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Theoretical and experimental analysis of debris flow: rheology and two-phase modelling

机译:泥石流的理论和实验分析:流变学和两相建模

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To predict debris flow dynamics a numerical model, based on 1D De Saint Venant (SV) equations, was developed. The McCormack-Jameson shock capturing scheme was employed for the solution of the equations, written in a conservative law form. This technique was applied to determine both the propagation and the profile of a two-phase debris flow resulting from the instantaneous and complete collapse of a storage dam.To validate the model, comparisons have been made between its predictions and laboratorymeasurements concerning flows of water and homogeneous granular mixtures in a uniform geometry flume reproducing dam-break waves. Agreement between computational and experimental results is considered very satisfactory for mature (non-stratified) debrisflows, which embrace most real cases. To better predict immature (stratified) flows, the model should be improved in order to feature, in a more realistic way, the distribution of the particles of different size within the mixture.On the whole, the proposed model can easily be extended to channels with arbitrary cross sections for debris flow routing, as well as for solving different problems of unsteady flow in open channels by incorporating the appropriate initial and boundary conditions. Copyright pb 2008 John Wiley & Sons, Ltd.
机译:为了预测泥石流动力学,建立了基于1D De Saint Venant(SV)方程的数值模型。方程的解采用了McCormack-Jameson激波捕获方案,并以保守律形式编写。这项技术被用于确定由于蓄水坝的瞬时和完全坍塌而产生的两相泥石流的传播和剖面。为了验证该模型,已对其预测和实验室对水和水流的测量进行了比较。均匀几何形状的水槽中的均质颗粒混合物会产生溃坝波。对于成熟的(非分层)泥石流,计算结果与实验结果之间的一致性被认为是非常令人满意的,这些泥石流涵盖了大多数实际情况。为了更好地预测未成熟的(分层的)流动,应该改进该模型,以便更真实地描述混合物中不同尺寸的颗粒的分布情况。总体而言,可以轻松地将所提出的模型扩展到通道具有任意横截面的泥石流路径,以及通过合并适当的初始条件和边界条件来解决明渠中不稳定流动的各种问题。版权所有pb 2008 John Wiley&Sons,Ltd.

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