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DebrisInterMixing-2.3: a Finite Volume solver for three dimensional debris flow simulations based on a single calibration parameter – Part 2: Model validation

机译:DebrisIntermixing-2.3:基于单个校准参数的三维泥石流模拟的有限体积求解器 - 第2部分:模型验证

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摘要

Here we present the validation of the fluid dynamic solver presented in part one of this work (von Boetticher et al., 2015), simulating laboratory-scale and large-scale debris-flow experiments. The material properties of the experiments, including water content, sand content, clay content and its mineral composition, and gravel content and its friction angle, were known. We show that given these measured properties, a single free model parameter is sufficient for calibration, and a range of experiments with different material compositions can be reproduced by the model without recalibration. The model validation focuses on different case studies illustrating the sensitivity of debris flows to water and clay content, channel curvature, channel roughness and the angle of repose of the gravel. We characterize the accuracy of the model using experimental observations of flow head positions, front velocities, run-out patterns and basal pressures.
机译:在这里,我们将对这项工作的一部分(von Boetticher等人,2015)中提出的流体动力学求解器进行验证,以模拟实验室规模和大规模泥石流实验。实验的材料特性包括水含量,砂含量,粘土含量及其矿物组成,砾石含量及其摩擦角。我们表明,给定这些测量的属性,单个自由模型参数就足以进行校准,并且无需重新校准就可以通过该模型重现具有不同材料成分的一系列实验。模型验证的重点在于不同的案例研究,这些案例说明了泥石流对水和粘土含量,河道曲率,河道粗糙度和砾石的休止角的敏感性。我们使用流头位置,前端速度,跳动模式和基础压力的实验观察来表征模型的准确性。

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