首页> 外文期刊>Oceanographic Literature Review >Runup of landslide-generated waves breaking on steep slopes captured using digital imagery and hydrochromic paint
【24h】

Runup of landslide-generated waves breaking on steep slopes captured using digital imagery and hydrochromic paint

机译:使用数码图像和水红十字涂料捕获的滑坡引起的滑坡的落水机会

获取原文
获取原文并翻译 | 示例
           

摘要

Runup of landslide-generated waves is an important natural hazard in coastal regions, and can result in major damage to the natural and built environment. Past work has investigated the runup of non-breaking waves, whereas, in contrast, little data is available on the runup of waves at the point of breaking prior to interaction with the opposing shore. In the present study, impulse waves were generated in a series of laboratory flume experiments by releasing a range of different slide source volumes of highly mobile slide material (water) into different reservoir depths, to observe the runup of breaking and non-breaking waves at the point of arrival at steep slopes ranging from 25° to 45°. Water surface characteristics including the maximum wave amplitude were measured using wave probes and digital imagery was obtained using high-speed cameras. The maximum runup, and the cross-slope variability in runup, of each wave was captured using hydrochromic paint, which changes colour on contact with water. The experimental results indicate that in the near-field the runup of breaking waves is dependent on the wave amplitude relative to the water depth, and is nearly independent of the slope angle. Statistical analysis of the runup observations for breaking and non-breaking waves indicate that the variability of runup across the width of the slope increases with increasing incident relative wave amplitude. These observations, combined with runup data from previous studies, are used to develop a new semi-empirical equation for the maximum runup of breaking and non-breaking waves. The formulation is valid over an extended range of relative wave amplitudes, relevant for near-field runup that has been documented in major field cases. The experimental observations in the present study provide, for the first time, a comprehensive dataset of runup for impulse waves involving breaking and no breaking on arrival at a slope.
机译:Landslide产生的波浪的速度是沿海地区的一个重要的自然危险,可能导致自然和建筑环境重大损坏。过去的工作已经调查了非破坏波的速度,而相比之下,在与相对的岸边相互作用之前,在破裂的角度下可以获得小的数据。在本研究中,通过将高移动滑动材料(水)的一系列不同的载玻片源体积(水)释放到不同的储层深度,在一系列实验室水槽实验中产生脉冲波,以观察突破和不断裂波的速度陡峭斜坡的到来点范围为25°至45°。使用波探针测量包括最大波幅的水面特性,使用高速摄像机获得数字图像。使用水红十码涂料捕获每波的最大流程和跑步的横向变化,从而改变了与水接触的颜色。实验结果表明,在近场中,断裂波的速度取决于相对于水深的波幅,并且几乎与倾斜角度不同。用于断裂和非断裂波的延伸观测的统计分析表明,随着入射相对波幅度的增加,斜率宽度的宽度的变化增加。这些观察结果与先前研究的运行数据相结合,用于开发一种新的半经验方程,以获得最大的破碎和非断裂波的速度。该配方在延长范围的相对波幅度范围内有效,对于在主要场地中被记录的近场运行相关。本研究中的实验观察是第一次提供跨越脉冲的脉冲综合数据集,涉及破坏的脉冲波,并且在距离抵达时不会破裂。

著录项

  • 来源
    《Oceanographic Literature Review》 |2021年第5期|1154-1154|共1页
  • 作者

  • 作者单位
  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号