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首页> 外文期刊>Journal of visualization >Versatile image-based measurements of granular flows and water wave propagation in experiments of tsunamis generated by landslides
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Versatile image-based measurements of granular flows and water wave propagation in experiments of tsunamis generated by landslides

机译:基于滑坡产生的海啸实验中基于图像的颗粒流和水波传播的多功能测量

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摘要

Landslides falling into water bodies can generate destructive waves, which can be classified as tsunamis. An experimental facility to study this phenomenon has been set up. It consists of a landslide generator releasing gravel at high-speed into a wave basin. A non-intrusive system has been designed ad-hoc to be able to measure the high velocity and the geometry of the landslide as well as the generated waves characteristics. The measurement system employs the treatment of images captured by a high-speed camera which records the launched granular material illuminated by a laser sheet. A grid of laser sheets marks the basin water surface. The water has been filled by a small amount of kaolin to properly reflect the laser light at water surface. Thus, by filming with high definition cameras the perturbed water surface and successively processing the resulting images, it has been possible to measure the generated waves. The measurement framework employs a versatile camera calibration technique which allows accurate measurements in presence of: (1) high lens distortions; (2) pronounced non-parallelism condition between camera sensor and plane of measurement coincident with the laser sheet. The maximum resolution of the measurement tool is 0.01 mm, while the maximum uncertainty due to systematic error has been estimated to be 15% for the worst-case scenario. This work improves the suitability of image-based measuring systems in granular flows and free surface hydraulics experiments.
机译:滑落到水体中的滑坡会产生破坏性波,可以将其分类为海啸。已经建立了研究这种现象的实验设施。它由一个滑坡发生器组成,它可以将砾石高速释放到波浪盆地中。非侵入式系统已被临时设计,能够测量滑坡的高速度和几何形状以及所产生的波浪特征。该测量系统采用由高速相机拍摄的图像进行处理,该相机记录由激光片照射的发射的粒状材料。激光薄片的网格标记了盆水表面。水中已经填充了少量高岭土,以在水表面适当反射激光。因此,通过用高清晰度照相机拍摄被摄动的水表面并相继处理所产生的图像,已经有可能测量所产生的波。测量框架采用了通用的相机校准技术,该技术可在以下情况下进行精确测量:(1)高镜头畸变; (2)相机传感器和与激光片重合的测量平面之间存在明显的非平行条件。测量工具的最大分辨率为0.01毫米,而在最坏的情况下,由于系统误差而导致的最大不确定度估计为15%。这项工作提高了基于图像的测量系统在颗粒流动和自由表面水力学实验中的适用性。

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