• Title/Summary/Keyword: Hydrologic simulation program-fortran (HSPF)

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Predicting Runoff and Sediment Yield on a Forest Dominated Watershed using HSPF and SWAT Models (HSPF와 SWAT 모형을 이용한 산림유역의 유출 및 유사량 추정)

  • Im Sang-Jun;Brannan Kevin M.;Mostaghimi Saied;Cho, Jae-Pil
    • Journal of Korean Society of Rural Planning
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    • v.9 no.4 s.21
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    • pp.59-64
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    • 2003
  • U.S. EPA의 BASINS (Better Assessment Science Integrating Point and Nonpoint Sources)에 통합되어 있는 HSPF (Hydrologic Simulation Program-Fortran)와 SWAT (Soil and Water Assessment Tool) 모형을 이용하여 Polecat Creek 유역의 유출과 유사량을 모의하였다. 모형의 보정을 위하여 1996년 9월부터 2000년 6월까지의 하천 유량 및 유사 농도 자료를 이용하였으며, 1994년 10월부터 1995년 12월까지의 관측자료를 이용하여 모형의 검정을 실시하였다. HSPF 모형에 의해 추정된 연 평균 유출량의 상대오차는 보정 및 검정기간에 각각 0.8%, 0.5%이었으며, S WAT 모형에 의해 추정된 연평균 유출량은 실측치와 각각 2.1%, 16.1%의 오차를 보였다. 연 평균 유사량을 비교하면, HSPF 모형이 보정 및 검정기 간에 각각 8.8%와 7.2%의 오차를 보인 반면에 SWAT 모형은 각각 40.0%, 188.4%의 차이를 보였다. HSPF 모형에 의해 추정된 월 평균 유출량 및 유사량의 상관계수는 보정기간에 대하여 0.94와 0.52이었으며, SWAT 모형에 의한 결과는 상관계수가 각각 0.84와 0.39이었다. 이상의 연구 결과에 의하면, HSPF 모형이 SWAT 모형보다 유출과 유사량을 관측치와 유사하게 모의함을 알 수 있었다. 하지만 입력 자료의 구축 및 모형의 적용에는 SWAT모형보다 많은 시간과 노력을 필요로 하였다.

A Study on the Discharge Characteristics of Pollutant Loads in Small Watershed According to the Probability Rainfall (확률 강우에 따른 홍수 전후의 소유역 오염부하량 배출특성 연구)

  • Kim, Phil-Sik;Kim, Sun-Joo;Shim, Jae-Hoon
    • Journal of The Korean Society of Agricultural Engineers
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    • v.52 no.6
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    • pp.75-83
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    • 2010
  • The objective of this paper is to study the discharge characteristics of pollutant loads in small watershed according to probability rainfall using the Hydrologic Simulation Program-Fortran (WinHSPF). The subwatershed of Gosam reservoir watershed in Gyeonggido province was simulated and the probability rainfall of study area was estimated by recurrence interval and duration. The probability rainfalls are 156.5, 205.9 and 277.4 mm for 6 hrs, 12 hrs and 24 hrs in 10 year frequency, and each probability rainfalls is distributed by Huff's 4th quantiles method and applied to HSPF. The pollutant loads were high for initial rainfall. The concentrations of TN, TP and BOD were high as rainfall duration is shorter and rainfall intensity is higher.

Review of Features and Applications of Watershed-scale Modeling, and Improvement Strategies of it in South-Korea (유역 모델 특성 및 국내 적용 현황과 발전 방향에 대한 검토)

  • Park, Youn Shik;Ryu, Jichul;Kim, Jonggun;Kum, Donghyuk;Lim, Kyoung Jae
    • Journal of Korean Society on Water Environment
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    • v.36 no.6
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    • pp.592-610
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    • 2020
  • In South Korea, the concept of water environment was expanded to include aquatic ecosystems with the Integrated Water Management implementation. Watershed-scale modeling is typically performed for hydrologic component analysis, however, there is a need to expand to include ecosystem variability such that the modeling corresponds to the social and political issues around the water environment. For this to be viable, the modeling must account for several distinct features in South Korean watersheds. The modeling must provide reasonable estimations for peak flow rate and apply to paddy areas as they represent 11% of land use area and greatly influence groundwater levels during irrigation. These facts indicate that the modeling time intervals should be sub-daily and the hydrologic model must have sufficient power to process surface flow, subsurface flow, and baseflow. Thus, the features required for watershed-scale modeling are suggested in this study by way of review of frequently used hydrologic models including: Agricultural Policy/Environmental eXtender(APEX), Catchment hydrologic cycle analysis tool(CAT), Hydrological Simulation Program-FORTRAN(HSPF), Spatio-Temporal River-basin Ecohydrology Analysis Model(STREAM), and Soil and Water Assessment Tool(SWAT).

Proposal of Soil Parameter Range of HSPF Considering Available Water Capacity According to Soil Layer (토양층에 따른 유효수분량을 고려한 HSPF의 토양 별 매개변수 범위 제안)

  • Kim, SooHong;Lee, Dongjun;Han, JeongHo;Yang, DongSeok;Kim, JongGun
    • Proceedings of the Korea Water Resources Association Conference
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    • 2019.05a
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    • pp.113-113
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    • 2019
  • 하천 오염 부하의 양적 증가를 해결하기 위해 환경부는 유역 내 목표 수질을 설정하고 목표 수질한도 내에서 오염물질 배출 총량을 할당하는 수질오염총량제를 도입하였다. 수질오염총량제 시행에 있어 시계열로 발생하는 유출특성을 반영하기 위해 장기유출모형의 적용이 가능한 Hydrologic Simulation Program-Fortran(HSPF)을 수질관리 및 평가 모델로 사용하고 있다. 그러나 HSPF 모델은 실제 다양한 특성을 가진 토양층을 Upper zone과 Lower zone 내에 통합적인 매개변수를 이용하여 유량을 모의하는 문제점이 있다. 이는 토양 내부에서의 유출에 대한 정확한 모의가 이루어지지 않는 결과를 초래할 수 있다. 따라서 본 연구에서는 국내 토양층에 따른 Available Water Capacity(AWC)에 대한 자료를 구축하고 기존보다 세분화된 토양 관련 매개변수 범위를 제시하였다. 본 연구에서 제시한 토양 관련 매개변수 범위를 반영할 경우 수질오염총량제 시행에 있어 HSPF 모델 모의 시 유역 내의 토양도를 고려하여 보다 정확한 중간유출과 기저유출분석이 가능할 것이라 사료된다.

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Analysis of Livestock Nonpoint Source Pollutant Load Ratio for Each Sub-watershed in Sancheong Watershed using HSPF Model (HSPF 모형을 이용한 산청 유역의 소유역별 축산비점오염부하량 비중 분석)

  • Kim, So Rae;Kim, Sang Min
    • Journal of The Korean Society of Agricultural Engineers
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    • v.62 no.1
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    • pp.39-50
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    • 2020
  • The objective of this study was to assess the livestock nonpoint source pollutant impact on water quality in Namgang dam watershed using the HSPF (Hydrological Simulation Program-Fortran) model. The input data for the HSPF model was established using the landcover, digital elevation, and watershed and river maps. In order to apply the pollutant load to the HSPF model, the delivery load of the livestock nonpoint source in the Namgang dam watershed was calculated and used as a point pollutant input data for the HSPF model. The hydrologic and water quality parameters of HSPF model were calibrated and validated using the observed runoff data from 2007 to 2015 at Sancheong station. The R2 (Determination Coefficient), RMSE (Root Mean Square Error), NSE (Nash-Sutcliffe efficiency coefficient), and RMAE (Relative Mean Absolute Error) were used to evaluate the model performance. The simulation results for annual mean runoff showed that R2 ranged 0.79~0.81, RMSE 1.91~2.73 mm/day, NSE 0.7~0.71 and RMAE 0.37~0.49 mm/day for daily runoff. The simulation results for annual mean BOD for RMSE ranged 0.99~1.13 mg/L and RMAE 0.49~0.55 mg/L, annual mean TN for RMSE ranged 1.65~1.72 mg/L and RMAE 0.55 mg/L, and annual mean TP for RMSE ranged 0.043~0.055 mg/L and RMAE 0.552~0.570 mg/L. As a result of livestock nonpoint pollutant loading simulation for each sub-watersehd using the HSPF model, the BOD ranged 16.6~163 kg/day, TN ranged 27.5~337 kg/day, TP ranged 1.22~14.1 kg/day.

Watershed-scale Hydrologic Modeling Considering a Detention Effect of Rice Paddy Fields using HSPF Surface-Ftable (논의 저류효과를 고려한 유역수문모델링 - HSPF Surface-Ftable의 적용 -)

  • Seong, Chounghyun;Oh, Chansung;Hwang, Syewoon
    • Journal of The Korean Society of Agricultural Engineers
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    • v.60 no.5
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    • pp.41-54
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    • 2018
  • A method to account a detention in a rice paddy field in hydrologic modeling was tested at plot and watershed scales. Hydrologic Simulation Program - Fortran (HSPF) and its one of surface runoff modeling method, i.e Surface-Ftable, were used to simulate a inundated condition in a rice paddy culture for a study plot and basins in Saemangeum watershed. Surface-Ftable in HSPF defines surface runoff ratio with respect to surface water depth in a pervious land segment, which can be implemented to the feature of water management in a rice paddy field. A Surface-Ftable for paddy fields in Saemangeum watershed was developed based on the study paddy field monitoring data from 2013 to 2014, and was applied to Jeonju-chun and Jeongeup-chun basins which comprise 12% and 22% of paddy fields in the basins, respectively. Four gaging stations were used to calibrate and validate the watershed models for the period of 2009 and 2013. Model performed 7.13% and 9.68% in PBIAS, and 0.94 and 0.90 in monthly NSE during model calibrations at Jeonju and Jeongeup stations, respectively, while the models were validated its applicability at Hyoja and Gongpyung stations. The comparison of results with and without considering detention effect of paddy fields confirmed the validity of the Surface-Ftable method in modeling watersheds containing rice paddy fields.

CALIBRATION AND VALIDATION OF THE HSPF MODEL ON AN URBANIZING WATERSHED IN VIRGINIA, USA

  • Im, Sang-Jun;Brannan, Kevin-M.;Mostaghimi, Saied
    • Water Engineering Research
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    • v.4 no.3
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    • pp.141-154
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    • 2003
  • Nonpoint source pollutants from agriculture are identified as one of the main causes of water quality degradation in the United States. The Hydrological Simulation Program-Fortran (HSPF) was used to simulate runoff, nitrogen, and sediment loads from an urbanizing watershed; the Polecat Creek watershed located in Virginia. Model parameters related to hydrology and water quality were calibrated and validated using observed hydrologic and water quality data collected at the watershed outlet and at several sub-watershed outlets. A comparison of measured and simulated monthly runoff at the outlet of the watershed resulted in a correlation coefficient of 0.94 for the calibration period and 0.74 for the validation period. The annual observed and simulated sediment loads for the calibration period were 220.9 kg/ha and 201.5 kg/ha, respectively. The differences for annual nitrate nitrogen ($NO_3$) loads between the observed and simulated values at the outlet of the watershed were 5.1% and 42.1% for the calibration and validation periods, respectively. The corresponding values for total Kjeldahl nitrogen (TKN) were 60.9% and 40.7%, respectively. Based on the simulation results, the calibrated HSPF input parameters were considered to adequately represent the Polecat Creek watershed.

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A study on water quality change by land use change using HSPF

  • Kim, Tae Geun;Choi, Kyoung-sik
    • Environmental Engineering Research
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    • v.25 no.1
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    • pp.123-128
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    • 2020
  • Non-point source pollutant load reductions were calculated using the Hydrologic Simulation Program-Fortran (HSPF) model under the assumption that landuse pattern was changed according to land purchases. Upon the simulation of non-point pollutant and areas with high land purchase ratios to select a buffer zone, the Namgang dam Reach 11, Imha dam Reach 10, and the Reach 136 watershed of the main river were found to rank high for the construction of buffer zones. Assuming that the forms of the purchased lands were changed to wetlands, biological oxygen demand (BOD) loads were changed through the HSPF model. No changes of BOD were present in the Namgang dam and the Imha dam watersheds. BOD loads in Reach 136 according to landuse change were analyzed through a flow duration analysis based on the total maximum daily loads of the United States. The flow duration analyses undertaken to examine changes in BOD of main river Reach 136 watershed indicated a shift of 0.64 kg/d from 3.16 to 2.52 during high flow. The change of BOD under the conditions of moist, mid-range and dry were 11.9%, 9% and 4.5%. At the low flow condition, the variation range in the BOD load was from 0.58 kg/d to 0.41 kg/d.

Streamflow Modeling in Data-scarce Estuary Reservoir Watershed Using HSPF (HSPF 모형과 호소 물수지를 이용한 미계측 간척 담수화호 수문모델링)

  • Seong, Choung Hyun
    • Journal of The Korean Society of Agricultural Engineers
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    • v.56 no.6
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    • pp.129-137
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    • 2014
  • This research presents an streamflow modeling approach in a data-scarce estuary reservoir watershed which has been suffered from high salinity irrigation water problem after completion of land reclamation project in South Korea. Since limited hydrology data was available on the Iwon estuary reservoir watershed, water balance relation of the reservoir was used to estimate runoff from upstream of the reservoir. Water balance components in the reservoir consists precipitation, inflow from upstream, discharge through sluice, and evaporation. Estimated daily inflow data, which is stream discharge from upstream, shows a good consistency with the observed water level data in the reservoir in terms of EI (0.93) and $R^2$ (0.94), and were used as observed flow data for the streamflow modeling. HSPF (Hydrological Simulation Program - Fortran) was used to simulate hydrologic response of upstream of the reservoir. The model was calibrated and validated for the periods of 2006 to 2007 and 2008 to 2009, respectively, showing that values of EI and $R^2$ were 0.89 and 0.91 for calibration period, 0.71 and 0.84 for validation period.

Application of land cover and soil information for improvement of HSPF modeling accuracy (HSPF 예측 정확도 제고를 위한 토지피복 및 토양 특성 자료의 활용)

  • Kang, Yooeun;Kim, Jaeyoung;Seo, Dongil
    • Journal of Korea Water Resources Association
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    • v.55 no.10
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    • pp.823-833
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    • 2022
  • This study aims to improve the runoff modeling accuracy of a basin using Hydrological Simulation Program-FORTRAN (HSPF) model by considering nonhomogeneous characteristics of a basin. By entering classified values according to the various types of land cover and soil to the parameters in HSPF-roughness coefficient (NSUR), infiltration (INFILT), and evapotranspiration (LZETP)- the heterogeneity of the Yongdam Dam basin was reflected in the model. The results were analyzed and compared with the one where the parameters were set as a single value throughout the basin. The flow rate and water quality simulation results showed improved results when classified parameters were used by land cover and soil type than when single values were used. The parameterization changed not only the flow rate, but also the composition ratio of each hydrologic components such as surface runoff, baseflow, and evapotranspiration, which shows the impact of the value set to a parameter on the entire hydrological process. This implies the importance of considering the heterogeneous characteristics of the land cover and soil of the basin when setting the parameters in a model.