首页> 外文期刊>Arabian journal of geosciences >Effect of the groundwater contribution, the climatic change, and the human-induced activities on the hydrological behavior of discharge playas: A case study Sidi El Hani discharge playa, Tunisian Sahel
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Effect of the groundwater contribution, the climatic change, and the human-induced activities on the hydrological behavior of discharge playas: A case study Sidi El Hani discharge playa, Tunisian Sahel

机译:地下水贡献,气候变化和人为活动对排泄滩水文行为的影响:以突尼斯萨赫勒地区的Sidi El Hani排泄滩为例

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摘要

This study is meant to provide an insight into how discharge playas, which are strongly influenced by a regional salty groundwater flow regime, such as the discharge playa of Sidi El Hani, would respond to the climatic variability and to the materials coming from the subsurface of the Sahel area. In order to choose the appropriate method, a special care was given in this paper to different methods of investigation of the groundwater contribution in water and salt budgets of saline systems. The hydrogeological map of the surrounding aquifers proved their convergence toward Sidi El Hani discharge playa. As consequence of the dominance of a salty groundwater contribution, the climate variability may be considered minor. Accordingly, the model proposed by this study showed the dominance of the salty water coming from the hydrogeology at the expense of the fresh water coming from the climatic contribution. Moreover, according to the adopted model, the effect of the human-induced activity on the hydrogeological contribution such as the installation of dams in the Tunisian center and the overexploitation of the phreatic aquifer of Kairouan was judged increasing the convergence of Kairouan aquifer towards Sidi El Hani discharge playa. On the other hand, the consumption of salt reserves from the discharge playa tends to decrease its salinization.
机译:这项研究旨在提供洞察力,该办法受到了区域咸地下水流机制的强烈影响,例如西迪·哈尼(Sidi El Hani)的排放法,将如何应对气候变化和来自地下亚热带的物质。萨赫勒地区。为了选择合适的方法,本文特别注意了调查盐分系统中水和盐分预算中地下水贡献的不同方法。周围含水层的水文地质图证明了它们向西迪哈尼排放滩的趋同。由于咸水对地下水的贡献占主导地位,气候变化可能被认为是微小的。因此,这项研究提出的模型表明,来自水文地质学的咸水占优势,而来自气候贡献的淡水则占优势。此外,根据采用的模型,可以判断人为活动对水文地质贡献的影响,例如在突尼斯中心安装水坝和对凯鲁万潜水地带的过度开发,从而增加了凯鲁万含水层向西迪埃伊的收敛性。哈尼排出普拉亚。另一方面,从排出普拉亚盐中消耗盐储备趋于降低其盐碱化。

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