开发泥石流和河水多次流入的沉积和洪水传播数值模型

T. Wada, K. Nakatani, Y. Satofuka, T. Mizuyama, K. Kosugi, H. Miwa
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摘要

因此,我们开发了一种数值模型,该模型可根据泥石流的不同特征,考虑这些泥石流在汇流处的沉积和洪水传播情况。因此,我们建立了一个名为 "泥石流和河流洪水多流入模型 "的数值模型。在所开发的模型中,多个山区溪流一维计算区域的下游两端在任意选定点上连接在一个汇流区的二维计算区域上。利用所开发的模型,我们进行了计算,再现了 2011 年台风 "塔拉斯 "在日本和歌山县那智川平原引发的泥石流灾害。在这次灾害中,泥石流同时从几条山涧流入河流,造成了溪流和河流汇合处周围的沉积和洪水,周围的受损区域也随之扩大。计算结果表明,我们可以合理地估算出泥石流和河流洪水在汇合点及其下游地区周围的沉积和洪水传播情况。这也表明,所开发的模型有助于我们研究从山涧流入的多股泥石流是如何造成灾害的,并针对这些流入的泥石流制定更有效的对策。
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Development of a Numerical Model for Deposition and Flood Propagation by Multiple Inflows of Debris Flows and River Floods
a numerical model that considers how the deposition and flood propagation of these flows occur at the confluences based on their various characteristics. Therefore, we developed a numerical model named “the multiple inflow model with debris flows and river floods.” In the developed model, the downstream ends of several 1-D calculation areas for mountain streams are connected on a 2-D calculation area for a confluence area at any selected points. With the developed model, we performed calculations to reproduce the debris flow disaster in the Nachigawa River plain, which induced by 2011 Typhoon Talas in Wakayama Prefecture, Japan. During this event, the debris flows that simultaneously flowed into the river from several mountain streams contributed to the deposition and flooding around the streams and river confluences, and the damaged areas around them expanded. The calculated result indicates that we can estimate reasonably the deposition and flood propagation of the debris flows and river flood around the confluences and their downstream areas. This also indicates that the developed model helps us to investigate how multiple debris flows inflowing from mountain streams contribute to the disaster, and develop more efficient countermeasures for these inflows.
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