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박상덕 ( Sang Doeg Park ),김용현 ( Yong Hyun Kim ),함광현 ( Gwang Hyun Ham ),손상진 ( Sang Jin Son ),나락스메이 ( Raksmey Na ),김남진 ( Nam Jin Kim ) 한국지형학회 2021 한국지형학회지 Vol.28 No.3
In mountain gully, channelized debris flow is an important phenomenon in the process of topographical change. Social infrastructure as roads may be damaged by channelized debris flows, but there has been little information about their occurrence and movement to prepare for the risk of the debris flow. Most of the channelized debris flows occur during heavy rains in mountainous valleys that are difficult to access, so there are not many field data. In this study, the topographical characteristics of the catchment, the rainfall and runoff related to the debris flow, the sedimentary pattern and the cross-sectional change of the channel bed, and the underflow velocity of the gravel bed have been investigated and analyzed in the Singi gully where the channelized debris flows occurred. In the catchment, there was almost no sediment runoff because the vegetation combine with the debris landforms and covered the surface. Therefore, the obvious cause of the channelized debris flows is the collapse of the slope and bed of the gully. Even if the gravel, cobbles, and boulders of the channel bed were lost by debris flow, the thalweg change due to debris flow may not be significant because they are supplied from the gully side slope normally. After the gabion structures were installed, the debris flow increased the thalweg change, bed erosion and side slope of the gully. Various sedimentary structures in the gully were classified according to the factors supporting the sedimentation. The hypsometric curve of the gully reflects the debris landforms and vegetation characteristics of the watershed and the sediment runoff due to debris flow, etc. The relationship between the flow velocity and the hydraulic gradient was non-linear under the condition that the porous medium with gully bed gravels is saturated with water. These results may be used as basic data for channelized debris flow research.
박상덕 ( Sang Doeg Park ) 한국지형학회 2018 한국지형학회지 Vol.25 No.2
The sediment transport process in a river reflects the process of geomorphological change in the watershed, influences the river bed variation and the river channel migration, and is a parametric phenomenon that exhibits a dynamic self-adjusting process. Sediment load is divided into bedload and suspended load depending on the dominant mechanism. Quantitative sediment load is important information for solving river problems. Because it is difficult and time consuming to measure bedload, compared to that of suspended load, data on the sediment transport load and the research required for the gravel-bed rivers are insufficient. This study is to analyze the ratio of the bedload to the total sediment load in gravel-bed rivers. The sediment load ratio in gravel-bed rivers increases with the flow rate per unit width, and the rate of the bedload varies more rapidly than the suspended load. The sediment transport efficiency coefficient has been affected by the ratio of the flow depth to the mean diameter of particles and has been dependent on the shear velocity Reynolds number. So A* and B* are introduced to compensate for the uncertainties such as bed materials, sediment transport, and flow velocity distribution, and the coefficient of bedload ratio has been presented. For the sediment load data in experimental channels and rivers, A* was 3.1. The dominant variables of B* were u<sub>*</sub>d<sub>m</sub>/ν in the gravel-bed and h/d<sub>m</sub> in the sand-bed. When B* the is the same, in the experimental channels the coefficient of bedload ratio was affected by the bed forms, but in the rivers it was of little difference between the gravel-bed and sand-bed.
박상덕(Park, Sang Deog),백중철(Paik, Joongcheol),전우성(Jeon, Woo Sung),이현재(Lee, Hyun Jae) 대한토목학회 2019 대한토목학회논문집 Vol.39 No.2
개수로 만곡부에서 흐름은 원심력이 작용하기 때문에 횡방향 수면경사가 나타나고 유심선은 만곡 외측으로 치우친다. 수중 수제는 만곡부의 다양한 공학적인 문제를 해결하는 데 사용될 수 있다. 수중 수제가 흐름방향과 이루는 입사각과 수제 열 간격이 만곡부의 하상변동과 편수위에 미치는 영향을 파악하기 위해서 90°만곡 직사각형 단면 수로에 잔자갈을 깔고 이동상 수리실험을 하였다. 만곡부에 수중 수제를 설치하면 최대 세굴심은 증가하나 균일한 둔각으로 수제를 설치하면 세굴을 줄일 수 있다. 수제를 설치한 만곡부에 수제설치 기준하상의 형성유량과 같은 유량이 흐를 경우 최대 세굴이 발생하는 위치가 하류로 이동하고 편수위는 증가한다. 그 유량보다 작으면 최대 세굴심의 위치가 상류로 이동하며 편수위는 감소한다. 만곡부에서 수중 수제는 입사각, 유량, 수제 열 간격의 상호작용에 따라 하상변동과 편수위에 대한 영향이 다르다. Since the centrifugal force acts on the flow in the curved channel, a transverse water surface gradient occurs and the thalweg is biased toward the outer bank. The submerged vanes may be used to solve various engineering problems of the curved channels. In order to analyze the influence of an attack angle and the distance between the vane arrays on the river bed variation and the superelevation in a bend, movable bed hydraulic experiments were conducted in a 90°curved rectangular channel of a small-size gravel bed. Installing the submerged vanes in the bend increases the maximum scour depth. But if vanes are installed in a uniform obtuse angle, the scour depth may be reduced. If the flow rate in the channel bend with vanes equals to the channel forming discharge, the location of the maximum scour depth moved to the downstream and the superelevation increased. However if the flow rate is smaller than that, the location of the maximum scour depth moved upstream and the superelevation decreased. The channel bed change and the superelevation due to the installation of the submerged vanes have been dependent on the interaction of the attack angle, the flow rate, and the distance between the arrays.