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A numerical model for heterogeneous and confined debris flows

机译:非均质和受限泥石流的数值模型

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The flow equation for a uniform debris flow can be obtained, analytically, from integration of the local constitutive equations only in very simple schemes, for example under the assumption of uniform solid concentration and absence of lateral walls. The flow discharges computed using these assumptions are much higher than those observed. In this paper a less restrictive solution is attempted. The fluid is assumed monophase (equal velocity of solids and fluid) and heterogeneous (solid concentration variable in the cross section). The effect of the mixture heterogeneity is described, and for a monophase fluid the constitutive parameters are expressed as a function of local solid concentration. A computational code has been implemented for estimating the concentration and velocity distribution in the cross section. The code is applied to a viscoplastic (Herschel-Bulkley) mixture.
机译:仅在非常简单的方案中,例如在假设固体浓度均匀且没有侧壁的情况下,才可以通过局部本构方程的积分来解析地获得均匀泥石流的流动方程。使用这些假设计算出的流量远高于观察到的流量。本文尝试了一种限制性较小的解决方案。假设流体是单相的(固体和流体的速度相等)而流体是非均质的(横截面中的固体浓度可变)。描述了混合物异质性的影响,对于单相流体,本构参数表示为局部固体浓度的函数。已经实现了用于估计横截面中的浓度和速度分布的计算代码。该代码适用于粘塑性(Herschel-Bulkley)混合物。

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