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An integrated method for rapid estimation of the valley incision by debris flows

机译:碎片流动快速估计谷切口的综合方法

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AbstractValley incision by debris flow is an important process in creating and maintaining the topography of a valley, in addition to explaining the significant growth of the magnitudes of debris flow hazards. In this paper, we introduce a semi-empirical method to quantitatively estimate the valley incision process by debris flows over complex bed surface. We first reproduce natural bed surface across the valley by a polyline, and use a hydrograph of discharge versus time to represent the temporal variation of debris flow process. The presented method subsequently predicts the debris flow behavior over an irregular bed surface. A dynamic erosion law considers the solved debris flow behavior and estimates an instantaneous erosion rate. Finally, the accumulative incision depth of bed sediment is calculated, reshaping the initial bed surface across the valley. The presented method is simple and therefore notably beneficial for practical work. The performance of the proposed method has been tested using two case study applications. Results demonstrate that the presented method estimates comparable incision depth as revealed in the in-situ survey and the numerical simulation.Highlights?A quantitative method for predicting valley incision by debris flow is introduced.?Velocity distribution of debris flow across the valley can be analyzed.?A dynamic erosion law is incorporated to estimate instantaneous erosion rate.?The performance of the proposed method has been tested by two cases.]]>
机译:<![cdata [ 抽象 碎片流动的谷类切口是创建和维护谷地形的重要过程,除了解释碎片流动危害大小的显着增长。在本文中,我们介绍了一种半经验方法,通过碎片流过复杂的床表面来定量估计谷切口过程。我们首先通过折线再现山谷的天然床面,并使用排出的水文与时间来代表碎片流程过程的时间变化。呈现的方法随后预测不规则床表面上的碎屑流动。动态侵蚀法考虑了解决的碎片流动行为,估计瞬时侵蚀率。最后,计算床沉积物的累积切口深度,将初始床表面倒在山谷上。呈现的方法很简单,因此有利于实际工作。已经使用两种案例研究应用测试了所提出的方法的性能。结果表明,呈现的方法估计了原位调查中揭示的可比切口深度和数值模拟。 亮点 通过碎片流预测谷流程的定量方法。 可以分析谷谷流的速度分布。 a动态侵蚀法纳入o估计瞬时侵蚀率。 所提出的方法的性能已经通过两种情况进行了测试。 ]]>

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