Groundwater exploration in fissured media with electrical and VLF methods

J. Bernard, P. Valla
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引用次数: 58

Abstract

Direct current electrical methods are among the most popular tools for groundwater exploration, in both porous and fissured media. In the case of fissured media, the areas most favourable to the presence of water are selected according to the minima of apparent resistivity values measured at the surface, the alteration and fissuration making the resistivity of rocksto decrease. VLF methods, which are less used than the previous ones because their depth of investigation is more limited, permit location of conductive zones through an electromagnetic induction process.

In order to improve the groundwater field surveys as much as possible, BRGM has been developing easy-to-use instruments with automatic measurement process, automatic computation of geophysical parameters (apparent resistivity) and digital storage of data. Hence, SYSCAL-R1 and R2 resistivity meters and SYSCAL-VLF and T-VLF electromagnetic instruments have been designed. The newly developed T-VLF receiver has the advantage of not requiring any specific orientation of the operator with respect to the direction of the antenna.

Several cases histories of groundwater exploration with electrical and VLF methods in fissured media are presented in various geological backgrounds:

  • &#x02022;

    - groundwater exploration in Botswana, in fissured dolomites, with resistivity maps (electrical profiling);

  • &#x02022;

    - village groundwater project in Burkina Faso, in crystalline basement, with resistivity profiling and VLF (tilt angle mode);

  • &#x02022;

    - village groundwater project in Togo, in crystalline basement, with resistivity mapping (gradient array);

  • &#x02022;

    - finally, methodological study in France, in a granitic basement, with the comparison of anomalies obtained by electrical profilings (one station and two station arrays) and by VLF profilings (in the tilt angle and in the resistivity modes).

Although the rate of success cannot be guaranteed (which yield can be obtained for a given conductive anomaly?), the DC and VLF classical methods are efficient tools for borehole siting in groundwater exploration: the new measuring instruments should make them still more cost effective.

电法和甚低频法在裂隙介质中勘探地下水
无论是在多孔介质还是裂隙介质中,直流电法都是地下水勘探中最常用的工具之一。在裂隙介质的情况下,根据在地表测量的视电阻率值的最小值选择最有利于水存在的区域,蚀变和裂隙使岩石的电阻率降低。VLF方法可以通过电磁感应过程确定导电区域的位置,由于其调查深度受到限制,因此比以前的方法使用较少。为了最大限度地提高地下水野外调查水平,BRGM开发了具有自动测量过程、自动计算地球物理参数(视电阻率)和数据数字化存储的易用仪器。为此,设计了SYSCAL-R1和R2电阻率仪以及SYSCAL-VLF和T-VLF电磁仪表。新开发的T-VLF接收机的优点是不需要操作员相对于天线方向的任何特定方向。介绍了在不同地质背景下,利用电法和甚低频法在裂隙介质中进行地下水勘探的几个历史实例:• • • • • • • • • • • • • • • •-最后,在法国的花岗岩基底进行方法研究。将电剖面(单站和双站阵列)和VLF剖面(倾角和电阻率模式)得到的异常进行比较。虽然成功率不能保证(对于给定的导电异常,可以获得多少产量?),但直流和VLF经典方法是地下水勘探中钻孔定位的有效工具:新的测量仪器应该使它们更具成本效益。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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