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An energy-based approach to predict debris flow mobility and analyze empirical relationships

机译:一种基于能量的方法来预测泥石流流动性并分析经验关系

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摘要

Several empirical relationships allowing a preliminary estimate of debris flow runout distances have been proposedudto correlate the runout length to the volume of the sliding granular mass, delimit potentially hazardous areas, and designudsafeguarding measures. To overcome their large variability and define their fields of applicability, an energy-based model,udpredicting debris flow mobility, is developed. The power balance of a granular mass sliding along two planar surfaces is writtenudby taking into account the volume of the debris mass, the slopes of the sliding surfaces, an assigned interstitial pressure, theudpossible mass variation along the motion, the energy dissipation due to the grain inelastic collisions (“granular temperature”udwithin a basal “shear layer”), and friction. A system of ordinary differential equations is obtained; its numerical solution allows,udthrough parametrical analyses: (i) highlighting of the role of physical and mechanical parameters on the runout distance, suchudas grain size material, interstitial pressures, grain collisions, and erodibility of the crossed channel; and (ii) defining of theudfavourable conditions for debris flows mechanism generation. Finally, through the back-analysis of some cases, an originaludrelationship to estimate the runout length, as well as to interpret the results of the empirical formulas, is proposed.
机译:已经提出了几种经验关系,可以初步估计泥石流的跳动距离,以使跳动长度与滑动颗粒物的体积相关,划定潜在的危险区域以及设计/防暴措施。为了克服它们的巨大可变性并定义它们的适用范围,开发了一种基于能量的模型,该模型可以预测泥石流的流动性。沿两个平面滑动的颗粒状物质的功率平衡是通过考虑碎屑的体积,滑动面的斜率,分配的间隙压力,沿运动的不可能的质量变化,能量耗散来写入 ud由于晶粒无弹性的碰撞(基底温度“剪切层”内的“颗粒温度” ud)和摩擦。得到一个常微分方程组;通过数值分析,可以进行参数分析:(i)突出物理参数和机械参数在跳动距离上的作用,例如,颗粒大小,间隙压力,颗粒碰撞和交叉通道的易蚀性; (ii)定义产生泥石流的有利条件。最后,通过对某些情况的反分析,提出了一种原始非关系式来估算跳动长度,并解释经验公式的结果。

著录项

  • 作者

    Federico F; Cesali C;

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  • 年度 2015
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  • 原文格式 PDF
  • 正文语种 eng
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