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首页> 外文期刊>Journal of African Earth Sciences >Geophysical demonstration of the absence of correlation between lineaments and hydrogeologically usefull fractures: Case study of the Sanon hard rock aquifer (central northern Burkina Faso)
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Geophysical demonstration of the absence of correlation between lineaments and hydrogeologically usefull fractures: Case study of the Sanon hard rock aquifer (central northern Burkina Faso)

机译:地貌与水文地质有用裂缝之间不存在相关性的地球物理证明:Sanon硬岩含水层(布基纳法索中北部)的案例研究

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摘要

The conceptualization of hard rock aquifers in terms of their geometry and structure has undergone considerable progress over the last two decades. Despite these advances, hydrogeologists are still divided by the models used to describe two central concepts: (i) the influence of weathering processes on hydraulic conductivity; (ii) the influence of tectonics on the hydraulic conductivity of hard rock aquifers. In order to provide further insight into this debate, the present study proposes a conceptual model for hard rock aquifers, based on an integrated hydrogeological and geophysical approach, using information acquired at different scales. The data and observations used for this case study were derived from the Sanon experimental site, located in Burkina Faso, which is presently exposed to a Sudano-Sahelian climate.
机译:在过去的二十年中,硬岩含水层在几何形状和结构方面的概念化已经取得了长足的进步。尽管取得了这些进展,但水文地质学家仍被用于描述两个中心概念的模型所划分:(i)风化过程对水力传导率的影响; (ii)构造对硬岩含水层水力传导率的影响。为了提供对此辩论的进一步了解,本研究提出了一种硬岩含水层的概念模型,该模型基于综合的水文地质和地球物理方法,使用了在不同规模下获得的信息。用于此案例研究的数据和观察结果来自布基纳法索的Sanon实验点,该实验点目前处于Sudano-Sahelian气候中。

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