• Title/Summary/Keyword: River confluence

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Calculation of low flow for estimating TMDL (허용 부하량 산정을 위한 저수유량 산정 방안)

  • Jung, Yoon-Min;Kwon, Jae-Hyuk;Kang, Sang-Hyuk
    • Spatial Information Research
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    • v.17 no.2
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    • pp.223-239
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    • 2009
  • The low fow analysis for small-mid sized river basins is very difficult because of insufficient flow data or ungauged basins. The objective of this study is to suggest effective method of low flow using area function method for calculating Total Maximum Daily Loads (TMDL) by considering environmental carrying capacity. Two watersheds which are Juchon watershed having $606km^2$ areas and ungauged watershed having $4,551km^2$ areas were selected for this study. As a result of application, the low flow in the downstream of Juchon River and the Han River after confluence of Okdong River were $1.9m^3/s$ and $20.7m^3/s$, respectively. Then we consider the target BOD of 1.0-1.2mg/l in Youngwol prefecture, the TDML was estimated 164-197kg/day and 1,788-2,146kg/day, respectively. This approach will useful for estimating TDML to insufficient watershed of flow data and ungauged watershed of flow data.

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Prediction of River Bed Change due to Yongdam Dam Discharge (용담댐 방류에 따른 하상변동 예측)

  • Kim, Young-Bok;Jung, Seung-Kwon;Shim, Soon-Bo
    • Journal of the Korean Society of Hazard Mitigation
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    • v.6 no.1 s.20
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    • pp.69-81
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    • 2006
  • The purpose of this study is to identify the downstream influences due to the dam discharge by using 2-dimensional model, SMS(Surface water Modeling System). RMA-2 and SED-2D in SMS were applied to Yongdam multipurpose dam watershed located in Gum river basin. Through the simulation, erosion and deposit quantitative analysis of sinuous channels and scour pattern analysis of bridges have been done. A differences erosion depths between deposit are simulated as $-102.4 mm{\sim}54.2 mm$ at No.176(1.4 km) and $-104.1 mm{\sim}28.9 mm$ at No.146(7.4 km), sinuous channel. The river bed at Kamdong bridge in straight channal is simulated as uniform erosion. However, the river bed at Dumdul bridge in sinuous channal has been shown as different erosion depths at each sides. Consequently, the parts that could not be simulated on the existing 1-dimensional model, can be improved results by using a 2-dimensional model, about weakness points for hydraulic modeling such as extreme bend, tributary confluence.

Restoration of Iksan Imperial Capital City Structure and Construction Model in Late Baekje from the Point of Ancient Capital City Planning (백제 후기 익산도성 조영계획모델에 대한 도성계획사적 해석)

  • Lee, Kyung-Chan
    • Journal of architectural history
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    • v.24 no.3
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    • pp.31-41
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    • 2015
  • This study aims to draw out planning principles and structure of Iksan imperial capital city in late Baekje, especially in view of the relationship among imperial capital city planning area, skeletal axis and the location of royal castle. With site survey and analysis of historical records, old maps, topographical maps, archeological excavation data, land registration map of 1915, some significant inferences were drawn out. Firstly from the point of topological conditions, the contiguous line of a stratum from Mireuk mountain(彌勒山) to Wangkung-ri castle(王宮里遺蹟) and two waterways made a topological axis of Iksan Imperial capital city. Secondly district of Iksan imperial capital city can be deduced to the inner area north to Kummado soil wall(金馬都土城), south to the confluence of Iksan river(益山川) and Busang river(扶桑川), west to Okum mountain fortress(五金山城) and Galjeon river(葛田川), east to line near to eastern wall of Jesuksa temple(帝釋寺). Iksan ssang-reung(益山雙陵) was located outside western boundary line of capital city. Thirdly axis from Wangkung-ri castle to northern Kummado soil wall made a skeletal axis of city structure. It got through northern lowland along Buk river(北川) between Yonghwa(龍華山) and Mireuk mountain. Fourthly the location of royal palace can be deduced to the north part of the city around Kumma town area along the planning principle of northern royal palace.

A Monte Carlo Simulation and 1D Hydraulic Model-Based Approach for Estimating River Discharge at the Confluence using Artificial Multi-Segmented Rating Curves (K-RIVER와 Monte Carlo 방법을 이용한 홍수기 간접유량 추정 기법)

  • 강한솔;김연수;노준우;허영택;변지선;안현욱
    • Proceedings of the Korea Water Resources Association Conference
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    • 2023.05a
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    • pp.483-483
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    • 2023
  • 2020년 8월 섬진강 유역에서 100년 빈도 이상의 대홍수가 발생함에 따라 제방이 붕괴되거나 하천 범람이 발생하는 피해가 발생하였다. 8월 홍수를 대상으로 섬진강 본류 남원(신덕리) 수위국에서 기존의 수위-유량 관계 곡선식(이하 Rating curve)의 최대 적용 가능 수위는 2.53m 이지만, 해당 기간 첨두 수위는 10m 이상을 기록하였다. 이러한 대홍수의 경우 기왕의 관측데이터가 없을 뿐만 아니라 기존의 Rating curve를 외삽하여 활용하는 것에도 한계가 있어 간접적으로 유량을 산정할 수 있는 기법이 필요하다. 본 연구에서는 이와 같이 유량측정이 어려운 지점을 대상으로 주어진 유량에 대하여 수위를 재현할 수 있는 K-water에서 개발된 K-River모형(1차원 하천수리해석모형)과 Monte Carlo 시뮬레이션 기법을 활용하여 간접적으로 유량을 산정할 수 있는 기법을 개발하였다. 개발된 방법론은 고수위 구간에 대한 Rating curve의 불확실성으로 인하여 본류와 지류의 유입량 추정이 어려웠던 섬진강 요천 합류부에 적용하였다. 대상구간은 본류(섬진강) 26km 및 지류(요천) 15km로 구성되어 있으며, 본류와 지류의 상류인 수위국 남원(신덕리) 관측소와 남원(동림교) 관측소에는 각각 기존의 Rating curve가 존재한다. 불확실성이 높은 Rating curve의 고수위 구간에 대한 매개변수를 조정하여 다수의 Rating curve를 생성하고, 이를 기반으로 관측수위를 다수의 상류 시계열 유량자료(경계조건)로 환산하였다. 다음으로 이 유량자료를 기반으로 앙상블 모의를 수행 후 대상구간의 중간지점에 위치한 수위국(고달(고달교) 관측소, 송동(요천대교) 관측소, 곡성(금곡교) 관측소)에서 수위재현성(NSE, RSR등 활용)을 평가하여 최적 샘플 추출을 추출하였다. 추출된 샘플로부터 상류 경계지점의 적정 Rating curve 선정과 각 지점에서의 시계열 수위 및 유량을 역으로 추정하였다. 이를 통해 실제 유량측정결과 없이도 간접적으로 신뢰도 높은 유량 자료를 확보할 수 있음을 확인할 수 있었으며, 향후 수자원의 효율적 관리 및 홍수관리를 위하여 효율적으로 활용이 가능할 것으로 생각된다.

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Estimation of Sediment Transport and Long-term Prediction of Riverbed Elevation Changes in Yangon River (양곤강 퇴적물 이동 및 장기 하상변화율 측정)

  • Htet, Salaing Shine;Chang, Yeon S.
    • Journal of Korean Society of Coastal and Ocean Engineers
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    • v.31 no.6
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    • pp.450-457
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    • 2019
  • Sedimentation is a common problem for river ports. But its intensity depends on the rate of sedimentation, channel shape and size, hydrodynamic behavior of the river and the importance of the port. High sedimentation rate in Yangon River has become one major issue for Myanmar as her largest port is located on the Yangon riverbank. As a result of the high sedimentation rate, shallow water area near the confluence of Yangon River, Pazundaung Creek, and Bago River keeps blocking the navigation channel to the Yangon Port, which also limits the size of vessel calling to Yangon Port. Therefore, studies to understand sediment transport process in Yangon River are required because the economic development of Myanmar highly relies on the Yangon Port. This paper aims to calculate the sediment transport and to predict the riverbed elevation changes in Yangon River by using Bagnold (1966) theory. Calculation result shows that huge difference can be found in the bed load transport between the rainy season and dry season in Yangon River, and thus the sedimentation problem would become more severe in the dry season when the transported sediments are reduced. The estimated sedimentation rate in dry season indicates that the rate of riverbed level rise near the Yangon Port area is about 0.063 m per year, which would lead to approximately 3.15 m rise in the riverbed level in next 50 yrs, considering the same workload of dredging to maintain the navigation channel.

Analysis of the Effectiveness of Nature-based Solutions for River Flood Level Reduction (하천 홍수위 저감을 위한 자연기반해법의 적용효과 분석)

  • Hoyong Lee;Minseok Kim;Junhyeong Lee;Taewoo Lee;Hung Soo Kim;Soojun Kim
    • Journal of Wetlands Research
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    • v.25 no.4
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    • pp.379-385
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    • 2023
  • EDue to climate change and urbanization, the localized heavy rainfall frequently exceeded a design storm rainfall and flood damage has occurred in South Korea. The concept of addressing sustainable river management and environmental and social issues through Nature-based Solutions (NbS) is gaining attention as it seeks to resolve these issues through ecosystem services. Therefore, in this study, the flood reduction effect by river management using NbS was quantitatively analyzed for the Hwang River, which is directly downstream of Hapcheon Dam, South Korea. Floodplain excavation and dyke relocation, which are methods of the NbS, were applied to the flood risk area of the Hwang River. As a result of analyzing the flood level of the river through the unsteady flow analysis of HEC-RAS, we obtained flood level reduction by 8 cm at the confluence of the Nakdong River. The results of this study can be expected to be sufficiently utilized as a basis for use as a management plan through NbS rather than the river management with grey infrastructure.

Evaluation of Optimal Grid Resolution for Hydrodynamic Proper Simulation (수리동역학적 모의를 위한 적정 격자해상도 산정방법)

  • Ahn, Jung-Min;Park, In-Hyeok;Lyu, Si-Wan;Hur, Young-Teck
    • Journal of Korean Society for Geospatial Information Science
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    • v.20 no.1
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    • pp.109-116
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    • 2012
  • The effect of the grid resolution on the hydrodynamic simulation has been investigated by using CCHE2D and EFDC. Since a high resolution of the grid results in the increase of computation time, an appropriate grid resolution should be selected by considering the efficiency of simulation according to the objectives of projects. In order to understand the effect of grid resolution and determine the optimal grid resolution, several cases with different lateral grid resolutions have been simulated for the reach of Nakdong river at the confluence of Kumho river for the floods in 2006. Orthogonal curvilinear grids for the domain have been constructed from the survey products at the sections with the longitudinal interval of 20 m. Area-elevation curve and the comparison of simulated results with measured stage at the specific station have been used to check the effect of grid resolution. From the results, the existence of optimal grid resolution has been observed, which ensure both efficiency of computation and certainty of results.

Simulation of Pollutants Transport using 2-D Advection-Dispersion Model near Intake Station (2차원 이송-확산모형을 이용한 취수장 인근에서의 오염물질의 혼합거동 모의)

  • Kim, Jae-Dong;Kim, Young-Do;Lyu, Si-Wan;Seo, Il-Won
    • 한국방재학회:학술대회논문집
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    • 2008.02a
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    • pp.791-794
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    • 2008
  • The transport and dispersion of pollutants in natural river is a principal issue in intake station management. To study the pollutant transport in natural rivers, the effect of meandering and confluence of tributary on mixing process have to analyzed. The objective of this study is to simulate the mixing and transport of pollutants for operating water gate of Nakdong Estuary Barrage around the intake station. Mulgeum intake station being used as drinking water sources for Pusan. The flow around the intake station is influenced by operating water gate of Nakdong Estuary Barrage which is located downstream. The water gate system includes ten individual gates. The minor gate is usually opened according to elevation of the sea. When the river flow increases, the main water gate is opened. Daepo stream, tributary of the Nakdong river, is on opposite side of the intake station. The pollutants from Daepo stream often flows into the intake station acoording to the flow pattern. In this study, based on this simulation results, proper water gate operation which can minimize negative impact will be provided.

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Distribution Characteristics of Quaternary Geology and Aggregate Resources in Geumsan-gun, Chungcheongnam-do (충청남도 금산군 일대 제4기 지질 및 골재자원 분포 특성)

  • Kim, Jin Cheul;Kim, Ju Yong;Lee, Jin-Young
    • Economic and Environmental Geology
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    • v.54 no.5
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    • pp.595-603
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    • 2021
  • Sand layer distribution, which is the main target of river and land aggregate resources, mainly belongs to alluvial and river sedimentary environments among the Quaternary sedimentary environments. The distribution of aggregate resources in the area of Geumsan-gun, Chungcheongnam-do is characteristically developed around a sedimentation environment in which intrusive meandering river dominate. Although the area around Bonhwangcheon Stream and the area near the confluence of small streams are small, the river floodplain develops and corresponds to the aggregate distribution area. The sedimentary layer formed in the sedimentary environment such as colluvial deposits or alluvial fan deposits has a relatively low distribution rate of aggregate resources. The vertical distribution of the Quaternary sedimentary layers in the Geumsan-gun region ranges from about 5 to 12 m and has an average Quaternary sedimentary thickness of 8 m. The aggregate-bearing section has an average thickness of 3.6 m, and the average grain size is about 21% clay-silt, 67% sand, and 12% gravel. The main characteristics of the aggregate-bearing section are that coarse-grained sand predominates, and gravel is sub-angular or sub-rounded, and the sorting is generally poor and has a massive form of deposits, and the soil colour ranges from dark grey to yellowish-brown. In Geumsan-gun, the most likely distribution area for aggregate development is the alluvial sedimentary and river sedimentary layers distributed along the current and former riverbeds of the main Geumgang River, Bonhwangcheon and small River tributaries.

A study on TOC monitoring and spatial distribution analysis using a spectrometer in rivers (하천에서의 분광측정기를 이용한 TOC 모니터링 및 공간분포 분석 연구)

  • Yoon, Soo Bin;Lee, Chang Hyun;Kim, Young Do
    • Journal of Korea Water Resources Association
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    • v.56 no.11
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    • pp.815-822
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    • 2023
  • Organic pollution is one of the most common forms of water contamination. Under the Water Quality Conservation Act, indicators for measuring organic substances include BOD, COD, and TOC. Analysis of BOD and COD is labor-intensive, and in the case of organic substances where biological decomposition is not feasible or toxic substances are present, the accuracy is often low. Therefore, the Ministry of Environment is shifting towards TOC-centric management. With advancements in sensor technology today, various parameters can be monitored using sensors. In this study, digital monitoring of river TOC using a spectrophotometer called Spectro::lyser V3 was conducted. Initially, experiments were carried out at the Andong River Experiment Center to assess the applicability of the measurement equipment. Subsequently, data collected at the confluence of the Nakdong River was analyzed for the spatial distribution of TOC using the Kriging technique. This research proposes the utilization of sensors for river TOC monitoring and spatial distribution analysis. Real-time monitoring of changes in river TOC concentration can serve as fundamental data for pollution monitoring and response. Sensor-based river monitoring offers advantages in terms of temporal resolution and real-time data acquisition. When various spatial information interpretation methods are applied, it is expected to contribute to diverse studies such as aquatic ecological health, river water source selection, and stratification analysis in the future.