• 제목/요약/키워드: river model

검색결과 2,740건 처리시간 0.031초

1차원수리모형-분포형 연계모형을 이용한 수질오염사고 분석 (Pollution accident analysis using a hybrid hydrologic-hydraulic model(K-River & K-DRUM))

  • 이용현;안현욱;안정민;허영택
    • 한국수자원학회:학술대회논문집
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    • 한국수자원학회 2023년도 학술발표회
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    • pp.472-472
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    • 2023
  • 본 연구에서는 낙동강 수계에서 발생한 수질오염사고에 대해 K-River와 K-DRUM 결합모형을 이용하여 오염물질의 이동을 분석하였다. 국내에서는 수질오염총량제 도입 이후 수질관리에서 물순환과정을 수용한 배분모델의 필요성과 비점오염원의 중요성이 강조되었다. 따라서 비점오염원의 유출특성을 반영하기 위해 유역의 오염도를 분석할 수 있는 K-DRUM 분포모형을 사용하였다. 그리고 낙동강 수계에서 운영되는 댐 운영규칙을 적용하여 모델의 재현성을 높였다. 또한 하천 내 오염물질의 이동을 분석하기 위해 대류-분산 방정식의 대류 부분만을 1차원 수리모델 K-River에 적용하여 오염물질 추적을 수행하였다. 수질오염 분석 결과 오염물질의 최고농도는 과소평가 되었으나 도착시간과 전체 오염물질 농도의 추이는 잘 재현되었다.

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하천폭의 국부적 축소 및 확대에 따른 수리특성 연구 (A Study of the Stream Specific by River Width's Downsizing & Extension)

  • 최한규;김주석;백효선
    • 산업기술연구
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    • 제27권B호
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    • pp.229-233
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    • 2007
  • This research investigated the way of generating the flowing of water in case of artificial fluctuation of river width by the unidimensional numerical analysis in order to reconstruct vertical and expanse features of flowing, and the problem of existing numerical analysis in accordance with local enlargement and reduction of river through hydraulic model experiments with results of numerical analysis. The result revealed that when the local section change in the same river is exist, it showed 0.93m in the case of no change of local section in the hydraulic model experiments and numerical analysis, however, it presented 1.645m on the occasion of local section changes in the hydraulic model experiments and numerical analysis. In other words, there was a significant difference in the existing numerical analysis, when there was a local section change. As a result of the experimental section for the enlargement and reduction of local river width, due to the sensitive change for fluctuation of flood discharge, there was a significant difference between numerical analysis and hydraulic model experiments. In addition, the result of comparison between the enlargement and reduction of local river width confirmed that the result of numerical analysis with hydraulic model experiments showed larger generation of deviation in case of enlargement of section than in case of reduction of section.

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NUMERICAL MODELLING OF SEDIMENT TRANSPORT IN CONNECTION WITH ARTIFICIAL GRAIN FEEDING ACTIVITIES IN THE RIVER RHINE

  • Duc Bui Minh;Wenka Thomas
    • Water Engineering Research
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    • 제6권1호
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    • pp.17-30
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    • 2005
  • The bed evolution of the stretch of the River Rhine between km-812.5 and km-821.5 is characterised by general bed degradation as a result of the river training works and dredging activities of the last two centuries. The degradation of the river bed affects the water levels, and so the navigation conditions. To combat the erosion of the river bed with the aim to keep up the shipping traffic and to avoid the ecological system damages due to water level reductions, sand-gravel-mixtures were added to the river (so called artificial grain feeding activities). This paper presents the results of an application of a graded sediment transport model in order to study morpholodynamical characteristics due to artificial grain feeding activities in the river stretch. The finite element code TELEMAC2D was used for flow calculation by solving the 2D shallow water equation on non-structured grids. The sediment transport module SISYPHE has been developed for graded sediment transport using a multiple layer model. The needs to apply such graded sediment transport approaches to study morphological processes in the domain are discussed. The calculations have been carried out for the case of middle water flow and different size-fraction distributions. The results show that the grain feeding process could be well simulated by the model.

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Soil Loss Vulnerability Assessment in the Mekong River Basin

  • Thuy, Hoang Thu;Lee, Giha
    • 한국지반환경공학회 논문집
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    • 제18권1호
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    • pp.37-47
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    • 2017
  • The Mekong River plays an extremely important role in Southeast Asia. Flowing through six countries, including China, Myanmar, Thailand, Laos PDR, Cambodia, and Vietnam, it is a site of great biological and ecological diversity and the habitat of numerous species of fish. It also supports a very large population that lives along the river basin. Therefore, much attention has been focused on the giant Mekong River Basin, particularly, its soil erosion and sedimentation problems. In fact, many methods have been used to calculate and simulate these problems. However, in the case of the Mekong River Basin, the available data is limited because of the extreme size of the area (about $795,000km^2$) and lack of equipment systems in the countries through which the Mekong River flows. In this study, we applied the Universal Soil Loss Equation (USLE) model in a GIS (Geographic Information System) framework to calculate the amount of soil erosion and sediment load during the selected period, from 1951 to 2007. The result points out dangerous areas, such as the Upper Mekong River Basin and 3S Basin (containing the Sekong, Sesan, and Srepok Rivers) that are suffering the serious consequences of soil erosion problems. Moreover, the present model is also useful for supporting river basin management in the implementation of sustainable management practices in the Mekong River Basin and other basins.

한강 수계에서의 다차원 시변화 수리.수온 모델 연구 (Multidimensional Hydrodynamic and Water Temperature Modeling of Han River System)

  • 김은정;박석순
    • 한국물환경학회지
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    • 제28권6호
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    • pp.866-881
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    • 2012
  • Han River is a complex water system consisting of many lakes. The water quality of Lake Paldang is significantly affected by incoming flows, which are the South and North branches of the Han River, and the Kyungan Stream. In order to manage the water quality of the Lake Paldang, we should consider the entire water body where the incoming flows are included. The objectives of this study are to develop an integrated river and lake modeling system for Han River system using a multidimensional dynamic model and evaluate the model's performance against field measurement data. The integrated model was calibrated and verified using field measurement data obtained in 2007 and 2008. The model showed satisfactory performance in predicting temporal variations of water level, flow rate and temperature. The Root Mean Square Error (RMSE) for water temperature simulation were $0.88{\sim}2.13^{\circ}C$ (calibration period) and $1.05{\sim}2.00^{\circ}C$ (verification period) respectively. And Nash-Sutcliffe Efficiency (NSE) for water temperature simulation were 1089~0.98 (calibration period) and 0.90~0.98 (verification period). Utilizing the validated model, we analyzed the spatial and temporal distributions of temperature within Han River system. The variations of temperature along the river reaches and vertical thermal profiles for each lakes were effectively simulated with developed model. The suggested modeling system can be effectively used for integrated water quality management of water system consisting of many rivers and lakes.

Modeling flood and inundation in the lower ha thanh river system, Binh dinh province, vietnam

  • Don, N. Cao;Hang, N.T. Minh
    • 한국수자원학회:학술대회논문집
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    • 한국수자원학회 2016년도 학술발표회
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    • pp.195-195
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    • 2016
  • Kon - Ha Thanh River basin is the largest and the most important river basin in Binh Dinh, a province in the South Central Coast of Vietnam. In the lower rivers, frequent flooding and inundation caused by heavy rains, upstream flood and or uncontrolled flood released from upstream reservoirs, are very serious, causing damage to agriculture, socio-economic activity, human livelihood, property and lives. The damage is expected to increase in the future as a result of climate change. An advanced flood warning system could provide achievable non-structural measures for reducing such damages. In this study, we applied a modelling system which intergrates a 1-D river flow model and a 2-D surface flow model for simulating hydrodynamic flows in the river system and floodplain inundation. In the model, exchange of flows between the river and surface floodplain is calculated through established links, which determine the overflow from river nodes to surface grids or vice versa. These occur due to overtopping or failure of the levee when water height surpasses levee height. A GIS based comprehensive raster database of different spatial data layers was prepared and used in the model that incorporated detailed information about urban terrain features like embankments, roads, bridges, culverts, etc. in the simulation. The model calibration and validation were made using observed data in some gauging stations and flood extents in the floodplain. This research serves as an example how advanced modelling combined with GIS data can be used to support the development of efficient strategies for flood emergency and evacuation but also for designing flood mitigation measures.

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홍수범람모의를 위한 내외수 연계모형 개발 (Development of a Combined Model for Flood Inundation Simulation)

  • 유재홍;김형준;조용식
    • 한국방재학회 논문집
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    • 제5권4호
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    • pp.1-8
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    • 2005
  • 본 연구에서는 홍수범람을 모의하기 위하여 하천모형과 우수관망모형을 결합하였다. 하천의 범람을 모의하는 하천모형은 2차원 Saint Venant 방정식을 유한차분기법으로 차분화하여 수치모형을 구성하였다. ILLUDAS를 기반으로 하는 우수관망모형은 관망의 통수능과 홍수량을 비교하여 제내지에서의 침수현상을 해석한다. 내외수연계모형을 실제 홍수범람사상에 적용하여 제내지와 제외지에서 일어나는 홍수범람현상을 적절히 모의함을 확인할 수 있었다.

한강 하류부 흐름해석을 위한 수리학적 모형의 구축 (Establishment of Hydraulic Model for flow Analysis of the Lower Han River)

  • 김상호;김원
    • 한국수자원학회논문집
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    • 제35권5호
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    • pp.485-500
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    • 2002
  • 본 연구에서는 한강 하류부 및 임진강에서 하천구조물, 조위, 주요 지류 등으로 인해 복잡하게 형성되는 흐름을 해석하기 위한 수리학적 홍수추적모형을 구축하였다. 이를 위해 하천측량 자료를 모형에서 자동적으로 처리할 수 있는 DWOPER-2K 모형을 개발하였다. 감조지역에서 이루어진 실측 조위자료와 최근의 하천측량성과를 이용하여 모형을 구축하였고 잠실수중보와 신곡수중보에서 발생하는 흐름을 효과적 모의할 수 있도록 하였으며 하천구간별 유량규모별로 조도계수를 최적화시켰다. 개발된 모형의 검증결과 한강 및 임진강 하류부에서 복잡하게 발생하는 여러 가지 형태의 흐름을 효과적으로 해석할 수 있는 것으로 나타나 홍수예경보 정확도 향상, 하천관리 등에 효율적으로 사용될 것으로 기대된다.

유전알고리즘을 이용한 하천수질관리모형에 관한 연구 (A Study on the River Water Quality Management Model using Genetic Algorithm)

  • 조재현;성기석
    • 상하수도학회지
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    • 제18권4호
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    • pp.453-460
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    • 2004
  • The objective of this research is to develop the water quality management model to achieve the water quality goal and the minimization of the waste load abatement cost. Most of existing water quality management model can calculate BOD and DO. In addition to those variables, N and P are included in the management model of this study. With a genetic algorithm, calculation results from the mathematical water quality model can be used directly in this management model. Developed management model using genetic algorithm was applicated for the Youngsan River basin. To verify the management model, water quality and pollution source of the Youngsan River had been investigated. Treatment types and optimum treatment costs of the existing and planned WWTPs in the baisn were calculated from the model. The results of genetic algorithm indicate that Kwangju and Naju WWTP have to do the advanced treatment to achieve the water quality goal about BOD, DO and TP. Total annual treatment cost including the upgrade cost of existing WWTPs in the Youngsan River basin was about 50.3 billion Won.

지형공간 특성자료를 이용한 하천유역의 강우-유출해석 (Rainfall-Runoff Analysis of River Basin Using Spatial Data)

  • 안승섭;이증석;도준현
    • 한국환경과학회지
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    • 제12권9호
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    • pp.949-955
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    • 2003
  • The subject basin of the research was the basin of Yeongcheon Dam located in the upper reaches of the Kumho River. The parameters of the model were derived from the results of abstracting topological properties out of rainfall-runoff observation data about heavy rains and Digital Elevation Modeling(DEM) materials. This research aimed at suggesting the applicability of the CELLMOD Model, a distribution-type model, in interpreting runoff based on the topological properties of a river basin, by carrying out runoff interpretation far heavy rains using the model. To examine the applicability of the model, the calculated peaking characteristics in the hydrograph was analyzed in comparison with observed values and interpretation results by the Clark Model. According to the result of analysis using the CELLMOD Model proposed in the present research for interpreting the rainfall-runoff process, the model reduced the physical uncertainty in the rainfall-runoff process, and consequently, generated improved results in forecasting river runoff. Therefore it was concluded that the algorithm is appropriate for interpreting rainfall-runoff in river basins. However, to enhance accuracy in interpreting rainfall-runoff it is necessary to supplement heavy rain patterns in subject basins and to subdivide a basin into minor basins for analysis. In addition, it is necessary to apply the model to basins that have sufficient observation data, and to identify the correlation between model parameters and the basin characteristics(channel characteristics).