• 제목/요약/키워드: stream hydraulic characteristics

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하천구조 개선에 따른 어류 서식적합도와 물리적 교란의 상관분석 (A Correlation Analysis between Physical Disturbance and Fish Habitat Suitability before and after Channel Structure Rehabilitation)

  • 최흥식;이웅희
    • Ecology and Resilient Infrastructure
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    • 제2권1호
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    • pp.33-41
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    • 2015
  • 본 연구는 어류서식적합도 향상을 위해 유전자알고리즘을 이용한 하천의 구조개선 방안을 제시하였다. 하천구조 개선에 의한 수리특성의 변화에 따른 어류 서식적합도와 물리적 교란양상과의 상관특성을 분석하였다. 원주천의 하천 환경조사와 어류의 군집특성을 이용하여 수중 생태계를 대표할 수 있는 복원 목표어종으로 참갈겨니를 선택하였다. 참갈겨니의 서식적합지수를 사용한 서식적합도 분석은 PHABSIM 모형을 이용하였다. HEC-RAS를 이용한 수리특성 분석과 하천교란 평가방법을 이용하여 물리적 교란평가를 수행하였다. 서식적합도 향상을 위한 최적의 저수로 폭의 개선방안을 제시하였다. 하천구조의 개선에 의한 수리특성의 변화에 따른 서식적합도와 물리적 교란의 상관성을 분석하여 어류 서식적합도와 물리적 교란 평가점수의 향상이 있음을 확인하였다. 서식적합도 향상을 위한 하천의 구조 개선은 물리적 교란의 평가점수의 향상을 가져옴을 확인하였다.

중소유역의 수문학적 특성이 하천유사량에 미치는 영향 (The Effects of Hydrologic Characteristics on Sediment Discharge in Streams with Small and Medium Size Watersheds)

  • 김활곤;서승덕
    • 한국농공학회지
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    • 제38권3호
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    • pp.127-136
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    • 1996
  • The purpose of this study is to provide with information for the water resources development and management in stream management planning, such as information on the sediment trensport, design of dam and water facilities, river improvement and flood plains management. The major results obtained from the field measurement and analysis of the watershed characteristics, hydraulic and sediment characteristics are as follows ; 1. The rating curve formulas obtained from the analysis of the hydraulic characteristics data collected are ; Q-=110.563 $(H-0.474)^2$ for 0.7m$(H-0.146)^2$ for 0.4m$Sr=aX{^2} {_1} X^{c}{_2}$, in the experimental watershed.

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도시하천의 부분복개화에 의한 하천수리특성치의 변화 (Changes of Fluvial Hydraulic Characteristics due to the Semi-Convering Work of Urban Stream)

  • 장인수
    • 한국산업융합학회 논문집
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    • 제2권1호
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    • pp.35-43
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    • 1999
  • The purpose of this study is to derive the optimal methodology estimating the changes of fluvial hydraulic characteristics due to semi-covering work of urban stream. First, after collecting the data of the daily maximum rainfall of Chungju gaging station, the frequency analysis was carried out with frequency factor method, which includes normal, two-parameter and three-parameter lognormal, Gumbel-Chow, pearson type III, log-pearson type III distribution, and the goodness of fit test was executed by $x^2$-test and Kormogorov-Smimov test. Using the SCS method, the effective rainfall was estimated and the peak flow was calculated by the area-routing method. The HEC-2 model was applied to calculate water surface profiles for steady, gradually varied flow at Kyohyun river system in Chungju city. The model was applied to floodplain and riverbed management to evaluate flood way encroachments and to delineate flood hazard by riverside roadway construction. The model also was used to evaluate effects on water surface profiles of river improvement and levees as well as the presence of bridges or other hydraulic structures in the floodplain.

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Groove 단면형상에 따른 유압 Spool Valve의 윤활해석 (Lubrication Analysis of Hydraulic Spool Valve with Groove Cross Sectional Shapes)

  • 박태조;황윤건
    • Tribology and Lubricants
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    • 제25권1호
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    • pp.13-19
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    • 2009
  • The spools in most hydraulic spool type control valve have several circumferential grooves to pre-vent well known hydraulic locking problems which result in high friction force and excessive wear. In this paper, a commercial computational fluid dynamics (CFD) code, FLUENT is used to investigate the flow and lubrication characteristics of grooved hydraulic spool valve. The stream lines and pressure distributions are obtained for various groove cross sectional shapes and film thicknesses. The stream lines are highly affected by groove cross sectional shape but pressure distributions mainly depend on the film shape and its magnitude. Therefore the numerical method adopted in this paper and results can be use in designing of various grooved spool valve.

유역(流域)의 하천형태학적(河川形態學的) 특성(特性)과 수리기하학적(水理幾何學的) 특성(特性)과의 상관성(相關性) (Correlations between the Stream Morphological Characteristics and the Hydraulic Geometry Characteristics for the Basin)

  • 안상진;윤용남;강관원
    • 대한토목학회논문집
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    • 제2권1호
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    • pp.1-17
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    • 1982
  • 하천형태학적(河川形態學的) 특성(特性)은 유역(流域)의 수문학적(水文學的) 특성(特性) 및 수리학적(水理學的) 특성(特性)과 밀접(密接)한 관계(關係)를 가진다. 본(本) 연구(硏究)에서는 하천형태학적(河川形態學的) 특성(特性)과 빈도유량(頻度流量) 및 수리기하(水理幾何)의 관계(關係) 그리고 빈도유량(頻度流量)과 수리기하학적(水理幾何學的) 특성간(特性間)의 상관성(相關性)을 금강수계(錦江水系)를 대상(對象)으로 분석(分析)하였으며, 이들 연구(硏究)의 목적(目的)은 미계획지점(未計劃地點)에 대한 이수계획(利水計劃)을 수립(樹立)하는데 필요한 자료(資料)를 제공(提供)하는데 있다. 금강수계(錦江水系)의 하천형태학적(河川形態學的) 특성분석(特性分析)은 Horton의 하천차수개념(河川次數槪念)을 이용(利用)하여 하천지형(河川地形)의 3대법칙(大法則)에 의거 분석(分析)하였으며 분석결과(分析結果)는 Horton의 법칙(法則)과 잘 일치(一致)하였다. 금강수계내(錦江水系內)의 5개(個) 수위표지점(水位標地點)에서 생기빈도(生起頻度) 0.1~0.9의 유량자료(流量資料)를 사용(使用)하여 얻은 각(各) 지점(地點)의 유량빈도곡선(流量頻度曲線)은 대체(大體)로 지수관계(指數關係)로 표시(表示)할 수 있었다. 하천형태학적(河川形態學的) 특성(特性)을 연속적(連續的)으로 표시(表示)하기 위하여 비례하천차수(比例河川次數)를 도입(導入)하였으며 이를 이용(利用)하여 유량(流量)-생기빈도(生起頻度)-비례하천차수간(比例河川次數間)의 관계(關係)에 대한 수학적(數學的) 모형(模型)을 정립(定立)하였다. 유역(流域)의 하천형태학적(河川形態學的) 특성(特性)을 매개변수(媒介變數)로 하여 빈도유량(頻度流量)과 수리기하학적(水理幾何學的) 인자간(因子間)의 관계(關係), 유역면적(流域面積)과 수리기하학적(水理幾何學的) 인자간(因子間)의 관계(關係)를 분석(分析)하여 각각(各各)에 대한 수학적(數學的) 모형(模型)을 제안(提案)하였다.

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Estimation and Classification of Flow Regimes for South Korean Streams and River

  • Park, Kyug Seo;Choi, Ji-Woong;Park, Chan-Seo;An, Kwang-Guk;Wiley, Michael J.
    • 한국수자원학회:학술대회논문집
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    • 한국수자원학회 2015년도 학술발표회
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    • pp.106-106
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    • 2015
  • The information of flow regimes continues to be norm in water resource and watershed management, in that stream flow regime is a crucial factor influencing water quality, geomorphology, and the community structure of stream biota. The objectives of this study were to estimate Korean stream flows from landscape variables, classify stream flow gages using hydraulic characteristics, and then apply these methods to ungaged biological monitoring sites for effective ecological assessment. Here I used a linear modeling approach (MLR, PCA, and PCR) to describe and predict seasonal flow statistics from landscape variables. MLR models were successfully built for a range of exceedance discharges and time frames (annual, January, May, July, and October), and these models explained a high degree of the observed variation with r squares ranging from 0.555 (Q95 in January) to 0.899 (Q05 in July). In validation testing, predicted and observed exceedance discharges were all significantly correlated (p<0.01) and for most models no significant difference was found between predicted and observed values (Paired samples T-test; p>0.05). I classified Korean stream flow regimes with respect to hydraulic and hydrologic regime into four categories: flashier and higher-powered (F-HP), flashier and lower-powered (F-LP), more stable and higher-powered (S-HP), and more stable and lower-powered (S-LP). These four categories of Korean streams were related to with the characteristics of environmental variables, such as catchment size, site slope, stream order, and land use patterns. I then applied the models at 684 ungaged biological sampling sites used in the National Aquatic Ecological Monitoring Program in order to classify them with respect to basic hydrologic characteristics and similarity to the government's array of hydrologic gauging stations. Flashier-lower powered sites appeared to be relatively over-represented and more stable-higher powered sites under-represented in the bioassessment data sets.

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도서지역 건천의 홍수유출 시 흐름 해석 (Stream Flow Analysis of Dry Stream on Flood Runoff in Islands)

  • 양원석;양성기
    • 한국환경과학회지
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    • 제22권5호
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    • pp.571-580
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    • 2013
  • In this study, compared with the result of water surface elevation and water velocity on the establishment of river maintenance basic plan and result of HEC-GeoRAS based GIS, and after use the result of water surface elevation and velocity were observed in the Han stream on Jeju island, analysis 2 dimensional stream flow. the lateral hydraulic characteristics and curved channel of the stream were analyzed by applying SMS-RMA2 a 2 dimensional model. The results of the analysis using HEC-RAS model and HEC-GeoRAS model indicated that the distribution ranges of water surface elevation and water velocity were similar, but the water surface elevation by section showed a difference of 0.7~2.18 EL.m and 0.63~1.16 EL.m respectively, and water velocity also showed differences of maximum 1.58m/sec and 2.67m/sec. SMS-RMA2 analysis was done with the sphere of Muifa the typhoon as a boundary condition, and as a result, water velocity distribution was found to be 1.19 through 3.91 m/sec, and the difference of lateral water velocity in No. 97 through 99 the curved channel of the stream was analyzed to be 1.59 through 2.36 m/sec. In conclusion it is anticipated that the flow analysis of 2 dimension model of stream can reflect the hydraulic characteristics of the stream curved channel or width and shape, and can be applied effectively in the establishment of river maintenance basic plan or management and designing of stream.

하도 합류부의 수리학적 특성을 고려한 RMA2 모형 매개변수의 민감도 분석 (Sensitivity Analysis of RMA2 Model Parameter Variation with Hydraulic Characteristics of Stream Junction Area)

  • 안승섭;임동희;서명준;이효정
    • 한국환경과학회지
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    • 제17권7호
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    • pp.783-793
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    • 2008
  • The purpose of this study is to analyze the sensitivity of the RMA2 model parameters reflecting the flow characteristics of stream junction and thus understand the hydraulic characteristics of the channel confluence flow. This study dealt with the input parameters of the RMA-2 model, a two-dimensional numerical analysis model widely used for researches both at home and abroad. The parameters of the RMA-2 model are roughness coefficient, turbulent diffusion coefficient, Coriolis forces latitude, Density, and mesh size. This study those parameters estimated from actual heavy rainfall, and varied the parameter size by (-)30%${\sim}$+30% to review the characteristics of the flow characteristics of the channel section. Weobserved that when the ratio of the channel width was relatively small, the smaller the approaching angle was, the farther from the junctions became the generating place of the maximum flow velocity, however, when the ratio of the channel width was relatively large, the larger the approaching angle was, the farther the generating place of the maximum flow velocity from the junctions became. In particular, the distance between junctions and the place where the maximum flow velocity generated showed an absolute correlationover 90% of the relative channel width, but an inverse relationwas found when the distance to the place where the flow velocity generated was shortened as relative the channel width between the main channel and tributary increased.

해석적 모형을 이용한 지하수 양수 및 하천수위 변화에 따른 하천수 감소 특성 분석 (Analysis of Stream Depletion due to Groundwater Pumping in Variable Stream Stages Using an Analytical Model)

  • 이정우
    • 지질공학
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    • 제29권4호
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    • pp.439-449
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    • 2019
  • 하천 건천화 예방 및 하천수와 지하수의 효율적 연계 이용을 위해서는 지하수 이용이 하천의 수량에 미치는 영향 평가가 수반되어야 한다. 이를 위해서는 대수층과 하천의 다양한 수리특성 조건에 대해 지하수 양수에 따른 하천수량의 변화 분석이 필요하다. 본 연구에서는 하천수위 변동을 반영할 수 있고 지하수 양수에 따른 하천수 감소량을 산정할 수 있는 Baalousha 해석해를 이용하여 하천수위가 지수함수적으로 감소하는 경우와, 감소 후 다시 회복되는 경우에 대해 지하수 양수로 인한 하천수 감소량의 변화 특성을 분석하였다. 대수층의 수리특성으로 투수량계수 10~100 ㎡/d 및 저류계수 0.05~0.3, 하천의 수리특성으로 하상수리전도성 0.01~20 m/d, 하천수위 감수상수 0.1~1.0 1/d, 그리고 하천과 관정의 이격거리 100~500 m 조건에 대해 지하수 양수량 대비 하천수 감소량인 하천수 기여도를 산정하고 그 거동 특성을 하천수위 변동 유무에 따라 종합적으로 분석, 제시하였다. 하천수위 감소 영향을 고려하였을 경우 하천수 기여도가 크게 감소하고 하천-관정 이격거리와 수리확산도의 함수인 하천고갈인자 값에 영향을 작게 받는 것으로 나타났으며, 반면에 하천수위 감소 후 회복되는 조건에서의 하천수 기여도는 하천수위 변동이 없는 경우와 큰 차이가 없는 것으로 나타났다. 이러한 결과는 하천수위 조절을 통해 지하수 양수시 하천수 및 대수층 저류량에 미치는 상대적 영향의 통제가 가능함을 의미한다.

안양시 관내하천 수질모형 예측에 관한 연구 (A Study on Mathematical Model for Water Quality Forecasting at Anyang Stream)

  • 김갑진;이양규
    • 상하수도학회지
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    • 제11권3호
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    • pp.112-123
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    • 1997
  • The Anyang stream is one of the Han river in Seoul Metropolitan area. It is 35.1km long, has a basin area of $282.26km^2$ and touches seven cities of Kyounggido and some of Seoul Metropolitan area. The situations of Anyang stream have resulted in severe stream water pollution problems. The purpose of this study were to measure the hydraulic characteristics and water quality, to make the countermeasures to achieve the stream water quality, to suggest the future conditions to improve water quality trough the Hydrodynamic and Water Quality Modal(WASP4). As the result of Anyang stream water quality forecsat, they are follows. Sewerage systems in the watershed of the Anyang stream have to be amended for wrong systemn and constructed in the upstream area of Anyang. The discharge of industrial wastewater has to be throughly controlled from the upstream area of the Anyang stream. Hydrodynamic and Water Quality Model(WASP4) for this study revealed the future water quality of the Anyang stream by computer simulation.

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