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Impact of blocks on deformable layers: Influence of block rotation and size

机译:块对可变形层的影响:块旋转和大小的影响

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To model the trajectories followed by a block falling along a slope, it is crucial the adoption of rules capable of simulating the changes in the boulder energy content due to impacts. The numerical simulation of impacts is thus fundamental for assessing the risk associated with rockfall events and for designing sheltering structures. The different approaches developed to simulate the impact of a boulder on a soil layer can be classified in three main categories: lumped mass, rigorous and hybrid. Lumped mass approaches consider the boulder as a material point and the boulder-soil interaction is evaluated by means of restitution coefficients. Rigorous approaches simulate the boulder-soil interaction by either continuum mechanics or the distinct element method. Hybrid approaches model the boulder as a point mass but the interaction with the soil is simulated by means of more advanced constitutive relationships. Both the lumped mass and the hybrid models do not generally take the influence of rotation and boulder shape into account. In order to investigate these factors, the authors improved the hybrid model BIMPAM proposed by di Prisco and Vecchiotti (2006). In this renewed version: i) a rotational degree of freedom for the boulder is added; ii) a moment- rotation relationship is defined; and iii) a toppling slider, simulating the occurrence of toppling at the end of the impact phase, conceived. The model is capable of accounting for the influence of the boulder shape. The parametrical analysis, concerning inclined trajectories on horizontal strata, clearly shows that during the impact a boulder spin originates, even in case the initial motion of the block is purely translational.
机译:为了模拟轨迹,然后沿着斜坡下降的块,采用能够模拟由于撞击而引起的巨石能量含量变化的规则至关重要。因此,影响的数值模拟对于评估与落石事件相关的风险以及设计避难所结构至关重要。为模拟巨石对土壤层的影响而开发的不同方法可分为三大类:集总质量,严格质量和混合质量。集总质量方法将巨石视为实质点,并通过恢复系数评估巨石与土壤的相互作用。严格的方法通过连续力学或独特元素方法来模拟巨石与土壤的相互作用。混合方法将巨石建模为点质量,但通过更高级的本构关系模拟了与土壤的相互作用。集总质量模型和混合模型通常都没有考虑旋转和巨石形状的影响。为了研究这些因素,作者改进了di Prisco和Vecchiotti(2006)提出的混合模型BIMPAM。在这个更新的版本中:i)增加了巨石的旋转自由度; ii)定义了力矩-旋转关系; iii)设想了一个推顶滑块,它模拟了在冲击阶段结束时发生的推翻。该模型能够说明巨石形状的影响。有关水平地层倾斜轨迹的参数分析清楚地表明,即使在块体的初始运动纯粹是平移的情况下,在撞击过程中也会产生巨石旋转。

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