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Physically Based Model for Evaluation of Rock Scour due to High-Velocity Jet Impact

机译:基于物理模型的高速射流冲击对岩石冲刷的评估

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摘要

Scour of rock may occur downstream of dam spillways, as a result of the impact of high-velocity jets. The phenomenon is traditionally assessed by means of (semi-) empirical methods. These partially neglect basic physical processes responsible for rock mass breakup. Therefore, a model to evaluate the ultimate depth and time evolution of scour in jointed rock is presented. The model is based on near-prototype scaled experimental investigations of transient water pressures in artificially created rock joints and on a numerical modeling of the measured pressures. It describes two different ways of rock mass destruction, i.e., failure by instantaneous or progressive breakup of closed-end rock joints, and failure by dynamic ejection of single rock blocks. The corresponding computational methods are easily applicable to practice, without neglecting relevant physics. The basic principles are outlined and applied to the well-known scour hole at Cabora-Bassa Dam.
机译:由于高速射流的撞击,岩石冲刷可能会发生在大坝溢洪道的下游。传统上,该现象是通过(半)经验方法进行评估的。这些部分忽略了导致岩石破裂的基本物理过程。因此,提出了一种评价节理岩石冲刷极限深度和时间演化的模型。该模型基于人工创建的岩缝中瞬时水压力的近原型规模实验研究,并且基于测得压力的数值模型。它描述了两种不同的破坏岩石质量的方法,即,由于封闭端岩石节的瞬时或渐进破坏而导致的破坏,以及动态弹出单个岩石块而导致的破坏。相应的计算方法很容易应用到实践中,而不会忽略相关的物理学。概述了基本原理,并将其应用于Cabora-Bassa大坝的著名冲孔。

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