillage applications for upland crop areas using SWAT (Soil and Water Assessment Tool) watershed modeling. For Byulmi-cheon small rural catchment ($1.17km^2$) located in upstream of Gyeongan-cheon watershed, the rainfall, discharge and stream water quality have been monitored in the catchment outlet since 2011. The SWAT model was calibrated and validated in hourly basis using 19 rainfall events during 2011-2013. The average Nash-Sutcliffe model efficiency and $R^2$ (determination coefficient) for streamflow were 0.67 and 0.79 respectively. Using the 10 % surface runoff reduction from experiment results for no-tillage condition in field plots of 3 % and 8 % slopes under sesami cultivation, the soil saturated hydraulic conductivity for upland crop areas was adjusted from 0.001 mm/hr to 0.0025 mm/hr in average. Under the condition, the catchment sediment, T-N (total nitrogen, TN), and T-P (total phosphorus, TP) discharge loads were reduced by 6.9 %, 7.4 %, and 7.7 % respectively.

L-THIA를 이용한 낙동강수계 임하댐유역 비점오염원의 공간적 분포해석 (Spatial Analysis of Nonpoint Source Pollutant Loading from the Imha dam Watershed using L-THIA)

  • 전지홍;다니엘차;최동혁;김태동
    • 한국농공학회논문집
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    • 제55권1호
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    • pp.17-29
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    • 2013
  • Long-Term Hydrologic Impact Assessment (L-THIA) model which is a distributed watershed model was applied to analyze the spatial distribution of surface runoff and nonpoint source pollutant loading from Imha watershed during 2001~2010. L-THIA CN Calibration Tool linked with SCE-UA was developed to calibrate surface runoff automatically. Calibration (2001~2005) and validation (2006~2010) of monthly surface runoff were represented as 'very good' model performance showing 0.91 for calibration and 0.89 for validation as Nash-Sutcliffe (NS) values. Average annual surface runoff from Imha watershed was 218.4 mm and Banbyun subwatershed was much more than other watersheds due to poor hydrologic condition. Average annual nonpoint source pollutant loading from Imha wateshed were 2,295 ton/year for $BOD_5$, 14,752 ton/year for SS, 358 ton/year for T-N, and 79 ton/year for T-P. Amount of pollutant loading and pollutant loading rates from Banbyun watershed were much higher than other watersheds. As results of analysis of loading rate from grid size ($30m{\times}30m$), most of high 10 % of loading rate were generated from upland. Therefore, major hot spot area to manage nonpoint source pollution in Imha watershed is the combination of upland and Banbyun subwatershed. L-THIA model is easy to use and prepare input file and useful tool to manage nonpoint source pollution at screening level.

농촌 비점원 오염 모형을 이용한 농촌 소유역 축산농가 관리기법에 관한 연구(지역환경 \circled1) (A Study on the Farmstead Management in Small Agricultural Watershed using AGNPS model)

  • 이윤아;김성준;장석길
    • 한국농공학회:학술대회논문집
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    • 한국농공학회 2000년도 학술발표회 발표논문집
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    • pp.536-542
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    • 2000
  • The purpose of this study is to evaluate the effect of stream quality by the farmer's livestock wastes management in a typical small agricultural watershed. AGNPS model has the capability to adjust the level of pollutant load from farmstead and the fertilization level of upland field. A small agricultural watershed(4.12 $\textrm{km}^2$) which has as livestock farmhouses located in Gosan-myun, Ansung-gun was selected. AGNPS data were prepared by using Arc/info and Idrisi. 4 storm events in 1999 was used for runoff calibration, and 2 storm event which is measured in hourly-base at 4 locations along the stream were used for water quality(TN, TP) calibration. Model's behavior to stream quality for 3 cases was investigated. First, the variation of pollution produced from the cattle shed affected little to the stream quality because the cattle sheds were roofed. Second, the good management of ground in farmstead affected to stream quality with 11% and 17% decrease in TN and TP, respectively. Third, the reduction of fertilization level to upland field affected to stream quality with 27.2% and 38.5% decrease in TN and TP, respectively.

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USLE 및 GIS, RS를 이용한 서낙동강 유역 농경지 토양침식 위험도 평가 (Assessment of Arable Soil Erosion Risk in Seonakdong River Watershed using GIS, RS and USLE)

  • 고지연;이재생;정기열;윤을수;최영대;김춘식;김복진
    • 한국토양비료학회지
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    • 제39권3호
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    • pp.173-183
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    • 2006
  • 서낙동강 유역에서 USLE모형을 이용하여 농경지의 작물생산량 및 농업용수 수질과 관련 있는 농경지의 토양침식량을 평가하였다. 모형인자의 data set은 구축에 드는 노력과 시간의 소모를 최소화하고자 정밀토양도, 인공위성 영상 및 DEM자료로부터 RS와 GIS를 이용하여 구축하였는데, 토양상별 K 인자를 정밀토양도에 적용하여 주제도를 작성하고, 인공위성 영상(Landsat TM)으로부터 토지 피복도를 작성하여 C 및 P 인자의 주제도를 작성하였으며, DEM으로부터 LS 인자 주제도를 작성하였다. R인자는 서낙동강 유역 내에 위치하는 김해농업기술센터의 AWS 자료를 이용하여 계산하였다. 농경지발생 토양침식량은 유역전체 발생량의 31.5%였고, 농경지 토양유실량의 97.5%는 밭토양에서 일어나는 것으로 나타났다. 이는 서낙동강 유역이 삼각주평야지대로 경사가 거의 없으나 밭토양의 30.4%는 severe 및 very severe의 침식정도에 분포하였기 때문이다. 또한 식생의 토지 피복 상태 및 강우량의 정도에 따라 작물재배기(5월~9월)와 비재배기(10월~4월)로 나누어 토양침식량을 평가한 결과, 작물재배기는 연간 토양유실위험도와 유사한 경향이었고, 작물비재배포기는 R 값이 작물재포기의 약 1/5에 불과하였음에도 산과 인접한 경사지 밭토양의 일부는 severe 및 very severe의 토양침식 등급을 나타내어서 토양침식 관리에 주의가 필요하였다.

SWAT 모형을 이용한 시.공간적 토지 이용변화에 따른 유량 및 유사량 특성분석 (Analysis of Watershed Runoff and Sediment Characteristics due to Spatio-Temporal Change in Land Uses Using SWAT Model)

  • 신용철;임경재;김기성;최중대
    • 한국관개배수논문집
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    • 제14권1호
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    • pp.50-56
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    • 2007
  • In this study, the Soil and Water Assessment Tool (SWAT) model was used to assess spatiotemporal effects on watershed runoff and sediment characteristics due to land uses changes from 1999 to 2002 at the small watershed, located in Chuncheon-si, Gangwon province. The annual average flow rate of Scenario I (long-term simulation using land use of 1990), II (long-term simulation using land use of 1996), III(long-term simulation using land use of 200) and IV(simulation using land use of 1990, 1995, and 2000) in long-term simulation) using the SWAT model were 29,997,043 m3, 29,992,628 m3, 29,811,191 m3 and 29,931,238 m3, respectively. It was shown that there was no significant changes in estimated flow rate because no significant changes in land uses between 1990 and 2000 were observed. The annual average sediment loads of Scenarios I, II, III and IV for 15 year period were 36,643 kg/ha, 45,340 kg/ha , 27,195 kg/ha and 35,545 kg/ha, respectively. The estimated annual sediment loads from Scenarios I, II, and III, were different from that from the scenario IV, considering spatio-temporal changes in land use and meterological changes over the years, by 10%, 127%, and temporal changes in land use and meterological changes over the years, by 10%, 127%, and 77%. This can be explained in land use changes in high soil erosion potential areas, such as upland areas, within the study watershed. The comparison indicates that changes in land uses upland areas, within the study watershed. The comparison indicates that changes in land uses can affect on sediment yields by more than 10%, which could exceed the safety factor of 10% in Total Maximum Daily Loads (TMDLs). It is, therefore, recommended that not only the temporal analysis with the weather input data but also spatial one with different land uses need to be considered in long-term hydrology and sediment simulating using the SWAT model

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산림유역의 계류수질 현황 및 계절적 변동 특성 (Characteristics on Seasonal Variation of Stream Water Quality on Upland Headwater Streams in Forested Catchments)

  • 남수연;임홍근;이기문;최형태;양현제;김재훈
    • 한국물환경학회지
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    • 제38권5호
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    • pp.220-230
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    • 2022
  • Seasonal variability of water quality in the upland headwater streams in ten forested catchments (37.0~209.0 ha) was examined from April to November 2021. Here, seven physicochemical parameters were analyzed including pH, electrical conductivity (EC), biochemical oxygen demand (BOD), chemical oxygen demand (COD), total nitrogen (T-N), total phosphorous (T-P), and BOD/TOC. The parameters were compared with those of lowerland rivers as middle and lower reaches within a watershed. The pH showed was low (6.4~6.9) during all the seasons, however, BOD and BOD/TOC in the fall season were 2-fold higher than in the spring and summer seasons. Based on environmental standards, the water quality level revealed that the upland headwater streams maintained the purity and cleanliness of water except for pH in the summer season. BOD/TOC of all the seasons and BOD of the fall season in the upland headwater streams were higher than that in the lowerland rivers, whereas the rest of the physicochemical parameters in the upland headwater streams were lower than that in the lowerland rivers. Additionally, the water quality level maintained the purity and cleanliness of water as "Good" in two reaches. The unique aspects of our study design enabled us to draw inferences about water quality characteristics with temporal and spatial analysis in upland headwater streams. This design will be useful for the long-term strategy of effective water quality management for integrated upland headwater streams and lowerland rivers within a watershed.

간월호 유역의 토지이용 및 기후변화에 따른 논밭 필요수량 변화 추정 (Estimation of Crop Water Requirement Changes Due to Future Land Use and Climate Changes in Lake Ganwol Watershed)

  • 김시내;김석현;황순호;전상민;송정헌;강문성
    • 한국농공학회논문집
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    • 제63권6호
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    • pp.61-75
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    • 2021
  • This study aims to assess the changes in crop water requirement of paddy and upland according to future climate and land use changes scenarios. Changes in the spatiotemporal distribution of temperature and precipitation are factors that lower the stability of agricultural water supply, and predicting the changes in crop water requirement in consideration of climate change can prevent the waste of limited water resources. Meanwhile, due to the recent changes in the agricultural product consumption structure, the area of paddy and upland has been changing, and it is necessary to consider future land use changes in establishing an appropriate water use plan. Climate change scenarios were derived from the four GCMs of the CMIP6, and climate data were extracted under two future scenarios, namely SSP1-2.6 and SSP5-8.5. Future land use changes were predicted using the FLUS (Future Land Use Simulation) model. Crop water requirement in paddy was calculated as the sum of evapotranspiration and infiltration based on the water balance in a paddy field, and crop water requirement in upland was estimated as the evapotranspiration value by applying Penman-Monteith method. It was found that the crop water requirement for both paddy and upland increased as we go to the far future, and the degree of increase and variability by time showed different results for each GCM. The results derived from this study can be used as basic data to develop sustainable water resource management techniques considering future watershed environmental changes.