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首页> 外文期刊>Natural hazards and earth system sciences >Brief communication: 3-D reconstruction of a collapsed rock pillar fromWeb-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 fromWeb-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:三维重建折叠岩石柱从Web检索的图像和地面激光乐节数据 - 2005年的DRUS西面脸(MONT BLANK MASSIF)

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摘要

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 680m3 (+/- 5.6 %). This result is close to the value previously assessed by Ravanel and Deline (2008) for this same rock avalanche (265 000 +/- 10 000m(3)). 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,一系列主要岩石事件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地面裂变扫描,但没有先前的点云。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 - 从动作(SFM)算法)建立了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。然后,我们通过将SFM模型与2005年10月和2011年10月收购的地面激光雷达数据进行比较来重建堕落隔间的形状和体积。该体积计算为292 680M3(+ / - 5.6%)。此结果接近以前由Ravanel和Deline(2008)评估的值为同一岩石雪崩(265000 +/- 10 000米(3))。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,没有排除在ravanel和德雷(2008)计算的音量略微低估,从历史照片中手动评估块的厚度。

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