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Application of frequency-domain helicopter-borne electromagnetics for groundwater exploration in urban areas

机译:频域直升飞机电磁在城市地下水勘探中的应用

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Airborne geophysical methods have been used successfully in groundwater exploration over the last decades. Particularly airborne electromagnetics is appropriate for large-scale and efficient groundwater surveying. Due to the dependency of the electrical conductivity on both the clay content of the host material and the mineralisation of the water, airborne electromagnetics is suitable for providing information on groundwater resources, water quality, aquifer conditions and protection levels. Frequency-domain helicopter-borne electromagnetic systems are used to investigate near-surface groundwater occurrences in detail even in rough terrain and populated areas. In order to reveal the subsurface conductivity distribution, the quantities measured, the secondary magnetic fields, are generally inverted into resistivity-depth models. Due to the skin-effect the penetration depths of the electromagnetic fields depend on the system characteristics used: high-frequency data describe the shallower parts of the conducting subsurface and the low-frequency data the deeper parts. Typical maximum investigation depths range from some ten metres (highly conductive saltwater saturated sediments) to several hundred metres (resistive hard rocks).In urban areas there are a number of man-made sources affecting the electromagnetic measurements. These effects on the secondary field values are discussed on the basis of synthetic data as well as uncorrected and corrected field data. The case histories of different hydrogeological setups in Indonesia, The Netherlands and Germany demonstrate that airborne electromagnetics can be applied to groundwater exploration purposes even in urban areas.
机译:在过去的几十年中,机载地球物理方法已成功用于地下水勘探。特别是机载电磁波适用于大规模高效的地下水测量。由于电导率既取决于基质材料的粘土含量又取决于水的矿化作用,因此机载电磁波适合于提供有关地下水资源,水质,含水层状况和保护水平的信息。频域直升飞机电磁系统用于详细调查近地面地下水的发生,即使在崎even的地形和人口稠密的地区也是如此。为了揭示地下电导率分布,通常将测得的量(次级磁场)转化为电阻率-深度模型。由于集肤效应,电磁场的穿透深度取决于所使用的系统特性:高频数据描述了导电地下的较浅部分,而低频数据则描述了较深的部分。典型的最大调查深度范围从几十米(高导电性盐水饱和沉积物)到几百米(电阻性硬岩石)。在城市地区,有许多人为干扰电磁测量的源。这些对次要字段值的影响将根据合成数据以及未校正和已校正的字段数据进行讨论。在印度尼西亚,荷兰和德国,不同水文地质条件的案例历史表明,机载电磁技术甚至可以用于城市地区的地下水勘探。

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