• 한국수자원학회논문집
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• 제50권12호
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• pp.827-836
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• 2017

하도홍수추적 방법에서 많이 사용되고 있는 Muskingum 방법의 가장 중요한 매개변수는 저류상수와 가중인자이다. Muskingum 방법은 상류유입지점에서 하류 유출지점까지 측방유입량이 고려되지 않지만, 실제 유역에는 강우로 인하여 측방유입유량이 발생한다. 이로 인해 상하류 실측자료를 이용하여 저류상수 및 가중인자를 산정하는 것이 매우 어려운 상황이다. 이에 본 연구는 HEC-RAS 1차원 부정류 해석모형을 이용한 수리학적 홍수추적을 통해 측방유입유량이 제외된 상태에서의 하도에서 전파되는 유량을 산정하였고, 이를 이용하여 저류상수 및 가중인자를 산정하는 방법을 제시하였다. 이와 함께 저류상수가 유하시간과 관계있음을 감안하여 국내 하천기본계획 수립 시 사용되는 유하시간 경험 공식들을 저류상수로 적용한 결과를 비교 분석하였다. 마지막으로 유량이 고려된 유하시간 산정 식을 개발하고, 유입량의 변화에 맞춰 유하시간을 업데이트하여 모의를 수행하는 방법을 제시하였다. 유량을 고려한 유하시간을 저류상수로 적용한 경우, 유량의 상승 및 하강 과정, 첨두 유량, 그리고 첨두 시간에 대해서 잘 모의하는 것으로 분석되었다.

• 농업과학연구
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• 제37권3호
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• pp.481-490
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• 2010

Baekgog reservoir is located in Jincheon county, Chungbuk province, of which full water levels will be heightened from EL. 100.1 m to EL. 102.1 m, and total storages from 21.75 $Mm^3$ to 26.67 $Mm^3$. The simulation for reservoir inflow was conducted by DAWAST model. The annual average irrigation water was estimated to 33.19 $Mm^3$ supplied to 2,975 ha and the instream flows could be allocated with 0.14 mm/d from October to April with annual average of 2.52 $Mm^3$. The operation rule curve was drawn using inflow, irrigation, and instream flow requirements data. The reservoir water storage was simulated on a daily basis in case of both normal and withdrawal limit operation. In case of normal operation, the annual average irrigation water supply increased from 31.95 $Mm^3$ to 33.32 $Mm^3$, the instream water supply from 2.40 $Mm^3$ to 2.44 $Mm^3$, the water storages from 15.74 $Mm^3$ to 19.88 $Mm^3$, and the water supply reliability from 77.3 % to 81.6 %. In case of operation with withdrawal limit, the amount of instream water supply was 2.52 $Mm^3$ from reservoir regardless of the condition while the water storage increased from 16.77 $Mm^3$ to 20.65 $Mm^3$. The irrigation water supply capacity was appropriate for the case of normal operation with 2 m heightened condition. The present instream water supply capacity was 35,000 $m^3$/d (6.86 $Mm^3$/y) while 42,000 $m^3$/d (8.36 $Mm^3$/y) in 2 m heightened condition in case of withdrawal limit operation.

• 한국환경복원기술학회지
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• 제16권5호
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• pp.1-17
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• 2013

We researched the fauna restoration of 5 urban streams in Ulsan established as ecological streams by improving water quality and river environment. The fauna inhabitation were compared according to the conditions of geometrical feature such as river width, low-water channel width, ect and water quality, water volumn, inland and forceland. The Mugeo cheon has clearly shown the fauna restoration effects resulting from supplying sustainable maintenance water and wastewater treatments. In the Yaksa cheon, on the other hand, the restoration effects were low due to the inflow of wastewater and sledges in some part of stream ever though the improvement of water quality. The Yeocheon cheon was found to have disadvantage on the ecological inhabitations due to supplying the maintenance water with highly concentrated salinity. The fauna restoration effect of the Meongjeong cheon was low due to the inflow of wastewater to the down stream. Therefore by supplying the maintenance water and improving the connection to the Taehwa river at the estuary, better restoration effects could be observed. In the Cheokgwa cheon, which is almost a natural river, the ecological integrity of the fauna population has been maintained quite well. It was concluded that the project to transform urban streams into ecological streams should focus on not only keeping water volume and quality but also maintaining favorable conditions for the migration and settlement of animal species close to the natural state.

• 한국해양공학회지
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• 제18권6호
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• pp.22-28
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• 2004

A mathematical model has been developed to evaluate the capability of sea water exchanges under tidal and diffusive environments and has been verified through comparison with numerical experiments. From the mathematical analysis, this study presents the rates of sea water exchanges due to the tidal inflow and diffusion process. The port characteristic length $L_p$ is the most significant evaluation index.

• 한국수자원학회논문집
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• 제33권6호
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• pp.745-755
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• 2000

현재 우리나라에서 홍수조절 업무에 황용하고 있는 홍수관리시스템은 댐에서 조절이 불가능한 댐하류부 수문현상들을 고려하여 방류계획을 수립할 수 없으며, 예측 강우량에 의한 댐으로의 유출상황을 고려한 예비방류에 관한 지침이 마련되어 있지 않다. 따라서 본 연구에서는 댐의 제약조건 댐 상.하류의 유출상황을 고려하여 홍수기 댐을 운영 할 수 있는 모의기법에 의한 모형을 개발하였다. 개발된 모형(EV ROM이라 명명)은 댐에서 조절이 불가능한 댐하류 지류에 의한 하류 홍수제어 지점의 Cumulative Lateral Flow Hydrograph를 고려하여 방류계획을 수립한다. EV ROM에서는 댐하류 지역의 첨두홍수량 경감을 위하여 홍수제어지점의 수문곡선 상승부에서 예비방류를, 첨두부에서는 댐에 저류를 하였다가 수문곡선 하강부에 다시 방류를 수행하는 특징이 있다. EV ROM을 강우-유출모형에 결합하여 금강수계 대청댐을 중심으로 3개 홍수사상에 적용해 본 결과, 기존의 Rigid ROM이나 Technical ROM 보다 우수한 것으로 나타났다. 이는 본 연구에서 개발한 EV ROM이 댐 유역뿐만 아니라 댐하류 홍수제어지점의 수문상황을 동시에 고려하여 댐의 방류계열을 결정하기 때문이다. 따라서, 본 연구에서 개발된 EV ROM을 다양한 홍수사상에 적용, 예측강우량의 정확도 개선 및 프로그램의 보완이 이루어진다면, 현재보다 한차원 높아진 저수지운영을 기대 할 수 있을 것이다.

• 생태와환경
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• 제38권1호통권110호
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• pp.105-117
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• 2005

낙동강 수계의 최대 인공호인 안동댐 저수지에서 2002${\sim}$2004년 동안 홍수기의 수온성층 구조에 따른 고탁수의 유입특성과 시 ${\cdot}$ 공간적 변동을 조사하였다. 6월부터 수온성층이 형성되었으며 성층구조에 따라 유입 수괴의 이동경로가 결정되었고 고탁수의 유입에 의해 성층구조가 변하였다. 고탁수는 유입 시기와 수량에 관계없이 저수지 상류부에서는 심층류로 유입되었고 중류부에서 바닥으로부터 분리되어 중층 밀도류의 형태로 하류까지 이동하였다. 또한 중층 밀도류의 형성지점은 유입량과 시기에 따라 공간적으로 다소 차이가 있었다. 유입량에 의해 수온성층과 DO 분포가 변하였고, 시기에 따라 변수층에는 2개의 수온 급감층과 저산소층이 각각 존재하였다. 최하류까지 이동한 홍수량의 고탁수층은 상승류를 형성하여 수심 15 m 아래에서 최대 20 m 두께로 고탁수층을 형성하였다. 고탁수층은 저수지 바닥으로 침전되지 않았고 중층의 취수구를 통해 하류로 배출되었으며 가을 순환시기 이후 완전 소멸되었다.

• 상하수도학회지
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• 제26권2호
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• pp.177-189
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• 2012

Sediment load deposited in sewers and manholes reduces not only the capacity of pipes but also the efficiency of the whole sewer system. This causes the inundations of the low places and overflows at manholes, Moreover, sulfides and bad odor can occur due to deposited sediment with organic loads in manholes. Movements of sediment load in manholes are complicated depending on manhole size, location, inside structure, sediment load type, and time. Therefore, it is necessary to understand the movements of sediment load in manholes by experiments. In this study, experiments were implemented by a square manhole with straight path to measure deposited sedimentation quantity. The experimental apparatus was consisted of a high water tank, an upstream tank, test pipes, a sediment supplier, a manhole, and a downstream tank to measure the experimental discharge. The quantity of deposited sediment load was measured by different conditions, such as the inflow condition of sediment(continuous and certain period), the amount of inflow sediment, discharge, and the type of sediment. Jumoonjin sand(S=2.63, D50=0.55mm), general sand(GS, S=2.65, D50=1.83mm) and anthracite (S=1.45, D50=0.80mm) were employed for the experiment. The velocities in inflow pipe were 0.45 m/s, 0.67 m/s, and 0.9 m/s. Sediment load movement and sedimentation quantity in manhole were influenced by many factors such as velocity, shear stress, viscosity, amount of sediment, sediment size, and specific gravity. Suggested regression equations can estimated the quantity of deposited sediment in the straight path square manholes. The connoted equations that were evaluated through the experimental study have velocity range from 0.45 to 0.9m/sec. The study results illustrates that appropriation of design velocity ragne between 1.0 and 2.0m/sec could implement to maintain and manage manholes.

• 환경영향평가
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• 제19권3호
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• pp.215-222
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• 2010

This research aims to gain the result of assessment of inflow categorized by runoff path using DIROM (Daily Irrigation Reservoir Operation Model) for Baengnyeong-myeon reservior which was built for residents of Baengnyeong island to solve the shortage of drinking water and stable supply of domestic water. The simulation results of DIROM and actual hydrograph of the reservoir show very low correlation with geological characteristics. The simulation results by DIROM after adjusting with modified Tank III model which considers all outflow from Tank II model as interflow among 3 level tanks show good correlation of its regional runoff and inflow characteristics with $R^2$=0.9058. In the study area, diffluence of 37% of rain fall of the study year has been simulated, which shows low result compared to the average river runoff of national water resource. In addition, 34.5% of total inflow to the study reservoir is mainly interflow and baseflow among expected several channels.

• 대한토목학회논문집
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• 제5권1호
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• pp.91-100
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• 1985

본(本) 연구(硏究)는 한강유역(漢江流域) 댐군(群)의 비상사태하(非常事態下)(큰 홍수파(洪水波) 유하시(流下時))에서의 수문조작(水門操作) 기준설정(基準設定)에 관한 것으로 얻어진 결과(結果)는 다음과 같다. 1) 수문조작(水門操作)을 저수위(貯水位)와 유입량(流入量)으로 실시(實施)할 수 있게끔 6개 댐(화천(華川), 춘천(春川), 소양강(昭陽江), 의암(衣岩), 청평(淸平), 인당(人堂)댐)에 대해 수문조작(水門操作) 기준(基準)을 수식화(數式化)하였다. 2) 수문(水門)의 개방면적(開放面積), 유입량(流入量), 저수위(貯水位), 방류량(放流量) 간의 다중회귀분석(多重回歸分析)에 의해서 얻어진 식(式)으로 홍수추적(洪水追跡)을 실시한 결과 그 적용가능성(適用可能性)을 확인(確認)하였다. 3) 본(本) 연구(硏究)에서 얻어진 수문조작(水門操作) 기준(基準)과 홍수추적방법(洪水追跡方法)을 사용(使用)하여 비상사태하(非常事態下)(큰 홍수파(洪水波) 유하시(流下時))에서의 각 댐을 검토(檢討)한 바, 모두 안전(安全)하였으나, 소양강(昭陽江), 의암(衣岩), 청평(淸平)댐만은 저수지(貯水池) 초기방류수위(初期放流水位)를 미리 저하(低下)시킨 상태(狀態)에서 수문조작(水門操作)이 이루어져야 할 것이다.

• 한국농공학회지
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• 제35권1호
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• pp.50-58
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• 1993

The sedimentation patterns at a reservoir, important to the reservoir capacity curve were simulated using a depth averaged, two-dimensional sediment transport model, that is capable of depicting velocity distributions and sediment transportation. The Banweol reservoir, whose stage capacity relationships have been surveyed before and after the construction, was selected and the daily inflow rates and stages were simulated using a reservoir operation model(DI-ROM). The applicability of the transport model was tested from the comparisons of simulated sedimentation patterns to the surveyed results. The simulated inflow rates and water level fluctuations at the reservoir during twenty-one years from 1966 to 1986, showed that water levels exceeding 80 percent of the total capacity occurred for 70 percent of the periods and inflow rates less than 5000rn$^3$/day sustained for 54 percent of the spans. Dorminant flow directions were simulated from two streamflow inlets to the dam site. And simulated sediment concentrations were higher near the inlets and lower at the inside of the reservoir. Sediment was deposited heavily near the inlets, and portions of sediments were distributed along the flow paths within the reservoir. The comparisons between the simulation results and the surveyed depositions were partially matched. However, it was not possible to compare two results at the upper parts of the reservoir where dredging was carried out few times for the purpose of reservoir maintenance. This study demonstrates that sedimentation patterns within the reservoir are closely related to incoming sediment and flow rates, water level fluctuations, and flow circulation within the reservoir.