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Parameterization of a numerical 2-D debris flow model with entrainment: A case study of the Faucon catchment, Southern French Alps

机译:带夹带的二维泥石流数值模型的参数化:以法国南部阿尔卑斯山Faucon流域为例

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摘要

The occurrence of debris flows has been recorded for more than a century in the European Alps, accounting for the risk to settlements and other human infrastructure that have led to death, building damage and traffic disruptions. One of the difficulties in the quantitative hazard assessment of debris flows is estimating the run-out behavior, which includes the run-out distance and the related hazard intensities like the height and velocity of a debris flow. In addition, as observed in the French Alps, the process of entrainment of material during the run-out can be 10-50 times in volume with respect to the initially mobilized mass triggered at the source area. The entrainment process is evidently an important factor that can further determine the magnitude and intensity of debris flows. Research on numerical modeling of debris flow entrainment is still ongoing and involves some difficulties. This is partly due to our lack of knowledge of the actual process of the uptake and incorporation of material and due the effect of entrainment on the final behavior of a debris flow. Therefore, it is important to model the effects of this key erosional process on the formation of run-outs and related intensities. In this study we analyzed a debris flow with high entrainment rates that occurred in 2003 at the Faucon catchment in the Barcelonnette Basin (Southern French Alps). The historic event was back-analyzed using the Voellmy rheology and an entrainment model imbedded in the RAMMS 2-D numerical modeling software. A sensitivity analysis of the rheological and entrainment parameters was carried out and the effects of modeling with entrainment on the debris flow run-out, height and velocity were assessed.
机译:在欧洲阿尔卑斯山,已有超过一个世纪记录了泥石流的发生,这是对定居点和其他人类基础设施导致死亡,建筑损坏和交通中断的风险的解释。泥石流定量危害评估中的困难之一是估算跳动行为,其中包括跳动距离和相关的危险强度(如泥石流的高度和速度)。另外,如在法国阿尔卑斯山所观察到的那样,跳动期间物料的夹带过程相对于在源头区域触发的最初动员的体积而言可能是体积的10至50倍。夹带过程显然是可以进一步确定泥石流的大小和强度的重要因素。泥石流夹带数值模拟的研究仍在进行中,并涉及一些困难。这部分是由于我们缺乏对物质吸收和掺入的实际过程的了解,以及由于夹带对泥石流的最终行为的影响。因此,重要的是对这一关键的侵蚀过程对跳动和相关强度形成的影响进行建模。在这项研究中,我们分析了2003年在巴塞洛内特盆地(法国南部阿尔卑斯山)的Faucon流域发生的高夹带率泥石流。使用Voellmy流变学和嵌入在RAMMS 2-D数值建模软件中的夹带模型对历史事件进行了反向分析。进行了流变学和夹带参数的敏感性分析,并对夹带建模对泥石流跳动,高度和速度的影响进行了评估。

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