• Magazine of the Korean Society of Agricultural Engineers
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• v.37 no.3_4
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• pp.23-33
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• 1995

Geographic data which are difficult to handle by the characteristics of spatial variation and variety turned into a possibility to analyze with tlie computer-aided digital map and the use of Geographic Information System(GIS). The purpose of this study is to develop and apply a GIS application model (GISCELWAB) for the spatial simulation of surface runoff from a small watershed. This paper discribes the modeling procedure and the applicability of the cell water balance model (CELWAB) which calculates the water balance of a cell and simulates surface runoff of watershed simultaneously by the interaction of cells. The cell water balance model was developed to simulate the temporal and spatial storage depth and surface runoff of a watershed. The CELWAB model was constituted by Inflow-Outflow Calculator (JOC) which was developed to connect cell-to-cell transport mechanism automatically in this study. The CELWAB model requests detail data for each component of a cell hydrologic process. In this study, therefore, BANWOL watershed which have available field data was selected, and sensitivity for several model parameters was analyzed. The simulated results of surface runoff agreed well with the observed data for the rising phase of hydrograph except the recession phase. Each mean of relative errors for peak discharge and peak time was 0.21% and2.1 1% respectively. In sensitivity analysis of CELWAB , antecedent soil moisture condition(AMC) affected most largely the model.

• Journal of The Korean Society of Agricultural Engineers
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• v.59 no.6
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• pp.101-108
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• 2017

This study attempted to improve the accuracy of streamflow and baseflow prediction of Soil and Water Assessment Tool (SWAT) by applying baselfow recession constants for each sub-watershed. This study set two different scenarios (S1 and S2) to evaluate the impact of application of baseflow recession constants for each sub-watershed on streamflow prediction. In S1, Only the baseflow recession constant obtained from the streamflow station located in the final outlet of study area was applied for whole sub-watersheds. In S2, baseflow recession constants obtained from six different streamflow stations were applied for each sub-watershed. Then, baseflow was separated form the measured streamflow data and the predicted streamflow of S1 and S2 using Web-based Hydrograph Analysis Tool (WHAT). The results showed Nash-Sutcliff efficiency (NSE) and $R^2$ of S2 were a little higher than these of S1 in both streamflow and baseflow prediction results. However, it is important that S2 reflected physical meaning of baseflow recess. Also, recession part of hydrograph in S2 was calibrated better than that of S1 compared to the measured hydrograph.

• Proceedings of the Korea Water Resources Association Conference
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• 2016.05a
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• pp.551-551
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• 2016

북한과의 대표적 공유하천인 임진강 유역은 유역의 2/3를 차지하고 있는 북한지역내에서 신뢰할만한 강우 및 수문관련 정보에 접근할 수 없는 문제점이 존재한다. 또한, 임진강 중류에는 북한에서 운영하는 황강댐의 예고없는 수문운영에 따라 수시로 하류 홍수피해가 발생할 수 있는 상황이며, 이에 대비하여 우리나라에는 군남 홍수조절지를 건설하여 운영하고 있다. 하지만 임진강 상류에 대한 수문정보를 취득하기 어렵기 때문에 가까운 수위관측소의 수위변화와 저류함수 모형 등을 이용하여 댐 운영을 실시하고 있는 것이 현실이다. 본 연구에서는 미계측유역에서의 수문정보를 확보하기 위한 목적으로 레이다강우 등 원격탐사정보와 분포형 강우-유출모형을 이용하여 황강댐 유입량을 산정할 수 있는 수문모형을 구축하였다. 황강댐유역의 수문모형 실매개변수를 보정하기 어렵기 때문에 인근 한탄강댐유역의 매개변수를 지역화를 통하여 전이하여 활용하였다. 산정된 수문곡선은 동시간대 한탄강댐 유입량의 면적비적용, 강수의 공간전이후 산정된 한탄강댐 유입량의 면적비적용등의 다양한 시나리오에서 모의된 수문곡선과의 비교를 수행하여 본 기법의 타당성을 입증하고자 시도하였다. 또한 군남홍수조절지 유입수문곡선과의 비교를 통하여 황강댐과 4월 5일댐의 수문운영현황 및 잔유역유입량을 역추정코자 하였다.

• Journal of the Korean Geophysical Society
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• v.7 no.2
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• pp.151-155
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• 2004

To solve the urban flood problems, it must get the enough channel conveyances and pumping capacities. It needs set up the detention system to control the flow over the channel capacity. Inspite of this detention system, the peak flow may increased by rainfall distribution and the delay of flow. This shows a design model of detention system which can consider the time problems from mutual connections of the detention storages and pumping flow using IDP(Incremental Dynamic Programming) method.

• Journal of The Geomorphological Association of Korea
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• v.23 no.1
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• pp.77-85
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• 2016

To understand the difference of runoff discharge processes between Gwangneung deciduous and coniferous forest catchments, we collected hydrological data (e.g., precipitation, soil moisture, runoff discharge) and conducted hydrochemical analyses in the deciduous and coniferous forest catchments in Gwangneung National Arboretum in the northwest part of South Korea. Based on the end-member mixing analysis of the three storm events during the summer monsoon in 2005, the hillslope runoff in the deciduous forest catchment was higher 20% than the coniferousforest catchment during the firststorm event. Howerver, hillslope runoff increased from the second storm event in the coniferous catchment. We conclude that low soil water contents and topographical gradient characteristics highly influence runoff in the coniferous forest catchment during the first storm events. In general, coniferous forests are shown high interception loss and low soil moisture compared to the deciduous forests. It may also be more likely to be a reduction in soil porosity development when artificial coniferous forests reduced soil biodiversity. The forest soil porosity is an important indicator to determine the water recharge of the forest. Therefore, in order to secure the water resources, it should be managed coniferous forests for improving soil biodiversity and porosity.

• Proceedings of the Korea Water Resources Association Conference
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• 2022.05a
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• pp.474-474
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• 2022

미세플라스틱이 물 환경으로 배출되는 주요 경로로는 하수처리장 방류수와 강우유출수가 있다. 하수처리장 및 유역에서 배출된 미세플라스틱은 하천과 하구역을 거쳐 해양과 같은 대규모 수역으로 이동하는데, 이 과정에서 해양뿐만 아니라 담수호, 저수지 등과 같은 공공수역에도 미세플라스틱이 지속적으로 축적되고 있다. 특히 강우유출수에 포함된 미세플라스틱은 적절한 처리 과정 없이 하천으로 유입되는 경우가 많아 공공수역 내 미세플라스틱 저감 기술의 필요성이 증가하고 있다. 그러나 미세플라스틱 관련 기존 연구는 미세플라스틱의 분포 등 현황에 대한 모니터링 및 환경위해성과 관련한 것이 대부분이며, 미세플라스틱 저감기술 관련 연구 또한 일부 정수처리 및 하수처리 공정을 대상으로 하는 초기 단계의 연구가 진행되고 있을 뿐 공공수역에서의 미세플라스틱 저감기술 개발 관련 연구는 전무한 실정이다. 따라서, 본 연구에서는 기존의 물리·화학적 수처리 공정인 용존공기부상법(Dissolved Air Flotation, DAF)에 물의 전기분해 시발생하는 브라운가스를 활용하여 응집된 물질을 빠르게 부상시켜 수체 내 오염물질을 제거할 수 있는 기술을 통해 수체 내 미세플라스틱 저감효과를 분석하였다. 또한, 해당 기술을 공공수역인 저수지에 적용하여 오염물질과 함께 미세플라스틱을 제거할 수 있는지 검토하였다.

• KSCE Journal of Civil and Environmental Engineering Research
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• v.39 no.6
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• pp.877-886
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• 2019

The size of the subway entrance should be calculated according to the user's demand, but Korea has the same size for each entrance by applying a uniform value. Recently, the installation of mobile convenience facilities such as escalators, elevators, etc. is mandated by the traffic weakness promotion law, but it is inconvenient to use the existing stations because it is mainly arranged in the place where it can be installed regardless of user demand. This study aims to establish a model for estimating the size of mobile convenience facilities by predicting the use demand of each station entrance so that the location and size of mobile facilities can be reflected in the design or construction of the station. To this end, a multiple regression model was established to forecast daily demand by utilizing the demand for getting on and off by station and the building association area for each purpose around the railway station. The actual data of Dongdaemun and Jonggak Stations were used to verify the estimated model. In addition, the escalator installation scale was compared / analyzed by doorway using domestic and overseas escalator equations. As a result, it was more accurate to estimate the usage demand for a single station. Also, Jonggak Station has an up and down escalator installed at exit 1, but it was analyzed that it is appropriate to install at exit 4. This study is an advanced form of the essay model for estimating the users of the entrance and exit users of urban railway stations published in 2018. In addition, it seems to be the basis of the current escalator installation criteria.

• Proceedings of the Korea Water Resources Association Conference
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• 2007.05a
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• pp.89-96
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• 2007

농업 비점오염원으로부터의 수질 보전이나 수자원 관리는 유역단위로 하는 것이 세계적 추세이며, 지형이 복잡한 우리나라에서는 더욱 효율적일 수 있다. 유역은 물이나 기타 물질들이 모여 강이나 더 큰 수계로 흘러드는 지표수의 범위라 표현할 수 있으며 그 범위를 정함에 따라 매우 중요한 의미를 지니게 된다. 특히, 강우에 따른 수자원의 유입과 유출이 토양을 통해 발생함에도 불구하고 기존의 유역단위 구분이 토양의 특성을 전혀 반영하지 못하고 있는 우리의 현실은 효율적 관리를 위한 유역단위 구분의 큰 단점으로 작용해왔다. 따라서, 농업적 관리뿐만 아니라 수질관리 및 수자원 관리를 위해서도 유역단위 특히, 소유역을 토양특성이 포괄하는 체계적 단위로 분류할 필요성이 있다. 토양학에서는 동일한 모재에서 유래된 일련의 토양이 미세지형에 따라 연속적으로 분포된 것을 Soil Catena(토양연접군)라고 한다. 이 토양연접군을 위주로 토양을 분류하게 되면 수문이나 기상현상 등의 주요 매질인 토양을 그룹화할 수 있는 가능성을 얻게 되고 이런 그룹화는 유역을 수계 위주의 유역군이 아닌 동일특성이나 유사특성을 나타낼 수 있는 유역군으로 분류가 가능하도록 유도할 것이므로, 이런 분류는 토양을 포함하는 다양한 수문모형의 적용성을 확대해 합리적 수자원 관리에 도움이 될 것이며 수자원 환경에 영향을 미치는 오염물질 관리에 대한 유역단위 보편성을 확보하고 농업에서의 최적관리를 가능하게 할 것이다. 우리나라 유역 세분화는 토양조사가 되어 있는 지역에만 한정해 분류에 이용했다. 대유역은 15개로 구분하였으며(그림 1), 중유역은 117개 소유역은 1,108개를 분석에 사용했다. 유역의 만곡도(하천의 실제길이 하천의 직선장) 산림의 비율(표준유역내 임지토양의 면적 / 소유역의 면적), 평탄지의 비율(표준유역내 평탄지의 비율 / 소유역의 면적), 다른 소유역으로부터의 유입이 있는지의 여부 등을 기본자료로 하였다. 이렇게 구분된 소유역은 유형적으로 보면 유사한 지형 및 토양특성에 따라 그룹화하였다. 유역내 평탄지가 유역면적의 25% 이상을 차지하는 지역을 평야지로 구분하며, 유역내 평탄지가 25% 미만이고 경사지가 45% 이상인 중간지, 유역내 평탄지가 25% 미만이고, 경사지가 45% 미만인 곳을 산간지로 구분하였다. 경사지는 산악지와 구릉지를 제외하여 모든 소유역을 모암 유래토양특성에 따라 16유형, 농업지대에 따라 3개의 유형으로 나눌 수 있으며 총 개의 유형으로 분류하였다. 이런 분류의 토대위에 향후 필요분야마다 구분이 가능한 기후특성을 포함시킨다면 최종적으로는 모든 것이 해설될 수 있는 유역군으로 만들 수 있을 것이다. 즉, 토양특징, 농업특징, 기후특징에 비점오염가능성 등 토지이용상 문제점등을 포괄한다면 다양한 자연현상을 기술할 수 있는 효과적인 유역군이 될 것이다.

• Korean Journal of Ecology and Environment
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• v.41 no.2
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• pp.206-215
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• 2008

Temporal and spatial distributions of salinity, temperature, dissolved oxygen (DO), and turbidity were investigated at seven sites in the upper regions of brackish Lake Sihwa with a limited water exchange, from March to October 2005. During the study period, salinity and temperature varied $0.1{\sim}29.9\;psu$ and $4.7{\sim}28.1^{\circ}C$, respectively, depending on seasons and sites sampled. A distinct halocline profile showing the maximum density gradient (difference over $20\;psu\;m^{-1}$ between surface and bottom layers) was observed during the rainy season, due to the decrease of salinity in surface layers by freshwater inflow. This result implies that rainfall event is the important factor forming the halocline. On the other hand, the depth and location of haloeline varied with the amount of seawater through the sluice gates and the operation systems (inflow or outflow). High DO (over 300% saturation) was observed at surface layer above the halocline in April when red tide occurred, whereas low DO (below 20% saturation) was at the bottom layer below the halocline in the rainy season. Turbidity ranged $1.5{\sim}80.3\;NTU$ showing the maximum turbidity at the layers above or upper the halocline. As a result, the distributions of DO and turbidity in the upper regions of brackish Lake Sihwa were largely affected by the variation of salinity. Also, when the halocline was formed, the water quality between upper and lower water layers may be expected completely different. This study suggests that the physicochemical characteristics of water in the brackish regions are closely associated with the causes of eutrophication such as red tide and DO deficit.

• Proceedings of the Korea Water Resources Association Conference
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• 2008.05a
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• pp.102-106
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• 2008

This study is to evaluated the impact of varying spatial resolutions of DEM (2 m, 10 m, and 30 m), land use (QuickBird, 1/25,000 and Landsat), and soil data (1/25,000 and 1/50,000) on the uncertainty of Soil and Water Assessment Tool (SWAT) predicted streamflow, sediment, T-N, and T-P transport in a small agricultural watershed ($1.21\;km^2$). SWAT model was adopted and the model was calibrated for a $255.4\;km^2$ watershed using 30 m DEM, Landsat land use, and 1/25,000 soil data. The model was run with the combination of three DEM, land use, and soil map respectively. The SWAT model was calibrated for 2 years (1999-2000) using daily streamflow and monthly water quality (SS, T-N, T-P) records from 1999 to 2000, and verified for another 2 years (2001-2002). The average Nash and Sutcliffe model efficiency was 0.59 for streamflow and the root mean square error were 2.08, 4.30 and 0.70 tons/yr for sediment, T-N and T-P respectively. The hydrological results showed that output uncertainty was biggest by spatial resolution of land use. Streamflow increase the watershed average CN value of QucikBird land use was 0.4 and 1.8 higher than those of 1/25,000 and Landsat land use caused increase of streamflow.