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The combined use of radio-frequency electromagnetics and radiomagnetotellurics methods in non-ideal field conditions for delineating hydrogeological boundaries and for environmental problems

机译:在非理想场条件下结合使用射频电磁学和无线电电磁学方法来划定水文地质边界和解决环境问题

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摘要

Radio frequency geophysical methods are known for being very versatile tools in ground- and groundwater investigation at shallow depths. They are fast and easy to use and allow a high density of information over large surfaces, which makes them very suitable for geological mapping sensu lato (faults, lithological contacts, groundwater-bearing structures, vulnerability maps, and contaminant plumes) and for selecting borehole locations. Significant improvement concerning 2D and 3D modelling of the data has occurred in recent decades. However, field surveys are very seldom performed in “ideal conditions”—the lack of necessary transmitters, in the convenient direction, in order to catch the structures in E- and H-pol for modelling purposes, is not an unusual situation. The present paper shows how the use of RMT and RF-EM is nevertheless of great help and suggests different ways to explore qualitative data in different geological settings.
机译:众所周知,射频地球物理方法是用于浅层地下水和地下水调查的通用工具。它们快速,易于使用,并能在较大的表面上提供高密度的信息,这使其非常适用于地质地图绘制(断层,岩性接触,地下水结构,脆弱性图和污染物羽流)以及选择井眼位置。在最近的几十年中,有关2D和3D数据建模的重大改进已经出现。但是,很少在“理想条件”下进行现场勘测-在方便的方向上缺少必要的发射器以捕获E-和H-pol中的结构以进行建模并非罕见的情况。本文显示了如何使用RMT和RF-EM仍然有很大帮助,并提出了在不同地质环境中探索定性数据的不同方法。

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