• 제목/요약/키워드: Water Right

검색결과 583건 처리시간 0.041초

시화호 인공습지에서 시공간적 수질분포 및 오염물질 제거효율 평가 (Temporal and Spacial Distributions of Water Quality and Evaluation of Pollutant Removal Efficiency in the Sihwa Constructed Wetland)

  • 최돈혁;최광순;김동섭;김세원;최동호;황인서;이윤경;강호
    • 대한환경공학회지
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    • 제30권10호
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    • pp.1013-1020
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    • 2008
  • 시화호 인공습지의 오염물질 제거효율을 분석평가하고 수질정화기능의 저하원인을 파악하기 위하여 습지내 16개 지점에서 시공간적 수질분포에 대해 조사하였다. TN을 제외한 오염물질 제거효율은 조성 초기에 비해 낮아졌으며, 계절변동 또한 매우 큰 것으로 나타났다. 특히 BOD와 TP의 평균 제거효율이 각각 12.3%, -44.5%로 낮고, TN과 SS에 비해 계절변동이 큰 것으로 나타났다. 월평균 BOD의 제거효율은 습지 하류부에서 식물플랑크톤이 대량 증식하였던 4월과 7월에 처리효율이 나타나지 않았으며, TP의 경우는 4월부터 8월까지 제거효율이 지속적으로 감소하였으며 수온이 가장 높았던 8월에 -291%를 나타냈다. 폐쇄수역에서 SS 농도분포는 좌안과 우안에 비해 중앙지점에서 높은 것으로 나타났다. 또한 ANOVA test로부터 수평적으로 유의적인 차이(p = 0.013, 중앙 > 좌안 > 우안)를 보였다. 시화호 인공습지에서 오염물질 제거효율의 저하원인은 과도한 유기물 생산에 의한 습지의 혐기성환경과 이에 따른 습지 하류부에서 용출된 인과 대량 증식한 식물플랑크톤이 균등하지 못한 물 흐름에 의해 식생대를 거치지 않고 유출되었기 때문으로 유추된다.

고라니에서 최소침습적 관절경과 TightRope®의 이용한 엉덩관절탈구 교정 증례 (Minimally Invasive Arthroscopic-Assisted Reduction with TightRope® for Coxofemoral Luxation in a Korean Water Deer (Hydropotes inermis argyopus))

  • 허수영;설재원;박지영;정성목;이해범
    • 한국임상수의학회지
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    • 제32권6호
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    • pp.540-543
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    • 2015
  • 왼쪽 뒷다리 체중부하 없는 파행을 가진 고라니가 구조 되었다. 임상검사와 방사선검사에서 앞쪽외측 엉덩 관절 탈구로 진단되었고 탈구에 원인은 확인 할 수 없었다. 고나리에 앞쪽외측 엉덩 관절 탈구는 토글 핀(mini-TightRope$^{(R)}$)과 관절경을 이용하여 최소 침습적 방법을 통해 교정 하였다. 고라니에 앞쪽외측 엉덩관절 탈구는 수술 후 성공적으로 교정되었다. 수술 후 60일후 고라니는 자연으로 복귀 할 수 있었다. 이번에 사용된 토글핀과 관절경을 이용한 최소 침습적인 엉덩관절 탈구 교정법은 야생동물에서 성공적으로 사용이 가능할 것으로 생각된다.

하천 만곡률과 홍수량에 따른 수면경사도 산정 (Estimation of the Water Surface Slope by the Flood Discharge with River Bend Curvature)

  • 최한규;이문희;백효선
    • 산업기술연구
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    • 제26권A호
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    • pp.129-137
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    • 2006
  • In this research, we made a one and two-dimensional analysis of numerical data collected from the bend curvature of a bended river section. According to the result from the numerical analysis, the inflow & output angle caused a water level deviation which increased with an increase of the flood discharge. From the water level deviation of our two-dimensional numerical model, we obtained the maximum slope of 6,67% when the inflow and output angle was 105 degrees and the flood discharge was 500 CMS. As for the right side, the differences with the one-dimensional numerical model were reduced when the angle was more than $90^{\circ}$. As for the left side the differences were reduced when the angle was more than $105^{\circ}$. For a river with more than 90 degrees bend curvature, a hydraulic experiment would be more appropriate than a numerical analysis.

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플랫강 유역의 위험에 처한 서식지 보호를 위한 MODSIM 하천 네트워크 흐름모의 (MOSIM NETWORK FLOW MODELING FOR IMPROVING CRITICAL HABITAT IN PLATTE RIVER BASIN)

  • 이진희;김길호;심명필
    • 한국수자원학회:학술대회논문집
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    • 한국수자원학회 2007년도 학술발표회 논문집
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    • pp.2039-2043
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    • 2007
  • Like other major river basin systems in the West of the United States the Platte River Basin are faced with the challenges of allocating more water for plant and animal species. A part of the Central Platte River was designated as critical habitat for the whooping crane in 1978. The water allocation system in the Platte River Basin is dominated by the Prior Appropriation Doctrine, which allocates water according to the priorities based on the date of water use. The Platte River Basin segregated into five subregions for purpose of analysis. 24 years of historic records of monthly flow and all the demands were complied. The simulation of river basin modeling includes physical operation of the system including water allocation by water rights and interstate compact agreements, reservoir operations, and diversion with consumptive use and return flow. MODSIM, a generalized river basin network model, was used for estimating the timing and magnitude of impacts on river flows and diversions associated with water transfers from each region. A total of 20 alternatives were considered, covering transfers from each of the five regions of basin with several options. The result shows that the timing and availability of augmented water at the critical habitat is not only a function of use by junior appropriators, but also of river losses, and timing of return flows.

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취입모의 경제적 계획취입수심 산정방법에 대한 연구 (A Study on a Calculation Method of Economical Intake Water Depth in the Design of Head Works)

  • 김철기
    • 한국농공학회지
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    • 제20권1호
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    • pp.4592-4598
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    • 1978
  • The purpose of this research is to find out mathemetically an economical intake water depth in the design of head works through the derivation of some formulas. For the performance of the purpose the following formulas were found out for the design intake water depth in each flow type of intake sluice, such as overflow type and orifice type. (1) The conditional equations of !he economical intake water depth in .case that weir body is placed on permeable soil layer ; (a) in the overflow type of intake sluice, {{{{ { zp}_{1 } { Lh}_{1 }+ { 1} over {2 } { Cp}_{3 }L(0.67 SQRT { q} -0.61) { ( { d}_{0 }+ { h}_{1 }+ { h}_{0 } )}^{- { 1} over {2 } }- { { { 3Q}_{1 } { p}_{5 } { h}_{1 } }^{- { 5} over {2 } } } over { { 2m}_{1 }(1-s) SQRT { 2gs} }+[ LEFT { b+ { 4C TIMES { 0.61}^{2 } } over {3(r-1) }+z( { d}_{0 }+ { h}_{0 } ) RIGHT } { p}_{1 }L+(1+ SQRT { 1+ { z}^{2 } } ) { p}_{2 }L+ { dcp}_{3 }L+ { nkp}_{5 }+( { 2z}_{0 }+m )(1-s) { L}_{d } { p}_{7 } ] =0}}}} (b) in the orifice type of intake sluice, {{{{ { zp}_{1 } { Lh}_{1 }+ { 1} over {2 } C { p}_{3 }L(0.67 SQRT { q} -0.61)}}}} {{{{ { ({d }_{0 }+ { h}_{1 }+ { h}_{0 } )}^{ - { 1} over {2 } }- { { 3Q}_{1 } { p}_{ 6} { { h}_{1 } }^{- { 5} over {2 } } } over { { 2m}_{ 2}m' SQRT { 2gs} }+[ LEFT { b+ { 4C TIMES { 0.61}^{2 } } over {3(r-1) }+z( { d}_{0 }+ { h}_{0 } ) RIGHT } { p}_{1 }L }}}} {{{{+(1+ SQRT { 1+ { z}^{2 } } ) { p}_{2 } L+dC { p}_{4 }L+(2 { z}_{0 }+m )(1-s) { L}_{d } { p}_{7 }]=0 }}}} where, z=outer slope of weir body (value of cotangent), h1=intake water depth (m), L=total length of weir (m), C=Bligh's creep ratio, q=flood discharge overflowing weir crest per unit length of weir (m3/sec/m), d0=average height to intake sill elevation in weir (m), h0=freeboard of weir (m), Q1=design irrigation requirements (m3/sec), m1=coefficient of head loss (0.9∼0.95) s=(h1-h2)/h1, h2=flow water depth outside intake sluice gate (m), b=width of weir crest (m), r=specific weight of weir materials, d=depth of cutting along seepage length under the weir (m), n=number of side contraction, k=coefficient of side contraction loss (0.02∼0.04), m2=coefficient of discharge (0.7∼0.9) m'=h0/h1, h0=open height of gate (m), p1 and p4=unit price of weir body and of excavation of weir site, respectively (won/㎥), p2 and p3=unit price of construction form and of revetment for protection of downstream riverbed, respectively (won/㎡), p5 and p6=average cost per unit width of intake sluice including cost of intake canal having the same one as width of the sluice in case of overflow type and orifice type respectively (won/m), zo : inner slope of section area in intake canal from its beginning point to its changing point to ordinary flow section, m: coefficient concerning the mean width of intak canal site,a : freeboard of intake canal. (2) The conditional equations of the economical intake water depth in case that weir body is built on the foundation of rock bed ; (a) in the overflow type of intake sluice, {{{{ { zp}_{1 } { Lh}_{1 }- { { { 3Q}_{1 } { p}_{5 } { h}_{1 } }^{- {5 } over {2 } } } over { { 2m}_{1 }(1-s) SQRT { 2gs} }+[ LEFT { b+z( { d}_{0 }+ { h}_{0 } )RIGHT } { p}_{1 }L+(1+ SQRT { 1+ { z}^{2 } } ) { p}_{2 }L+ { nkp}_{5 }}}}} {{{{+( { 2z}_{0 }+m )(1-s) { L}_{d } { p}_{7 } ]=0 }}}} (b) in the orifice type of intake sluice, {{{{ { zp}_{1 } { Lh}_{1 }- { { { 3Q}_{1 } { p}_{6 } { h}_{1 } }^{- {5 } over {2 } } } over { { 2m}_{2 }m' SQRT { 2gs} }+[ LEFT { b+z( { d}_{0 }+ { h}_{0 } )RIGHT } { p}_{1 }L+(1+ SQRT { 1+ { z}^{2 } } ) { p}_{2 }L}}}} {{{{+( { 2z}_{0 }+m )(1-s) { L}_{d } { p}_{7 } ]=0}}}} The construction cost of weir cut-off and revetment on outside slope of leeve, and the damages suffered from inundation in upstream area were not included in the process of deriving the above conditional equations, but it is true that magnitude of intake water depth influences somewhat on the cost and damages. Therefore, in applying the above equations the fact that should not be over looked is that the design value of intake water depth to be adopted should not be more largely determined than the value of h1 satisfying the above formulas.

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2차원 이송-확산 모형을 이용한 취수장 유입 수질 예측 (Water Quality Modeling for Intake Station by 2-dimensional Advection-Dispersion Model)

  • 김재동;김지훈;김영도;송창근;서일원
    • 상하수도학회지
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    • 제25권5호
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    • pp.667-679
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    • 2011
  • In this study, the influences of pollutant from Dae-po Stream and So-gam Stream located at the downstream of Nak-dong River on the water quality at Mul-geum water intake station were analyzed using RAMS model. Field measurements of velocity by ADCP, and water quality distribution of BOD and TP by water sampling were carried out to present the input and verification data for numerical simulations. The comparison between RAM2 and ADCP measurement, which aimed for the analysis of 2-D velocity distribution around Mul-geum water intake station showed that two results matched well along the spanwise direction. The prediction of pollutant concentration by RAM4 agreed fairly well with the measured data except for the points nearby right banks in the vicinity of tributary pollutant source. Flushing effect by the increase of mainstream discharge in Nak-dong River was analyzed to provide the damage mitigation in preparation for the accidental water pollution. With increasing mainstream discharge, high velocity and increased water quantity induced increasing dilution effect, thereby decreasing the inflow pollutant concentration rapidly.

한국고라니의 불완전한 상완머리동맥 (Incomplete Brachiocephalic Trunk in a Korean Water Deer)

  • 안동춘;태현진;박병용;심정하;김종택;김인식
    • 한국임상수의학회지
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    • 제28권5호
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    • pp.526-529
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    • 2011
  • 새김질동물류의 상완머리동맥은 대동맥활에서 분지하는 유일한 동맥으로 왼빗장밑동맥, 양목동맥 또는 왼 오른온목동맥, 오른빗장밑동맥을 분지한다. 이런 분지 양상은 발생초기에 왼온목동맥과 왼빗장밑동맥이 심장 내림현상에 따라 차례로 앞쪽으로 이동하여 일명 무명동맥과 합류함으로써 생긴다. 본 증례의 약 31개월령 한국고라니 암컷에서는 상완머리동맥과 왼빗장밑동맥이 합쳐져 외형상 하나의 혈관을 이루고 있었으나 두 동맥의 중간막 안쪽층이 남아 있었으며, 이에 따라 불완전한 상완머리동맥으로 남아 있었음을 볼 수 있었다. 이러한 기형은 왼빗장밑동맥이 정상적으로 이동 하였으나 합쳐지는 과정이 불완전하게 된 경우라고 볼 수 있으며, 한국고라니에서 처음 보고하는 바이다.

확률 분포형의 극치 수문량 예측 능력 평가에 관한 연구 (A Study on the Estimation of Extreme Quantile of Probability Distribution)

  • 정진석;신홍준;안현준;허준행
    • 한국수자원학회:학술대회논문집
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    • 한국수자원학회 2017년도 학술발표회
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    • pp.399-400
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    • 2017
  • 홍수나 가뭄 등 극치 현상의 통계분석 및 빈도해석에 있어 극치분포형이 널리 사용되고 있으며, 이러한 극치분포형의 특성을 이해하기 위해서는 분포형의 오른쪽 꼬리(right tail) 부분 특성을 자세히 분석할 필요가 있다. 이에 따라 본 연구에서는 Monte Carlo 모의를 통하여 다양한 극치분포형의 오른쪽 꼬리 부분의 통계적 특성 및 그 예측 능력을 연구하였다. 극치분포형으로는 우리나라 확률수문량 산정에 널리 활용되고 있는 generalized extreme value (GEV), Gumbel, generalized logistic 분포를 사용하였으며, 매개변수 산정 방법으로는 확률가중모멘트법을 사용하였다. 모의실험의 모분포로는 수문빈도해석에서 많이 사용되는 GEV 분포를 사용하였고, 30년 이상 자료를 보유한 기상청 지점 자료의 왜곡도를 조사하여 모의실험에 사용되는 모집단의 왜곡도로 가정하여 표본 자료를 발생시켰다. 예측 능력의 평가는 재현기간 10~1000년의 확률수문량을 왜곡도계수를 고려한 GEV 도시위치공식을 이용하여 GEV 확률지에 도시하고, 평균제곱근오차(root mean square error), 편의(bias), 평균상대오차(mean relative difference), 평균절대상대오차(mean absolute relative difference)를 이용하여 최적 분포형을 선정함으로써 이루어진다. 또한 예측 능력 평가결과의 타당성 확인을 위해 극치분포형의 적합정도를 잘 나타낸다고 알려진 modified Anderson-Darling 방법의 검정결과와 비교하여 적절성을 확인하였다.

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Effect of a Magnetic Field on Mixed Convection of a Nanofluid in a Square Cavity

  • Sheikhzadeh, G.A.;Sebdani, S. Mazrouei;Mahmoodi, M.;Safaeizadeh, Elham;Hashemi, S.E.
    • Journal of Magnetics
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    • 제18권3호
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    • pp.321-325
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    • 2013
  • The problem of mixed convection in a differentially heated lid-driven square cavity filled with Cu-water nanofluid under effect of a magnetic field is investigated numerically. The left and right walls of the cavity are kept at temperatures of $T_h$ and $T_c$ respectively while the horizontal walls are adiabatic. The top wall of the cavity moves in own plane from left to right. The effects of some pertinent parameters such as Richardson number (ranging from 0.1 to 10), the volume fraction of the nanoparticles (ranging 0 to 0.1) and the Hartmann number (ranging from 0 to 60) on the fluid flow and temperature fields and the rate of heat transfer in the cavity are investigated. It must be noted that in all calculations the Prandtl number of water as the pure fluid is kept at 6.8, while the Grashof number is considered fixed at 104. The obtained results show that the rate of heat transfer increases with an increase of the Reynolds number, while but it decreases with increase in the Hartmann number. Moreover it is found that based the Richardson and Hartmann numbers by increase in volume fraction of the nanoparticles the rate of heat transfer can be enhanced or deteriorated compared to the based fluid.

빙 및 일반해역 운항을 고려한 아라온호 선수프레임의 피로수명 계산 (Calculation of Fatigue Life of Bow Frame of ARAON Considering Navigating in Ice and Open Waters)

  • 안우성;이탁기;황미란
    • 한국해양공학회지
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    • 제32권6호
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    • pp.458-465
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    • 2018
  • Ice-going ships such as icebreakers, icebreaking tankers, and icebreaking LNG carriers are subjected to wave loads in open water and ice loads in ice-covered water. In terms of the ship's structural design, the local ice load is important. The fatigue failure due to repeated ice loads is also important. ISO 19906 specifies the assessment of the fatigue limit for a polar offshore structures. In addition, Lloyd's Register refers to fatigue damage based on ShipRight FDA ICE. In ShipRight FDA ICE, the fatigue damage indices due to wave and ice loads are simply presented as 0.5 for each load. It also states that the sum of the two fatigue damage indices should not exceed one. This study calculated and analyzed the fatigue damage index and fatigue life considering ARAON's voyage schedules and the assumed Antarctic voyage based on data measured during the Arctic voyage of ARAON in 2010.