Two-dimensional simulation of two viscous debris flows in Austria

J. Hübl, H. Steinwendtner
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引用次数: 37

Abstract

Risk mitigation and hazard assessment in steep torrent catchments requires a high level of information about possible runout distances, depth, velocities and resulting impact forces of mass movement processes and its consequences to endangered areas. Two well documented debris flow events at Wartschenbach/Eastern Tyrol and Moschergraben/Styria enable to investigate possible applications of the FLO-2D computer model. The FLO-2D computer model was developed at the Colorado State University and is a grid-based physical process model which routes precipitation-runoff and flood hydrographs over unconfined surfaces and channels using either a kinematic, diffusive or dynamic wave approximation to the momentum equation. All transitions between water floods and fully developed debris flows can be simulated using topographic data files to build the grid elements, information about surface roughness and properties of the sediment water mixture. A quadratic rheological model is used to describe flow behaviour of viscous debris flows. The rheological properties of deposited debris flow material are determined using a rotational viscometer and a new developed conveyor-channel.

The simulation results and the gained experience are of great promise to the future of debris flow modelling.

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奥地利两次粘性泥石流的二维模拟
在陡峭的激流集水区减轻风险和进行危害评估,需要掌握大量信息,了解可能的涌流距离、深度、速度和由此产生的大规模运动过程的冲击力及其对濒危地区的后果。在Wartschenbach/东蒂罗尔和Moschergraben/Styria发生的两个有充分记录的泥石流事件使我们能够研究FLO-2D计算机模型的可能应用。FLO-2D计算机模型是由科罗拉多州立大学开发的,是一种基于网格的物理过程模型,它利用动量方程的运动学、扩散或动态波近似,在无约束表面和通道上绘制降水径流和洪水曲线。利用地形数据文件,可以模拟洪水和完全发育的泥石流之间的所有过渡,以建立网格元素、有关表面粗糙度的信息和沉积物-水混合物的性质。采用二次流变模型描述粘性泥石流的流动特性。用旋转粘度计和新研制的输送通道测定了沉积泥石流物质的流变特性。模拟结果和获得的经验对今后的泥石流建模具有重要的指导意义。
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