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Variable-Concentration and Boundary Effects on Debris Flow Discharge Predictions

机译:泥石流流量预测中的浓度和边界效应

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The uniform flow of natural debris mixture is generally modeled assuming a uniform solid concentration and the absence of lateral walls. The resulting flow discharges are, however, higher than those observed and, in the case of erodible boundaries, the equilibrium between the moving and nonmoving mixtures cannot be simulated. Such a model also cannot simulate the effect of lateral rigid boundaries that generate lateral velocity and concentration gradients. This paper describes a numerical model to determine the concentration and velocity distribution in the two directions transverse to the flow. The model is applied to a uniform laminar flow of a mixture with a shear-thickening Herschel-Bulkley constitutive behavior, with rheological parameters expressed in terms of the local solid concentration, and allows the simulation of different conditions in the presence of both erodible and rigid boundaries.
机译:通常在假定固体浓度均匀且没有侧壁的情况下对天然碎片混合物的均匀流动进行建模。但是,所产生的流量高于观察到的流量,并且在边界易腐蚀的情况下,无法模拟移动混合物和非移动混合物之间的平衡。这样的模型也不能模拟产生横向速度和浓度梯度的横向刚性边界的影响。本文描述了一个数值模型,用于确定横向于水流的两个方向上的浓度和速度分布。该模型应用于具有剪切增稠的Herschel-Bulkley本构行为的混合物的均匀层流,其流变参数以局部固体浓度表示,并允许在存在易蚀性和刚性的情况下模拟不同条件边界。

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