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Integrating GPR and EMI to three-dimensionally reconstruct a WW I training trench at Stonehenge

机译:将GPR和EMI整合到三维地重建了巨石阵的WW I训练沟

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Given the upcoming centennial commemoration of the beginning of the Great War (WW I), the international attention for this conflict grows considerably. Questions will be raised about the nature of this heritage. In this study, we focus on a WW I training trench which was built in the Stonehenge (UK) World Heritage landscape where no fighting took place. Frequency-domain GPR and multi-receiver EMI were used to characterize this trench network in 3-D. The GPR measurements showed the trench infillings as strong reflections contrasting with the surrounding loess-chalk soil. However, converting the two-way travel times to absolute depths requires knowledge of the relative permittivity ε. Due to the impossibility to perform invasive observations in this protected landscape, we developed a procedure to integrate the GPR measurements with EMI magnetic susceptibility (κ) measurements. A fitting procedure allowed to estimate both the of the trench infilling and the surrounding soil material, and the ε of the material above and within the trench. This rendered absolute depth values to the GPR reflection data, improving the exact characterization of the trench system. Moreover, these results allowed to obtain depth-slices from EMI κ data. So integrating both GPR and EMI measurements enabled the 3-D reconstruction of the buried trench network.
机译:鉴于伟大战争开始的即将纪念(WW I),这种冲突的国际关注大大增长。关于这一遗产的性质将提出问题。在这项研究中,我们专注于WW I训练沟,建于巨石阵(英国)世界遗产,没有战斗。频域GPR和多接收器EMI用于在3-D中表征该沟槽网络。 GPR测量显示沟槽潜水,作为与周围黄土粉笔土壤对比的强烈反射。但是,将双向行程时间转换为绝对深度需要了解相对介电常数ε。由于在这种受保护的景观中执行侵入性观测的不可能,我们开发了一种将GPR测量与EMI磁性敏感(κ)测量集成的程序。允许允许沟槽infilling和周围土壤材料的两个和沟槽内部的ε的拟合程序。这将绝对深度值呈现给GPR反射数据,从而提高了沟槽系统的精确表征。此外,这些结果允许从EMIκ数据获得深度切片。因此,整合GPR和EMI测量使得掩埋沟槽网络的三维重构能够重构。

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