Photogrammetric rockfall monitoring in Alpine environments using M3C2 and tracked motion vectors

Lukas Lucks , Uwe Stilla , Ludwig Hoegner , Christoph Holst
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引用次数: 0

Abstract

This paper introduces methods for monitoring rock slope movements in Alpine environments based on terrestrial images. The first method is a photogrammtric point cloud-based deformation analysis, relying on M3C2. Although effective in identifying large changes, the method has a tendency to underestimate smaller-scale movements. A feature-based method is presented to address this limitation, using SIFT features to track keypoints in images from different epochs. These automatically detected 3D vectors offer high spatial density and enable small-scale movement detection in the order of a few millimeters. The results are incorporated into a deformation analysis that allows statistically based conclusions about the ongoing movements. The workflow relies on georegistration using Ground Control Points. To investigate the possibility of avoiding these points, a registration method based on the ICP algorithm and M3C2 is tested. The study utilizes data from an active landslide site at Hochvogel Mountain in the Alps, analyzing changes and deformations from 2018 to 2021, revealing an average motion of 75 mm.

利用 M3C2 和跟踪运动矢量对阿尔卑斯环境中的落石进行摄影测量监测
本文介绍了基于地面图像监测阿尔卑斯环境中岩石斜坡移动的方法。第一种方法是基于 M3C2 的摄影点云变形分析。这种方法虽然能有效识别大的变化,但往往会低估较小范围的移动。为了解决这个问题,我们提出了一种基于特征的方法,利用 SIFT 特征来跟踪不同年代图像中的关键点。这些自动检测到的三维矢量具有很高的空间密度,能够检测到几毫米量级的小范围移动。检测结果将被纳入变形分析,从而对正在发生的运动得出基于统计的结论。工作流程依赖于使用地面控制点进行的地理注册。为了研究避开这些点的可能性,测试了一种基于 ICP 算法和 M3C2 的注册方法。该研究利用阿尔卑斯山霍赫沃格尔山活动滑坡点的数据,分析了 2018 年至 2021 年的变化和变形,发现平均运动量为 75 毫米。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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CiteScore
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