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A collision fragmentation model for predicting the distal reach of brittle fragmentable rock initiated from a cliff

机译:碰撞碎裂模型,用于预测从悬崖开始的脆性碎裂岩石的远距离

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摘要

Collision-induced fragments from large volume isolated rock block collapsed from cliffs with heights of hundreds of meters could cause greater distal reaches via superimposing additional velocities on the frontal smaller fragments at the impact zone. These fragments may pose significant threats to distant infrastructure, life, and property due to their extremely high velocities and disastrously long runouts. To reveal the collision fragmentation mechanism on the evolution of higher velocities fragments and predict the distal reach of the frontal smaller ones, a two-dimensional block-terrain impact model of an intense brittle rock block colliding onto a rigid plane is proposed. Furthermore, the well-documented experiments on collision fragmentation of brittle chalk were used to verify the derived mathematical equations of the model. The results indicated that the calculated results can match experimental data well. The proposed model can provide meaningful insights into the kinetics of fragmental rockfalls and enable predictions of the possible distal reaches of explosive fragments, which are crucial for hazard zoning and mitigation design.
机译:来自数百米高的悬崖坍塌的大量孤立岩石块的碰撞诱发碎片可能会通过将附加速度叠加在撞击区的额叶较小碎片上而引起更大的远距离延伸。这些碎片由于其极高的速度和灾难性的长跳动而可能对遥远的基础设施,生命和财产构成重大威胁。为了揭示碰撞碎片在高速碎片演化过程中的作用机制,并预测较小的额叶的远距离,提出了一种强烈的脆性岩石块在刚性平面上碰撞的二维块体撞击模型。此外,使用有据可查的脆性粉笔碰撞碎裂实验来验证模型的推导数学方程。结果表明,计算结果与实验数据吻合良好。所提出的模型可以提供关于碎裂岩屑动力学的有意义的见解,并能够预测爆炸性碎屑的可能远距离,这对于危险区划和缓解设计至关重要。

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