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Landslide monitoring using multitemporal terrestrial laser scanning for ground displacement analysis

机译:使用多时相地面激光扫描进行滑坡监测以进行地表位移分析

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In the analysis of the temporal evolution of landslides and of related hydrogeological hazards, terrestrial laser scanning (TLS) seems to be a very suitable technique for morphological description and displacement analysis. In this note we present some procedures designed to solve specific issues related to monitoring. A particular attention has been devoted to data georeferencing, both during survey campaigns and while performing statistical data analysis. The proper interpolation algorithm for digital elevation model generation has been chosen taking into account the features of the landslide morphology and of the acquired datasets. For a detailed analysis of the different dynamics of the hillslope, we identified some areas with homogeneous behaviour applying in a geographic information system (GIS) environment a sort of rough segmentation to the grid obtained by differentiating two surfaces. This approach has allowed a clear identification of ground deformations, obtaining detailed quantitative information on surficial displacements. These procedures have been applied to a case study on a large landslide of about 10 hectares, located in Italy, which recently has severely damaged the national railway line. Landslide displacements have been monitored with TLS surveying for three years, from February 2010 to June 2012. Here we report the comparison results between the first and the last survey.
机译:在分析滑坡的时间演变和相关的水文地质灾害时,地面激光扫描(TLS)似乎是非常适合进行形态描述和位移分析的技术。在本说明中,我们介绍了一些旨在解决与监视有关的特定问题的过程。在调查活动期间和进行统计数据分析时,都特别关注数据地理配准。考虑到滑坡形态和采集的数据集的特征,选择了合适的数字高程模型生成插值算法。为了详细分析山坡的不同动态,我们确定了一些行为均一的区域,这些区域在地理信息系统(GIS)环境中应用了一种通过区分两个表面而对网格进行的粗略分割。这种方法可以清楚地识别地面变形,获得有关表面位移的详细定量信息。这些程序已应用于一个案例研究,该案例位于意大利大约10公顷的大型滑坡上,该滑坡最近严重破坏了国家铁路线。从TLS调查开始,从2010年2月到2012年6月对滑坡位移进行了三年的监测。在这里,我们报告了第一次和最后一次调查之间的比较结果。

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