• 제목/요약/키워드: downstream areas

검색결과 250건 처리시간 0.042초

Investigation on cavitating flow and parameter effects in a control valve with a perforated cage

  • Wang, Hong;Zhu, Zhimao;Zhang, Miao;Li, Jie;Huo, Weiqi
    • Nuclear Engineering and Technology
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    • 제53권8호
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    • pp.2669-2681
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    • 2021
  • Valve is widely used in the various industry areas to adjust and control the flow. Cavitation frequently takes place and sometimes is inevitable in various types of valve to cause the erosion damage. Therefore, how to control and minimize the effect of cavitation is still an important topic. This study numerically investigates the cavitating flow in a control valve with a perforated cage. The effects of some parameters on the cavitation are discussed. It also discusses to use the throttling steps to govern the cavitating flow. The results show that the opening degree of valve and the length of downstream divergent connection both influence the cavitation. The increase of the divergent length reinforces the cavitation. And the larger the opening of valve is, the intenser the cavitation is and the more vapor is present. The more throttling steps are helpful to decrease the cavitation.

영산강유역의 지형과 주민생활 (Topography of the Yeongsan River Basin and its Locals' Life)

  • 범선규
    • 한국지역지리학회지
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    • 제8권4호
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    • pp.451-467
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    • 2002
  • 영산강은 남한의 주요 강에 속하며, 유역은 식량생산의 핵심지 중의 하나이다. 영산강유역에는 범람원과 구릉지가 널리 발달되어 있으며, 현재의 영산호 일대에는 간석지도 넓게 분포했었다. 범람원은 '들'로 불리우며, 골짜기가 중은 '물목'의 상류쪽에 넓게 펼쳐진다. 범람원은 조선 발까지는 거의 전부 논으로 재발되었다. 이 농경지를 배경으로 도회지들이 성장했다. 구릉지는 '등', '까끔', '야산' 등으로 불리우며, 나주시와 영암군에 넓게 분포한다. 구릉지의 농경지개발은 1960년대부터 시작되었으며 오늘날에도 진행되고 있다. 많은 개간지의 영농은 외지인들에 의한 임차농의 형태로 영위된다. 간석지 즉 '뻘밭'은 영산강 하류의 남해만에 넓게 펼쳐져 있었으며, 곳곳에 '개옹'으로 불리우던 갯골이 발달했었다. 간석지는 1981년에 영산강하구둑이 준공된 이후 대대적인 간척사업에 의해 농경지로 개발되어 '영산평야'로 바뀌었다. 새로운 평야의 등장으로 모든 취락이 순수 농촌으로 탈바꿈하였다.

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부상웨어 설치에 따른 대청호 조류 성장 억제 효과 수치모의 (Numerical Modeling Effects of a Skimmer Weir Method on the Control of Algal Growth in Daecheong Reservoir)

  • 김유경;정세웅;이흥수;정용락
    • 한국물환경학회지
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    • 제23권5호
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    • pp.581-590
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    • 2007
  • A float-type weir has been proposed for the control of algal blooms in some of eutrophic reservoirs recently. It is known as a costly and ecologically sound method, but there is little understanding about the sustainability of this low-cost technology for reservoirs that are located in monsoon climate areas where large flood events during the summer cause high water surface fluctuations. The objective of this study was to assess the effectiveness of a skimmer weir aimed at controlling algal blooms in the lacustrine zone and near the drinking water withdrawal structures of Daecheong Reservoir under various hydrodynamic flow conditions. The effect of weir on the control of algal blooms was simulated using a laterally averaged two-dimensional hydrodynamic and eutrophication model that can accommodate vertical displacement of the weir following the water surface fluctuations. Numerical simulations were performed for two different hydrological conditions, 2001 and 2004 for representing drought year and normal year, respectively. The results showed that the weir is very effective method to control algal blooms in the reservoir by curtailing the transport of phosphorus and algae from contaminated inflow to the downstream lacustrine epilimnion during the draught year. However, large flood events occurred in 2004 transported nutrients and algae built upstream of the weir into the downstream euphotic zone by strong entrainments.

TOPMODEL과 Muskingum 기법을 연계한 안성천 유역의 홍수유출 분석 (Flood Runoff Analysis using TOPMODEL Linked with Muskingum Method - Anseong-cheon Watershed -)

  • 권형중;김성준
    • 한국지리정보학회지
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    • 제6권1호
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    • pp.1-11
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    • 2003
  • 본 연구는 안성천 유역($581.7km^2$)을 대상으로 TOPMODEL 분포형 수문모형에 Muskingum 하도 추적기법을 연계하여 유출분석을 수행하였다. 유역의 하류에 분포하고 있는 평야부에 대해서는 linear trend surface interpolation 기법을 사용하여 상류에서 하류방향으로 DEM을 평활화하는 방법으로 평야부의 흐름방향을 부여하였다. TOPMODEL 적용시 지형지표인자의 분포 및 빈도를 추출하기 위하여 MFD(multiple flow direction) 알고리즘을 이용하였다. 중규모 이상의 유역을 대상으로 TOPMODEL을 적용할 경우 DEM의 해상도 저하가 모형의 결과에 영향을 미치게 되므로, 그 해결방안으로서 전체유역을 소유역으로 분할하여 DEM의 해상도를 유지시키고, 소유역간의 결과는 Muskinguim 하도추적기법으로 전달되도록 하였다. 전체유역을 대상으로 500m 해상도로 TOPMODEL을 적용한 유출모의 결과 27.2%의 상대오차를 보인 반면, 유역을 2개의 소유역으로 나누어 300m 및 350m의 공간해상도로 TOPMODEL과 Muskingum 기법을 병행하여 적용한 결과 상대오차가 15.8%로 나타나, 모형의 효율이 증가하는 것을 확인할 수 있었다.

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수치해석모형에 의한 홍수추적 (Flood Routing Using Numerical Analysis Model)

  • 이용직;권순국
    • 한국농공학회지
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    • 제31권1호
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    • pp.117-130
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    • 1989
  • In this study, an implicit one-dimensional model, DWRM(Dynamic Wave Routing Model) was developed by using the four-point weighted difference method. By applying the developed model to the Keum River, the parameters were calibrated and the model applicability was tested through the comparison between observed and computed water levels. In addition, the effects of the construction of an estuary dam to the flood wave were estimated as a result of the model application. The results of the study can be summarized as follows; 1. The roughness coefficients were evaluated by comparison between observed and computed water level at Jindu, Gyuam and Ganggyeung station in 1985. The Root Mean Squares for water level differences between observed and computed values were 0.10, 0.11, 0. 29m and the differences of peak flood levels were 0.07, 0.02, 0. 07m at each station. Since the evaluated roughness coefficients were within the range of 0.029-0.041 showing the realistic value for the general condition of rivers, it can be concluded that the calibration has been completed. 2. By the application of model using the calibrated roughness coefficients, the R. M. S. for water level differences were 0.16, 0.24, 0. 24m and the differences of peak flood level were 0.17, 0.13,0.08 m at each station. The arrival time of peak flood at each station and the stage-discharge relationship at Gongju station agreed well with the observed values. Therefore, it was concluded that the model could be applied to the Keum River. 3. The model was applied under conditions before and after the construction of the estuary dam. The 50-year frequency flood which had 7, 800m$^3$/sec of peak flood was used as the upstream condition, and the spring tide and the neap tide were used as the downstream condition. As the results of the application, no change of the peak flood level was showed in the upper reaches of 19.2km upstream from the estuary dam. For areas near 9.6km upstream from the estuary dam, the change of the peak flood level under the condition before and after the construction was 0. 2m. However considering the assumptions for the boundary conditions of downstream, the change of peak flood level would be decreased.

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WASP4 모형에 의한 수질모델링 (Water Quality Modeling by the WASP4 Model)

  • 조홍연;전경수;이길성
    • 한국해안해양공학회지
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    • 제5권3호
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    • pp.221-231
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    • 1993
  • 하구 및 호소 수질모형인 WASP4를 사용하여 수도권 상수취수 대안지점들에서의 장래수질을 모의하였다. 모의 수질항목으로서 엽록소 a, 질소 순환요소들, 인 순환요소들, BOD 및 DO 등을 포함하였다. 1986년부터 1990년까지의 월별 댐유입량 및 방류량 자료를 사용한 계절별 물수지 분석에 의하여 모형의 경계단에서의 계절평균 유량 입력자료를 산정하여, QUAL2E 모형에 의하여 모의된 수질 입력자료와 함께 장래수질의 히절별 모의에 사용하였다. 또한 장래 오염부하량 및 취수 대안지점에서의 취수에 따른 민감도 분석을 수행하였다. 장래수질의 모의 결과, 여러 대안지점들 중 북한강 하류단 지점의 수실이 보든 수질항목에 대하여 가장 양호하며, 남한강 하류단 지점이 가장 불량한 것으로 나타났다. 또한, 북한강 대안지점에서 취수가 기손 취수지점에서의 오염도를 다소 증가시키나 그 정도는 미미한 것으로 나타났다.

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댐 운영방식에 따른 이수안전도의 비교 (Comparison of Water Supply Reliability by Dam Operation Methods)

  • 최시중;이동률;문장원
    • 한국수자원학회논문집
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    • 제47권6호
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    • pp.523-536
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    • 2014
  • 댐의 이수안전도는 물 수요량, 저수량, 가뭄에 의한 유입량에 의해서 주로 영향을 받는다. 그러나 댐 운영방식에 따라 댐의 이수안전도는 차이가 발생할 수 있다. 우리나라의 수자원장기종합계획은 K-WEAP모형을 이용하여 댐 하류의 물부족이 발생하면 물 부족량만큼 공급하는 부족량공급(Deficit supply) 방식을 이용하고 있으나 일정방류(Prime flow) 방식을 적용하면 이수안전도가 달라질 수 있다. 본 연구의 목적은 댐 운영방식에 따른 댐의 이수안전도의 변화를 분석하는 것이다. 이들 결과는 하류의 유지유량공급, 수력 발전을 위하여 일정방류가 고려되는 환경에서 댐의 이수안전도를 재평가하는데 활용될 수 있을 것이다.

강원도 남대천, 연곡천과 사천천의 식물플랑크톤 군집 (The Phytoplankton community of Namdae-stream, Yeongok-stream and of Sacheon-stream in Gangwon-do)

  • 김용진;이옥민
    • 환경영향평가
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    • 제20권3호
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    • pp.281-297
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    • 2011
  • The specie composition, stranding crops and the dominant species of phytoplankton were studied in three streams, Namdae-stream, Yeongok-stream and Sacheon-stream from May 2008 to February 2009. The water qualities of the three streams which run into estuary were also examined using phytoplankton indicators. As the result, the phytoplankton appeared 94 taxa in Namdae-stream, 79 taxa in Yeongok-stream and 73 taxa in Sacheon-stream, diatoms appeared the most in phytoplankton. Genus Navicula and Cymbella in diatoms appeared to be over 10 taxa in each stream, N. cryptocephala, N. cryptotenella and N. gregaria, the pollution tolerance taxa, appeared more frequent in the downstream. Due to the separation of each substrate by the rapid water velocity in the upstream, Achnanthes minutissima, a known periphyton, was dominant in upstream site at Namdae and Yeongok-stream. Some construction areas and sites of downstream of Namdae-stream, Yeongok-stream and Sacheon-stream were shown to be polluted because pollution tolerance taxa, such as Cyclotella meneghiniana, Nitzschia palea and Oscillatoria limnetica, were dominant. The total of 20 taxa phytoplankton indicators were found, composed of 16 taxa of Water pollution algae including Oscillatoria limosa, 2 taxa of Clean water algae Meridion circulare and Staurastrum puntulatum, 1 taxa of Toxic algae Microcystis aeruginosa and 1 taxa of Taste and odor algae Fragilaria construens. Water pollution indicators were appeared frequently in polluted sites of biological water quality(DAIpo, TDI) and of sites containing high trophic state index(TSI). Therefore, using the phytoplankton indicators can assess water quality through relation of biological water quality and trophic state index.

저수지 붕괴예보 시스템의 수위기준 검증 연구 (A Study on the Verification of water level criteria for forecasting system of reservoir failure)

  • 이백;최병한
    • 한국구조물진단유지관리공학회 논문집
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    • 제23권3호
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    • pp.51-55
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    • 2019
  • 저수지의 붕괴 발생 시 인명 및 재산피해의 예방 및 저감을 위하여 붕괴예보 시스템의 필요성은 대두되고 있는 상황이다. 붕괴 예보시스템의 효율적 활용을 위해서는 실시간 계측한 이상거동 및 붕괴징후에 따라 대응할 수 있는 관리기준은 가장 중요한 요소이다. 기 연구된 수위 관리기준의 검증을 위하여 저수량에 따라 10여개의 저수지를 선정하고 수위변화 자료를 분석하여 적정성을 검토하였다. 1년 동안의 수위계측 자료에서 가장 급격한 변화구간을 선정하여 가중치 및 추세선을 적용하여 분석한 결과 3분위로 수립된 관리기준값은 7%이내의 표준편차를 보여주었다. 이는 수립된 관리기준값은 적정하다고 판단된다.

동강의 하천 퇴적물의 입자 특성 및 암석의 반발 강도 특성에 대한 연구 (A Study on the Characteristics of River Sediments and the Rebound Strength of Rock and Sediment in Dong River)

  • 신원정;김종연
    • 한국지형학회지
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    • 제26권1호
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    • pp.41-57
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    • 2019
  • The grain size characteristics of river sediments and the characteristics of bedrock were investigated for the 24km section of the Dong River upstream of the Han River. The bedrock of the study area is various limestone belonging to the Paleozoic Choseon limestone group, and Mesozoic sandstone and conglomerate occur in some areas. Most of the river channel is made of limestone, and most of the river bottom is covered with fluvial sediments. More than 70% of these sediments are sandstone and conglomerate, rather than limestone which forms the basis of the valley. Sediment particles seem to have been supplied upstream of the study area rather supplied from the slope near of the channel. It is difficult to find the statistically significant difference in the shape of the sediment particles of limestones and non-limestones. However, limestones has platy forms rather than block forms, it can be assumed that the limestone was supplied from the surrounding valley wall and transported over a short distance. The particle sizes of DG1~DG2(the upstream section) are decreasing in the downstream direction. However, at DG3, which is a tributary, Jijangcheon, confluence particle size increases and at DG4 particle size increases more. In the case of DG4, it may be influenced by the influx of tributaries, but it also can be supposed as the impact of the large flood in 2002. In the downstream parts(DG5~DG7), the particle size decreases exponentially with distance. The rebound strength of stream sediments and bedrock was measured by using Schmidt hammer. Limestone showed lower rebound strength than non-limestone. According to the results of the sediment and bedrock, it can be seen that the sandstone and conglomerate with high rebound values pass through valley with the relatively low strength limestone. The sediments of limestone were decreased in grain size more rapidly than those of limestone sediments.