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Numerical analysis of submarine debris flows based on critical state soil mechanics

机译:基于临界状态土力学的海底泥石流数值分析

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Submarine debris flows are an extremely complex phenomenon that involves phase transition ofthe material from solid to semi-fluid. This is caused by large deformation and possible occurrence of entrainingambient fluid. In the conventional ‘equivalent fluid method’ based on Non-Newtonian fluid models, constantrheological parameters are assumed and calibrated using the evidence of previous debris flows. Such parameters,however, do not accurately represent the material behavior and the real physics involved in submarine debrisflows. The aim of this study is to develop a new modeling framework for submarine debris flows based onthe critical state soil mechanics. The effect of phase transition is incorporated in a modified Cam clay basedconstitutive model. The diagnostic analyses indicate that the proposed model is capable of reproducing theprevious flow event by using the material parameters derived from the conventional soil tests.
机译:海底泥石流是一种极其复杂的现象,涉及相变过程。 材料从固体到半流体。这是由于较大的变形和可能发生夹带引起的 环境流体。在基于非牛顿流体模型的常规“等效流体方法”中,常数 假定流变参数并使用先前泥石流的证据进行校准。这样的参数, 但是,不能准确地表示海底碎片所涉及的物质行为和真实物理学 流。这项研究的目的是为海底泥石流建立一个新的建模框架。 临界状态土壤力学。相变的影响被并入到改性的基于Cam的粘土中 本构模型。诊断分析表明,提出的模型能够重现 通过使用从常规土壤测试中得出的材料参数来确定先前的流动事件。

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