论文标题
通过摄影测量法重建“ Azure窗口”自然拱
Reconstruction of the collapse of the 'Azure Window' natural arch via photogrammetry
论文作者
论文摘要
Azure窗户是位于戈佐(Gozo)西海岸(马耳他群岛)西海岸的天然拱门,该拱门于2017年3月倒塌。我们采用了潜水员推进车辆安装的相机系统来捕获通过摄影测量法进行此倒塌的拱门的3D模型的数据。我们证明了使用这种方法来记录大面积区域中复杂的水下地貌学,并根据此3D模型对现场进行地貌评估和崩溃事件。该方法可以重建和理解崩溃事件。由于获得的高分辨率,我们能够将主要淹没的组件与其倒流前的位置进行交叉匹配;这使人们可以了解崩溃的动力学,确认沿现有关节的岩石破裂,并绘制塌陷事件中岩石和碎屑的分布。我们得出的结论是,在柱子底部的Azure窗口崩溃的关键阶段,导致后者沿西南方向倒塌,分为两个主要部分,这些部分沿着岩性边界分离。我们还发现明确的证据表明,支柱的某些部分遵循预先存在的关节。桥梁在支撑支撑失去支撑后垂直倒塌,分为两个主要组成部分和许多其他碎片。我们还记录了爆发后现场的进一步更改。我们表明,即使自崩溃以来已经过去了很长时间,这种方法也可以用于理解和表征此类事件,并且岩石已经发生了侵蚀和大量的海洋生长。
The Azure Window was a natural arch situated in the west coast of Gozo (Maltese Archipelago) that collapsed in March 2017. We employ a Diver Propulsion Vehicle-mounted camera system to capture data for the 3D-modelling of this collapsed arch via photogrammetry. We demonstrate use of this method to document complex underwater geomorphology spread across a large area, and draw up a geomorphic assessment of the site and collapse event on the basis of this 3D-model. The methodology enables a reconstruction and understanding of the collapse event. On account of the high-resolution attained, we are able to cross-match the principal submerged components with their pre-collapse location; this enables an understanding of the dynamics of the collapse, confirmation of rock break-up along existing joints, and mapping the distribution of the rock and debris from the collapse event. We conclude that the key stages in the collapse of the Azure Window entailed erosion at the base of the pillar, leading to the latter's collapse in the southwest direction, breaking into two main sections that separated along the lithological boundary. We also find clear evidence that separation of some sections of the pillar followed pre-existing joints. The bridge collapsed vertically upon loss of support from the pillar, breaking into two main components and many other fragments. We also document further changes at the site post-collapse. We show that this approach can be utilised to understand and characterise such events even when significant time has elapsed since collapse, and rocks have already undergone erosion and significant marine growth.