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Development of the cellular automaton model for simulating the propagation extent of debris flow at the alluvial fan: A case study of Yohutagawa, Japan

机译:模拟冲积扇处泥石流传播程度的元胞自动机模型的开发:以日本Yohutagawa为例

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As a two-phase anisotropic mixture, debris flow shows some complex fluid-dynamical characteristics on its motion behavior, which makes it difficult to be modelled or simulated through standard approaches. Consequently, Cellular Automaton (CA) model in the field of parallel computing, which has long been verified as efficiently applying in the simulation of complex natural process, are recently introduced to simulate flow-type phenomena. In this paper, the components of CA model for debris-flow simulation are reviewed, after that a two-dimensional cellular space is generated from the Digital Terrain Model (DTM) with 2.5 m high-resolution, and the relationship of lattices in the space is defined as Moore neighborhood type. A new transition function, aiming at flow direction determination, is proposed through the way that implementing the debris-flow inertial influence into the traditional topography-based D8 algorithm, by a multiplying equation or an addition equation. We also present a three-step propagation algorithm to integrate the single flow routines, then use the constant discharge model to assign the flow depth to each routine, in this way the propagation area can be gradually delineated through each increment step. We test the developed model with CH87 Brichboden debris-flow event, and illustrate its application with Yohutagawa debris-flow event in Japan, 2010. Results of both cases show that a more accurate propagation perimeter pattern is observed using addition equation in the modified flow direction algorithm, comparing to the traditional D8 algorithm and multiplying equation-based algorithm.
机译:作为两相各向异性混合物,泥石流在其运动行为上显示出一些复杂的流体动力学特征,这使得很难通过标准方法对其进行建模或模拟。因此,最近引入了并行计算领域中的元胞自动机(CA)模型,该模型已被证明有效地应用于复杂自然过程的仿真中,最近它被用来模拟流型现象。在本文中,对泥石流模拟的CA模型的组成进行了回顾,然后从具有2.5 m高分辨率的数字地形模型(DTM)生成了二维单元空间,并分析了空间中的晶格关系被定义为摩尔邻里类型。通过将泥石流的惯性影响通过乘积方程或加法方程实现到传统的基于地形的D8算法中,提出了一种针对流向确定的新过渡函数。我们还提出了一种三步传播算法来集成单个流量例程,然后使用恒定流量模型为每个例程分配流量深度,这样,传播区域就可以通过每个增量步骤逐渐描绘出来。我们使用CH87 Brichboden泥石流事件测试了开发的模型,并举例说明了其在2010年日本Yohutagawa泥石流事件中的应用。两种情况的结果表明,在修改的流向上使用加法方程可以观察到更精确的传播周长图样。与传统的D8算法和基于乘法方程的算法相比。

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