볏짚 피복에 의한 밭 비점오염원 유출저감효과 분석을 위한 HSPF와 SWAT 모델링

정충길,안소라,김성준,양희정,이형진,박근애,Jung, Chung Gil,Ahn, So Ra,Kim, Seong Joon,Yang, Hee Jeong,Lee, Hyung Jin,Park, Geun Ae 한국농공학회 2013 한국농공학회논문집 Vol.55 No.2

This study is to assess the reduction of non-point source pollution loads for rice straw mulching of upland crop cultivation at a watershed scale. For Byulmi-cheon watershed (1.21 $km^2$) located in the upstream of Gyeongan-cheon, the HSPF (Hydrological Simulation Program-Fortran) and SWAT (Soil and Water Assesment Tool), physically based distributed hydrological models were applied. Before evaluation, the model was calibrated and validated using 9 rainfall events. The Nash-Sutcliffe model efficiency (NSE) for streamflow using the HSPF was 0.62~0.76 and the determination coefficient ($R^2$) for water quality (sediment, total nitrogen T-N, and total phosphorus T-P) were 0.72, 0.62, and 0.63 respectively. The NSE for streamflow using the SWAT were 0.43~0.81 and the $R^2$ for water quality (sediment, T-N, and T-P) were 0.54, 0.87, and 0.64 respectively. From the field experiment of 16 rainfall events, the rice straw cover condition reduced surface runoff average 10.0 % compared to normal surface condition. By handling infiltration capacity (INFILT) in HSPF model, the value of 16.0 mm/hr was found to reduce about 10.0 % reduction of surface runoff. For this condition, the reduction effect of sediment, T-N, and T-P loads were 87.2, 28.5, and 85.1 % respectively. By handling soil hydraulic conductivity (SOL_K) in SWAT model, the value of 111.2 mm/hr was found to reduce about 10.0 point reduction of surface runoff. For this condition, the reduction effect of sediment, T-N, and T-P loads were 80.0, 83.2, and 78.7 % respectively. The rice straw surface covering was effective for removing surface runoff dependent loads such as sediment and T-P.

설마천 유역 CO₂ Flux 실측 자료에 의한 총일차생산성 (GPP)과 MODIS GPP간의 비교 평가

정충길,신형진,박민지,조형경,김성준 한국농공학회 2011 한국농공학회논문집 Vol.53 No.2

In this study, In order to evaluate reliable of MODIS GPP, the MODIS GPP and Flux tower measured GPP were compared to evaluate the use of method on 8 days composite MODIS GPP. The 2008 Flux data (CO₂Flux and air temperature) measured in Seolmacheon watershed (8.48 ㎢) were used. The Flux tower GPP was estimated as the sum of CO₂Flux and Re(ecosystem respiration) by Lloyd and Taylor method (1994). The summer Monsoon period from June to August mostly contributed the underestimation of MODIS GPP by cloud contamination on MODIS pixels. The 2008 MODIS GPP and Flux tower GPP of the watershed were 1133.2 g/m2/year and 1464.3 g/m2/year respectively and the determination coefficient (R2) after correction of cloud-originated errors was 0.74 (0.63 before correction). Even though effect of Cloud-Originated Errors was eliminated, Solar radiation and Temperature are affected at GPP. Measurement of correct GPP is difficult. But, If errors of MODIS GPP analyze on Cloud Moonsoon Climate in korea and eliminated effect of Cloud-Originated Errors, MODIS GPP will be considered GPP increasing of 9 %. There, Our results indicate that MODIS GPP show reliable and useful data except for summer period in Moonsoon Climate.

수생태 환경유지를 위한 하천생태유량 산정

정충길,이지완,안소라,황순진,김성준,Jung, Chung-Gil,Lee, Ji-Wan,Ahn, So-Ra,Hwang, Soon-Jin,Kim, Seong-Joon 한국농공학회 2016 한국농공학회논문집 Vol.58 No.3

The objective of this study is to analyze the relationship between stream water quality of TN (total nitrogen), TP (total phosphorus), and BOD (Biochemical Oxygen Demand) and TDI (Trophic Diatom Index) score determined by physico-chemical factors, biomass, and standing crops of epilithic diatoms, and to estimate the required amount of ecological streamflow for good water environment of Trophic Diatom. For the main stream of Chungju dam watershed of South Korea, total 100 field data of 3 years (2008~2010) measured in May and September were used to derive the relationship between water quality and TDI. Trophic Diatom had high correlation (0.55 determination coefficient) with TN. Using the relationship, the required streamflow was evaluated by using the Soil Water Assessment Tool (SWAT) for good Trophic Diatom water environment through T-N water quality maintenance. The SWAT simulated 8 years (2003~2010) stream discharges and T-N water quality along the main stream. From present garde C (score range: 30.0~45.0) to grade A (score above 60.0) of TDI, the May needs additional streamflow of $63.1m^3/sec$ (+36.7 % comparing with the present streamflow of $172.0m^3/sec$) at the watershed outlet.

볏짚 피복에 의한 밭 비점원오염 저감효과 분석을 위한 HSPF 모델링

정충길,박종윤,이형진,최중대,김성준,Jung, Chung-Gil,Park, Jong-Yoon,Lee, Hyung-Jin,Choi, Joong-Dae,Kim, Seong-Joon 한국농공학회 2012 한국농공학회논문집 Vol.54 No.4

This study is to assess the reduction of non-point source pollution loads for rice straw surface covering of upland crop cultivation at a watershed scale. For Byulmi-cheon watershed ($1.21km^2$) located in the upstream of Gyeongancheon, the HSPF (Hydrological Simulation Program-Fortran), a physically based distributed hydrological model was applied. Before evaluation, the model was calibrated and validated using 9 rainfall events. The Nash-Sutcliffe model efficiency (NSE) for streamflow was 0.62~0.78 and the NSE for water quality (Sediment, T-N, and T-P) were 0.68, 0.60, and 0.58 respectively. From the field experiment of 16 rainfall events, the rice straw covering reduced surface runoff average 10 % compared to normal surface condition. By handling infiltration parameter (INFILT) in the model, the value of 16.0 mm/hr was found to reduce about 10 % reduction of surface runoff. For this condition, the reduction effect of Sediment, T-N, and T-P loads were 87.2, 28.5, and 85.1 % respectively. The rice straw surface covering was effective for removing surface runoff dependent loads such as Sediment and T-P.

SWAT 모델링을 이용한 한강유역의 RCP 시나리오에 따른 미래수문 및 융설 영향평가

정충길,문장원,장철희,이동률,Jung, Chung Gil,Moon, Jang Won,Jang, Cheol Hee,Lee, Dong Ryul 한국농공학회 2013 한국농공학회논문집 Vol.55 No.5

The objective of this study is to assess the impact of potential climate change on the hydrological components, especially on the streamflow, evapotranspiration and snowmelt, by using the Soil Water Assessment Tool (SWAT) for 17 Hanriver middle watersheds of South Korea. For future assessment, the SWAT model was calibrated in multiple sites using 4 years (2006-2009) and validated by using 2 years (2010-2011) daily observed data. For the model validation, the Nash-Sutcliffe model efficiency (NSE) for streamflow were 0.30-0.75. By applying the future scenarios predicted five future time periods Baseline (1992-2011), 2040s (2021-2040), 2060s (2041-2060), 2080s (2061-2080) and 2100s (2081-2100) to SWAT model, the 17 middle watersheds hydrological components of evapotranspiration, streamflow and snowmelt were evaluated. For the future precipitation and temperature of RCP 4.5 scenario increased 41.7 mm (2100s), $+3^{\circ}C$ conditions, the future streamflow showed +32.5 % (2040s), +24.8 % (2060s), +50.5 % (2080s) and +55.0 % (2100s). For the precipitation and temperature of RCP 8.5 scenario increased 63.9 mm (2100s), $+5.8^{\circ}C$ conditions, the future streamflow showed +35.5 % (2040s), +68.9 % (2060s), +58.0 % (2080s) and +63.6 % (2100s). To determine the impact on snowmelt for Hanriver middle watersheds, snowmelt parameters of SWAT model were determined through evaluating observed streamflow data during snowmelt periods (November-April). The results showed that average SMR (snowmelt / runoff) of 17 Hanriver middle watersheds was 62.0 % (Baseline). The annual average SMR were 42.0 % (2040s), 39.8 % (2060s), 29.4 % (2080s) and 27.9 % (2100s) by applying RCP 4.5 scenario. Also, the annual average SMR by applying RCP 8.5 scenario were 40.1 % (2040s), 29.4 % (2060s), 18.3 % (2080s) and 12.7 % (2100s).

농업 비점오염원 평가를 위한 SWAT-APEX 모델의 적용성 검토

정충길,박종윤,이지완,정혁,김성준,Jung, Chung-Gil,Park, Jong-Yoon,Lee, Ji-Wan,Jung, Hyuk,Kim, Seong-Joon 한국농공학회 2011 한국농공학회논문집 Vol.53 No.5

This study is to check the applicability of SWAT-APEX (Soil and Water Assessment Tool-Agricultural Policy / Environmental eXtender) model as combined watershed and field models by applying the APEX to paddies in a watershed (465.1 $km^2$) including Yedang reservoir. Firstly, the SWAT were calibrated with 3 years (2000~2002) daily streamflow and monthly water quality (T-N and T-P) data, and validated for another 3 years (2003~2005) data. The average Nash-Sutcliffe model efficiency (ME) of streamflow during validation was 0.73, and the coefficient of determination ($R^2$) of T-N and T-P were 0.77 and 0.73 respectively. Next, running the SWAT-APEX model with the SWAT calibrated parameters for paddies, the $R^2$ of T-N and T-P were 0.80 and 0.76 respectively. The results showed that SWAT-APEX model was more correctly predicted for T-N and T-P loads than SWAT model. The difference results between watershed and field models was predicted to have substantial impact on NPS loads, especially on T-N and T-P loads. Therefore, to improve negative NPS load simulations should be considered the model characteristics as simulating mechanism to properly select the NPS model for agricultural watershed.

설마천 유역 CO₂ Flux 실측 자료에 의한 총일차생산성 (GPP)과 MODIS GPP간의 비교 평가

정충길,신형진,박민지,조형경,김성준,Jung, Chung-Gill,Shin, Hyung-Jin,Park, Min-Ji,Joh, Hyung-Kyung,Kim, Seong-Joon 한국농공학회 2011 한국농공학회논문집 Vol.53 No.2

In this study, In order to evaluate reliable of MODIS GPP, the MODIS GPP and Flux tower measured GPP were compared to evaluate the use of method on 8 days composite MODIS GPP. The 2008 Flux data ($CO_2$ Flux and air temperature) measured in Seolmacheon watershed ($8.48\;km^2$) were used. The Flux tower GPP was estimated as the sum of $CO_2$ Flux and $R_{ec}$ (ecosystem respiration) by Lloyd and Taylor method (1994). The summer Monsoon period from June to August mostly contributed the underestimation of MODIS GPP by cloud contamination on MODIS pixels. The 2008 MODIS GPP and Flux tower GPP of the watershed were $1133.2\;g/m^2/year$ and $1464.3\;g/m^2/year$ respectively and the determination coefficient ($R^2$) after correction of cloud-originated errors was 0.74 (0.63 before correction). Even though effect of Cloud-Originated Errors was eliminated, Solar radiation and Temperature are affected at GPP. Measurement of correct GPP is difficult. But, If errors of MODIS GPP analyze on Cloud Moonsoon Climate in korea and eliminated effect of Cloud-Originated Errors, MODIS GPP will be considered GPP increasing of 9 %. There, Our results indicate that MODIS GPP show reliable and useful data except for summer period in Moonsoon Climate.

플럭스 타워 설치 유역을 대상으로 탄소수지 분석을 위한 위성영상자료기반의 CO2 정량화 연구

정충길,이용관,김성준,장철희 한국농공학회 2015 한국농공학회논문집 Vol.57 No.3

Spatial heterogeneous characteristics of solar radiation energy from Climate Change gives rise to energy imbalance in the general ecological system including water resources. This study is to estimate the CO2 flux of South Korea using Terra MODIS image and to assess the reliability of MODIS data from the ground measured CO2 flux by eddy covariance flux tower data at 3 locations (two at mixed forest area and one at rice paddy area). The MODIS Gross Primary Productivity (GPP) product (MOD17A2), 8-day composite at 1-km spatial resolution was adopted for the spatial CO2 flux generation. The MOD17A2 data by noise like cloud and snow in a day were tried to fill by Inverse Distance Weighted (IDW) method from valid pixels and the damping effect of MOD17A2 data were corrected by Quality Control (QC) flag. The MODIS CO2 flux was estimated as the sum of GPP and Re (ecosystem respiration) by Lloyd and Taylor method (1994). The determination coefficient (R2) between MODIS CO2 and flux tower CO2 for 3 years (2011~2013) showed 0.55 and 0.60 in 2 mixed forests and 0.56 in rice paddy respectively. The CO2 flux generally fluctuated showing minus values during summer rainy season (from July to August) and maintaining plus values for other periods. The MODIS CO2 flux can be a useful information for extensive area, for example, as a reliable indicator on ecological circulation system.

머신러닝을 이용한 영산강 및 섬진강수계 갈수예보 전망 기술 소개

정충길,오창열,Jeong, Chung-Gil,O, Chang-Yeol 한국수자원학회 2020 물과 미래(한국수자원학회지) Vol.53 No.10

분포형 강우-유출 모형의 입력자료 해상도에 따른 유출변동 연구

정충길,문장원,이동률 한국수자원학회 2014 한국수자원학회논문집 Vol.47 No.9

최근 기후변화에 의한 기상이변이 발생하고 국지적 집중호우로 인한 홍수피해가 심각하게 증가하고 있다. 이러한 피해를 경감하기 위한 방법으로 정확한 홍수유출량 예측을 통한 홍수예경보 구축이 필요시 된다. 정확한 홍수유출량 예측을 위해 수문기상학적 요소와 특성인자들의 정확한 상호 연관성 규명과 공간적 변동성 해석은 강우-유출 모형에서 발생하는 불확실성을 감소시키는데 중요한 요소로 작용하게 된다. 본 연구에서는 정확한 홍수유출량을 산정하기 위한 강우-유출모형을 이용한 입력자료의 해상도에 따른 불확실성을 감소시키기 위해 강우격자 해상도와 지형인자 격자 해상도에 따라 강우-유출모형이 어떻게 반응하는지 분석하였다. 분포형 강우-유출 모형인 GRM 모형을 이용하여 내성천 및 감천 유역을 대상으로 이벤트를 산정하여 홍수유출 모의 및 검증을 실시하였다. GRM 모형 구성을 위한 입력자료(강우, DEM, 토지이용도, 토양도)의 해상도 격자크기는 500m 격자크기를 기본으로 각각 1 km, 2 km, 5 km, 10 km, 12 km 격자크기의 지형자료를 사용하여 유출모의를 실시하고 유출량 변화를 모의하였다. 입력자료별 모의결과로 DEM의 분석결과는 모든 시험유역에서 공통적으로 DEM의 격자크기가 증가할수록 첨두유량과 총유출량이 일정하게 감소하는 경향을 나타내고 있다. 나머지 입력자료로 토지이용 및 토양도에 격자크기에 따른 모의결과는 DEM과는 상반되게 일정한 경향성을 나타나지 않는 것으로 분석되었다. 특히 일정한 경향성이 나타나는 DEM의 분석결과는 DEM의 격자크기가 증가할수록 수평거리가 증가하여 경사도는 감소하는 특징으로 인해 나타나는 결과인 것으로 판단된다. Changes in climate have largely increased concentrated heavy rainfall, which in turn is causing enormous damages to humans and properties. Floods are one of the most deadly and damaging natural disasters known to mankind. The flood forecasting and warning system concentrates on reducing injuries, deaths, and property damage caused by floods. Therefore, the exact relationship and the spatial variability analysis of hydrometeorological elements and characteristic factors is critical elements to reduce the uncertainty in rainfall-runoff model. In this study, grid resolution depending on the topographic factor in rainfall-runoff models presents how to respond. semi-distribution of rainfall-runoff model using the model GRM simulated and calibrated rainfall-runoff in the Gamcheon and Naeseongcheon watershed. To run the GRM model, input grid data used rainfall (two event), DEM, landuse and soil. This study selected cell size of 500 m(basic), 1 km, 2 km, 5 km, 10 km and 12 km. According to the resolution of each grid, in order to compare simulation results, the runoff hydrograph has been made and the runoff has also been simulated. As a result, runoff volume and peak discharge which simulated cell size of DEM 500 m~12 km were continuously reduced. that results showed decrease tendency. However, input grid data except for DEM have not contributed increase or decrease runoff tendency. These results showed that the more increased cell size of DEM make the more decreased slope value because of the increased horizontal distance.