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首页> 外文期刊>International Journal of Geophysics >Environmental Geophysical Study of the Groundwater Mineralization in a Plot of the Cotonou Littoral Zone (South Benin)
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Environmental Geophysical Study of the Groundwater Mineralization in a Plot of the Cotonou Littoral Zone (South Benin)

机译:科托努沿海地区(南贝宁)某地块地下水矿化的环境地球物理研究

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摘要

Geophysical investigations comprising electrical resistivity and electromagnetic conductivities methods were deployed in a 350 m2sector, strewn with 11 wells. Within the framework of an environmental study on a small scale in the south of Benin, the water conductivity of these wells was measured to determine in a direct way mineralization of the coastal water table in the littoral zone. This environmental study aimed to prospect by the geophysical methods the space extension of the water table mineralization obtained by direct measurements of water conductivity in the well and the depth of the fresh water/salted water interface in the coastal aquifer. Electromagnetic measurements of conductivities made it possible to chart a gradient of mineralization in the northwest direction. The logs of vertical electric soundings showed a deepening of the fresh water/salted water interface in the southern part and its rupture in the northern part. The electrical resistivities of the interface are sensitive to the degree of its mineralization. It has been observed that the geophysical methods in electrical and electromagnetic prospection are a great contribution to the environmental study of the water table mineralization in the littoral zone for a sustainable management of the water resource.
机译:包括电阻率和电磁电导率方法在内的地球物理研究部署在一个350平方米的区域中,分布了11口井。在贝宁南部的小规模环境研究框架内,对这些井的水电导率进行了测量,以直接方式确定了沿海地区沿海水位的矿化作用。这项环境研究旨在通过地球物理方法来展望地下水位矿化的空间扩展,该空间扩展是通过直接测量井中水的电导率以及沿海含水层中淡水/咸水界面的深度来获得的。电导率的电磁测量使得绘制西北方向矿化梯度成为可能。垂直电测深表明,南部的淡水/咸水界面加深,而北部则破裂。界面的电阻率对其矿化程度敏感。已经观察到,电和电磁勘探中的地球物理方法对沿岸带地下水位矿化的环境研究做出了巨大贡献,以实现水资源的可持续管理。

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