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Field Meausurements and Numerical Simulation of Turbidity Current in the Shichikashuku Reservoir

机译:Shichikashuku水库的浊度场的现场测量和数值模拟

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A three dimensional numerical model was developed to predict the behavior of fine solids carried by flood water into a reservoir. The model is based on the standard k-ε turbulence model using the Boussinesq approximation and combined with a diffusion equation in which the settlement of fine solids is taken into account by using their terminal velocity relative to the surroundings. The model feasibility is tested for a flood caused by a typhoon in the reservoir where the authors have conducted detailed field measurements on turbidity current and sedimentation: the travel of fine solids in the reservoir during the flood was simulated for the whole process from the inflow at the upstream end to the deposition at the bottom of the reservoir. The calculation results successfully reproduced the observed profiles of turbidity currents and the spatial distribution of deposited sediment.
机译:建立了三维数值模型来预测洪水带入水库的细小固体的行为。该模型基于采用Boussinesq逼近的标准k-ε湍流模型,并与扩散方程式结合,在该扩散方程式中,通过使用相对于周围环境的最终速度考虑了细固体的沉降。对模型的可行性进行了测试,以应对由水库中的台风引起的洪水,作者对浊流和泥沙进行了详细的现场测量:模拟了洪水期间水库中细颗粒固体在整个过程中从入水口的运动。储层底部沉积的上游端。计算结果成功地再现了所观察到的浊流分布和沉积沉积物的空间分布。

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