利用电阻率层析成像法对加纳沿海的盐度进行横向和纵向测绘:以中部地区为例

Albert Asare , Emmanuel K. Appiah-Adjei , Frederick Owusu-Nimo , Bukari Ali
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引用次数: 0

摘要

海水入侵沿海含水层是一个世界性的问题,对沿海大多数社区的水质造成了挑战,并促使人们对其发生、来源和年龄进行了许多研究。然而,在评估沿海含水层地下水管理问题的空间分布时,仍然存在一个重大挑战。因此,本研究采用电阻率断层扫描技术来描绘加纳中部地区约13个沿海社区的盐度横向和垂直分布。在多电极ABEM隆德成像系统的帮助下,沿着从海岸线到社区的选定通道进行了多梯度阵列技术的调查。根据调查数据生成的二维电阻率伪剖面显示,受下伏当地地质和海水入侵的影响,每个群落内都有独特的电阻率分布。低电阻率层(<50 Ωm),可能与咸水饱和的地质构造有关,在几乎所有调查的浅层和较深的群落中都观察到。该研究还表明,海水入侵已经对社区的淡水含水层造成了超过5公里的内陆影响,需要加以解决。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Lateral and vertical mapping of salinity along the coast of Ghana using Electrical Resistivity Tomography: The case of Central Region

Seawater intrusion into coastal aquifers is a worldwide problem causing water quality challenges in most communities along the coast, and has prompted many investigations into its occurrence, sources and age. However, there is still a major challenge when it comes to evaluating the spatial distribution of the problem in coastal aquifers towards groundwater management. Therefore, this study has employed electrical resistivity tomography technique to delineate both the lateral and vertical distribution of the salinity within some thirteen coastal communities in the Central Region of Ghana. The survey was conducted using the multiple-gradient array technique with the aid of a multi-electrode ABEM Lund Imaging System along selected traverses from the coastline into the communities. 2-D resistivity pseudo-sections generated from the survey data showed a unique resistivity distribution within each community, influenced by the underlying local geology and seawater intrusion. Low resistivity layers (< 50 Ωm), which may be associated with saline water saturated geologic formations, are observed within almost all the communities investigated at both shallow and deeper depths. The study also revealed that, seawater intrusion has affected freshwater aquifers in the communities by more than 5 km in-land from the sea and need to be tackled.

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