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Assessing entrainment of bed material in a debris-flow event: a theoretical approach incorporating Monte Carlo method

机译:评估泥石流事件中的床层夹带:结合蒙特卡罗方法的理论方法

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摘要

Entrainment of underlying bed sediment by a debris flow can significantly increase the debris-flow magnitude. To study this phenomenon, a theoretical approach to assessing bed-sediment entrainment is presented. The approach is based on a static approximation that bed-sediment entrainment occurs when the shearing stress of the flow is sufficiently high to overcome the basal resistance of the bed sediment. In order to delineate erodible zones in a channel, we analyze the critical condition of this static equilibrium model, and subsequently propose a new concept of a critical line to detect the entrainment reaches in a channel. Considering the spatial and temporal uncertainties of the input parameter, the approach is further incorporated within a Monte Carlo method, and the distribution of entrainment zones and post-entrainment volumes can be analyzed. This approach is illustrated by back-analysis of the 2010 Yohutagawa debris-flow event, Japan. Results from 10 000 trials of Monte Carlo simulation are compared with the in situ surveys. It is shown that the present approach can be satisfactorily used to delineate erodible zones and estimate possible entrainment volume of the event. Discussion regarding the sensitivities and limitations of the approach concludes the paper. Copyright (c) 2015 John Wiley & Sons, Ltd.
机译:泥石流夹带下面的床底沉积物会显着增加泥石流的大小。为了研究这种现象,提出了一种评估床底泥沙夹带的理论方法。该方法基于静态近似,即当流的剪切应力足够高以克服床层沉积物的基础阻力时,床层夹带就会发生。为了描绘通道中的易蚀区域,我们分析了此静态平衡模型的临界条件,随后提出了一种临界线的新概念,以检测通道中的夹带。考虑到输入参数的时空不确定性,该方法进一步纳入了蒙特卡洛方法,并且可以分析夹带区域和夹带后体积的分布。对2010年日本Yohutagawa泥石流事件的反向分析说明了这种方法。将10000次Monte Carlo模拟试验的结果与现场调查进行了比较。结果表明,本方法可以令人满意地用于描绘易蚀区域并估计事件的可能夹带量。本文讨论了该方法的敏感性和局限性。版权所有(c)2015 John Wiley&Sons,Ltd.

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