首页> 外文期刊>Natural Hazards and Earth System Sciences Discussions >Brief communication: 3-D reconstruction of a collapsed rock pillar from Web-retrieved images and terrestrial lidar data – the 2005 event of the west face of the Drus (Mont Blanc massif)
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Brief communication: 3-D reconstruction of a collapsed rock pillar from Web-retrieved images and terrestrial lidar data – the 2005 event of the west face of the Drus (Mont Blanc massif)

机译:简要沟通:3-D从Web检索的图像和地面激光器数据的折叠岩柱重建 - 2005年的戏剧西面的活动(Mont Blanc Massif)

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In June 2005, a series of major rockfall events completely wiped out the Bonatti Pillar located in the legendary Drus west face (Mont Blanc massif, France). Terrestrial lidar scans of the west face were acquired after this event, but no pre-event point cloud is available. Thus, in order to reconstruct the volume and the shape of the collapsed blocks, a 3-D model has been built using photogrammetry (structure-from-motion (SfM) algorithms) based on 30 pictures collected on the Web. All these pictures were taken between September 2003 and May 2005. We then reconstructed the shape and volume of the fallen compartment by comparing the SfM model with terrestrial lidar data acquired in October 2005 and November 2011. The volume is calculated to 292?680?m3 (±5.6?%). This result is close to the value previously assessed by Ravanel and Deline (2008) for this same rock avalanche (265?000?±?10?000?m3). The difference between these two estimations can be explained by the rounded shape of the volume determined by photogrammetry, which may lead to a volume overestimation. However it is not excluded that the volume calculated by Ravanel and Deline?(2008) is slightly underestimated, the thickness of the blocks having been assessed manually from historical photographs.
机译:2005年6月,一系列主要岩石活动完全擦掉了位于传奇德鲁斯西脸(Mont Blanc Massif,France)的Bonatti Parkar。在此活动之后获得了西面的陆地激光乐队扫描,但没有比例点云可用。因此,为了重建折叠块的体积和形状,基于在网上收集的30张图像,使用摄影测量(结构 - 来自运动(SFM)算法)构建了3-D模型。所有这些图片都在2003年9月和2005年5月之间采取了所有这些照片。然后我们通过将SFM模型与2005年10月和2011年11月的地面激光雷达数据进行比较来重建堕落的隔间的形状和体积。该体积计算为292?680?M3 (±5.6?%)。此结果接近以前由Ravanel和德雷(2008)评估的值为同一岩石雪崩(265?000?±10?000?M3)。这两个估计之间的差异可以通过摄影测量法确定的体积的圆形形状来解释,这可能导致体积高估。然而,不排除由拉凡尔和德雷计算的体积略微低估,从历史照片中手动评估块的厚度。

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