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Monitoring of displacement evolution during the pre-failure stage of a rock block using ground-based radar interferometry

机译:使用地基雷达干涉法监测岩块预破坏阶段的位移演变

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摘要

As a typical abrupt geological hazard, rockfalls are widely distributed and occur frequently. It is often difficult to predict the occurrence, and therefore record and monitor the whole failure process of rockfalls. In this study, with the combined use of terrestrial laser scanning (TLS) and ground-based radar interferometry (GB-InSAR) technologies, a typical small collapse in the Hongshiyan post-earthquake rock slope was monitored. An accurate TLS three-dimensional (3D) rock slope model of the study area was established with high-resolution geometry and morphology information, the discontinuity sets and their orientations and distributions were visually identified and analyzed by means of an automatic discontinuity identification algorithm. A perspective view of the whole dynamic failure process of the small collapse was achieved; the displacement behavior during critical sliding stage was revealed by integrating the high-accuracy (millimetric) GB-InSAR monitoring results into the TLS 3D model. It can be used for a complete analysis of the failure behavior and stability assessment of the rock slope during a phase of emergency. The unstable rock block on the slope exhibited a rapid growth of displacement. The dynamic failure process of the rock block underwent three obvious accelerating periods. There was a correspondence between the spatial expansion of the moving area and the process of cracking propagation of rock bridges. The stability of the perilous rock above the tafoni was controlled by the connectivity of rock bridges. Thanks to monitoring, early warning and preventive measure were taken, which avoided a possible undesirable event. This typical case study can provide a reference for the monitoring of an unstable rock slope and the understanding of the evolution of rock block kinematics before collapse.
机译:作为典型的突然地质危害,岩石普遍分布并经常发生。通常难以预测发生,因此记录和监控岩石的整个故障过程。在这项研究中,随着陆地激光扫描(TLS)和地面雷达干涉学(GB-Insar)技术的结合使用,监测了洪夏岩后岩石岩坡中典型的小塌陷。通过高分辨率几何和形态信息建立了研究区域的精确TLS三维(3D)摇滚模型,通过自动不连续的识别算法目视识别和分析不连续组及其取向和分布。实现了小崩溃的整个动态故障过程的透视图。通过将高精度(毫米)GB-Insar监测结果集成到TLS 3D模型中,揭示了临界滑动阶段的位移行为。它可用于在紧急状态期间完全分析岩坡的故障行为和稳定性评估。斜坡上的不稳定岩石块表现出膨胀的快速增长。岩石块的动态故障过程介绍了三个明显的加速期。移动区域的空间膨胀与岩石桥梁裂缝的过程之间存在对应关系。 Tafoni上方的危险岩石的稳定性由岩石桥的连接控制。由于监测,采取了预警和预防措施,避免了可能的不良事件。这个典型的案例研究可以为监测不稳定的岩石坡度的监测以及理解崩溃前岩石运动学演变的参考。

著录项

  • 来源
    《Landslides》 |2019年第9期|共10页
  • 作者单位

    Sichuan Univ State Key Lab Hydraul &

    Mt River Engn Chengdu 610065 Sichuan Peoples R China;

    Sichuan Univ Coll Water Resource &

    Hydropower Chengdu 610065 Sichuan Peoples R China;

    Sichuan Univ State Key Lab Hydraul &

    Mt River Engn Chengdu 610065 Sichuan Peoples R China;

    Sichuan Univ Coll Water Resource &

    Hydropower Chengdu 610065 Sichuan Peoples R China;

    Sichuan Univ State Key Lab Hydraul &

    Mt River Engn Chengdu 610065 Sichuan Peoples R China;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 崩塌;
  • 关键词

    GB-InSAR technology; TLS; Rock collapse; Monitoring; Dynamic failure process;

    机译:GB-Insar技术;TLS;岩石崩溃;监测;动态故障过程;

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