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3D dynamics of debris flows quantified at sub-second intervals from laser profiles

机译:从激光曲线的子第二间隔以子第二间隔量化的碎片流量的3D动态

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摘要

We use pairs of parallel mounted laser profile scanners to measure main debris-flow variables in two debris-flow channels in central and southern Switzerland. The scanners measure the instantaneous cross-sectional geometry of debris flows at rates of 25-100 Hz, and we apply large-scale particle image velocimetery to estimate velocity. The scanners also provide direct measurements of flow depth. From these data, we were able to estimate debris-flow depth, velocity and discharge for 16 out of 17 events. These results are consistent with discharge estimated from a system of geophones and a radar gauge for two available datasets. We also investigated debris-flow geometry to quantify rheology-controlled cross-flow convexity and found that four events manifest strong surface convexity at their surge fronts where we expect the largest boulders and low pore-fluid pressures. The scanners provide a completely new view of debris-flow dynamics and channel morphology and present novel opportunities to measure discharge and investigate debris-flow geometries.
机译:我们使用一对并联安装的激光剖面扫描仪来测量中央和瑞士南部的两条碎片流动通道中的主要碎片流量。扫描仪测量碎片流量的瞬时横截面几何形状,速率为25-100 Hz,我们将大规模粒子图像速度应用于估计速度。扫描仪还提供流量深度的直接测量。从这些数据中,我们能够估计17个事件中的16个碎片流动深度,速度和放电。这些结果与来自地震孔系统的放电和两个可用数据集的雷达计估计一致。我们还研究了碎片流动几何,以量化流变术控制的横流凸起,发现四个事件在其浪涌前沿表现出强大的表面凸起,在那里我们预期最大的巨石和低孔隙流体压力。扫描仪提供了一种完全新的碎片流动动态和通道形态的新视图,并提出了测量放电和调查碎片流动几何的新机遇。

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