MPM modelling of debris flow entrainment and interaction with an upstream flexible barrier

被引:24
作者
Vicari, Herve [1 ]
Tran, Quoc Anh [1 ]
Nordal, Steinar [1 ]
Thakur, Vikas [1 ]
机构
[1] Norwegian Univ Sci & Technol NTNU, Dept Civil & Environm Engn, Trondheim, Norway
基金
欧盟地平线“2020”;
关键词
Landslide; Debris flow; Entrainment; Flexible barrier; Material point method; Flume; POINT METHOD; LANDSLIDE; DESIGN;
D O I
10.1007/s10346-022-01886-8
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
Flexible barriers may be installed upstream in debris flow channels to reduce entrainment of bed material. Simulating both the entrainment and the impact on a barrier by the same numerical tool remains challenging. For this purpose, a three-dimensional one-phase material point method (MPM) software is used herein to back-calculate two large-scale flume experiments. These experiments were conducted to measure the entrainment of an erodible bed and the impact on a flexible barrier. To simulate the entrainment of the wet bed, a Mohr-Coulomb softening model is introduced. In the model, the apparent friction angle of the bed material decreases as a function of the distortional strain, effectively reproducing the pore pressure increase observed in the experiments. From the tests and the numerical simulations, we identify two main mechanisms leading to entrainment: (i) the direct rubbing and colliding effect of the flow on to the bed and (ii) a significant bed shear strength reduction. Concerning the first mechanism, existing models only consider the rubbing of the bed surface by a shear stress parallel to the slope. However, we observe that a ploughing-type erosion occurs due to normal stresses acting on the bed in the flow direction. The additional ploughing explains why beds which are mechanically stronger than the flow can also be partly entrained. Larger entrainment volumes are found when the bed material loses shear strength due to pore pressure buildup that eventually leads to a self-propelled entrainment where the bed no longer has frictional strength to carry its own weight.
引用
收藏
页码:2101 / 2115
页数:15
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