地球物理和摄影测量勘探揭示的12世纪教堂的耳堂基础

C. Fauchard, L. Aillaud, A. Legrand, R. Antoine, V. Guilbert, C. Ledun, B. Beaucamp
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引用次数: 0

摘要

本研究介绍了在位于索特维尔滨海(诺曼底,法国)的圣母院-杜-瓦尔教堂进行的工作。当地政府正在考虑修复工作,并要求对周围环境进行地球物理调查。首先,无人机的航空摄影产生了教堂外部的运动结构(SfM)模型,由3D内部模型完成。地球物理勘探就是利用探地雷达(GPR)和电阻率成像(ERI)对周围浅层进行成像。GPR测量清楚地显示了教堂两侧的前斜面,对应的透射体与3D室内摄影测量模型中可见的填充开口的存在完全一致。ERI测量强调了一个非常具有电阻性的基底的存在,可能与当地建造教堂的白垩地层相对应。此外,电阻地层强调了用于支持过境会议的潜在土方工程,与GPR信号相关。一些探地雷达和ERI异常没有得到解释,值得更深入的调查:考古发掘仍然是确认其性质的唯一解决办法。在摄影测量模型内的恢复允许非常明确地显示结果,将教堂的建筑和地球物理测量相结合。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Transept Foundations of a 12th Century Chapel Revealed by Geophysical and Photogrammetric Prospection
Summary This study presents the work carried out at the Notre-Dame-du-Val chapel located in Sotteville-sur-Mer (Normandy, France). Local authorities are considering restoration work and have requested a geophysical survey of the surroundings. First, aerial photography by drone yields a Structure from Motion (SfM) model of the exterior of the chapel, completed by a 3D interior model. Geophysical prospecting consists in imaging shallow surface of surroundings, with help of Ground Penetrating Radar (GPR) and Electrical Resistivity Imaging (ERI). GPR measurements clearly reveal former apses on both sides of the chapel, corresponding to the transepts meets in perfect agreement with the presence of filled-in openings visible in the 3D interior photogrammetric model. The ERI measurements underline the presence of a very resistive substratum, probably corresponding to the local chalky formation where the chapel was built. Besides, resistive formation underlines the potential earthworks carried out to support the transepts meets, correlated with GPR signals. Several GPR and ERI anomalies have not been interpreted and deserve deeper investigation: archaeological excavations remains the only solution to confirm their nature. The restitution within the photogrammetric model allows a very explicit display of the results, integrating the architecture of the chapel and geophysical measurements.
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