In this study, numerical analysis is conducted to investigate the flow characteristics of a turning type flood gate fishway with various design factors. The shapes of the fishway are circular and rectangular type. Baffles are installed to reduce the velocity in the fishway, and the gap and rotational arrangement of the baffles are set as design factors. To reduce the maximum velocity, a cavity-shaped break region is installed to examine the flow characteristics according to the presence of the break region. As a result, in the condition where the shape of the fishway is rectangular, the outlet average flow velocity is larger than that in the circular condition. The highest flow velocity occurs when the baffle is rotated in 90-degree arrangement. As the baffle gap increases, the average velocity increases. The cavity-shaped break region creates a recirculation zone in the fishway, and as a result, shows a decrease in the maximum velocity of up to 5.8%.

본 연구에서는 수로가 비대칭으로 연결되어 있는 합류부 및 합류부 주위에서의 홍수흐름특성에 대해 수리모형실험 및 수치모의를 통해 분석을 수행하였다. 본 연구에서 적용된 수치모형은 상업용 3차원 CFD 모형인 ANSYS CFX(ver. 14)이다. 수로 내로 유입되는 유량 변화에 따른 수리모형실험과 수치모의에 의한 합류부 및 합류부 주위에서의 수심분포에 대한 측정된 결과와 모의된 결과를 비교한 결과 비교적 잘 일치하는 것으로 나타났다. 합류부와 연결된 네 개의 수로 중 물이 유입되는 두 개 수로 방향에 따라 합류부 및 합류부 주위에서의 수심분포의 양상은 달라지며, 수로 내로 유입되는 유량의 증가에 따라서도 많은 차이가 발생된다는 것을 확인하였다.

본 연구에서는 도로가 비대칭으로 연결되었을때 합류부 및 합류부 주위에서의 홍수흐름특성을 수리실험 및 3차원 유동모의 프로그램을 이용하여 실험적 분석 및 수치적 분석을 수행하였으며, 적용된 수치모형은 1990년대 초반 영국원자력공사(UKAEA)와 캐나다의 ASC(Advance Science Computing)의 TASCflow로부터 개발되어 CFX-4와 CFX-TASCflow를 기반으로 발전된 CFD 해석모형인 ANSYS CFX모형이다. 모의 및 분석결과 본 연구에서 적용된 모형은 유입유량 및 유입각 조건에 따라 도로 합류부에서 변화되는 복잡한 수면양상을 비교적 잘 모의하는 것으로 나타났다. 또한 도로 합류부 내에서의 시간 및 공간적 수심변화와 두 개의 하류경계에서의 유출유량에 대한 모의결과는 측정결과와 비교적 잘 일치하였다.

In this study, CN value was estimated by using detailed soil map and land cover characteristic against upper basin of Kumho watermark located on the upper basin of Kumho river and the hydrologic morphological characteristic factors were extracted from the basin by using the DEM document. Also the runoff analysis was conducted by the WMS model in order to study how the assumed CN value affects the runoff characteristic. First of all, as a result of studying the soil type in this study area, mostly D type soil was identified by the application of the 1987 classification criteria. However, by that in 1995, B type soil and C type soil were distributed more widely in that area. When CN value was classified by the 1995 classification criteria, it was estimated lower than in 1987, as a result of comparing the estimated CNs by those standars. Also it was assumed that CN value was underestimated when the plan for Geum-ho river maintenance was drawn up. As a result of the analysis of runoff characteristic, the pattern of generation of the classification criteria of soil groups appeared to be similar, but in the case of the application of the classification criteria in 1995, the peak rate of runoff was found to be smaller on the whole than in the case of the application of the classification criteria in 1987. Also when the statistical data such as the prediction errors, the mean squared errors, the coefficient of determination and other data emerging from the analysis, was looked over in total, it seemed appropriate to apply the 1995 classification criteria when hydrological soil classification group was applied. As the result of this study, however, the difference of the result of the statistical dat was somewhat small. In future study, it is necessary to follow up evidence about soil application in many more watersheds and in heavy rain.