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首页> 外文期刊>Journal of African Earth Sciences >Geochemical modeling of the hydrogeochemical processes affecting groundwater quality of the Eocene aquifer east of El Minia Governorate -Eastern desert - Egypt
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Geochemical modeling of the hydrogeochemical processes affecting groundwater quality of the Eocene aquifer east of El Minia Governorate -Eastern desert - Egypt

机译:影响El Minia Governorate Eastern Desert - Egypers - Eocenia Aquifer地下水质量的地球化学建模

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The Eocene limestone aquifer represents a renewable source of groundwater that can be used to enhance the sustainable agriculture at the eastern desert fringes of El Minia Governorate. The current research aims to investigate quantitatively the physicochemical processes which control the chemical composition of groundwater extracted from the Eocene aquifer using the PHREEQC code. The total dissolved solids of the Eocene groundwater range from 453 to 1903 mg/1 indicating fresh to slightly brackish water quality. The simulation of the double mixing between rain (or Nile) water with Nubian water reveal that rain or Nile water contribution by 50% or more to the Eocene limestone aquifer system can explain the chemical composition of most groundwater samples of the Eocene aquifer. This means that the contribution from rain or Nile water infiltration to the Eocene aquifer is much more important than upward leakage from the underlying Nubian sandstone aquifer. The triple mixing processes simulation indicate also that the most effective end members of mixing are found to be rain and Nile waters, with some contribution from the groundwater encountered at the Nubian sandstone aquifer. The evaporation of 75%-95% of rain or Nile water explain the chemical content of most water samples which imply that evaporation is a dominant physicochemical process at East of El Minia area due to the elevated air temperature and the exploitation of groundwater at relatively shallow depths. The results of the current geochemical modeling study indicates that there are processes other than evaporation and mixing which affect the groundwater quality of the Eocene aquifer (such as carbonate and sulfate minerals dissolution). Finally, the usage of PHREEQC code in the quantitative assessment of the Eocene aquifer can be applied for similar aquifers and areas surrounding the Nile Valley Region in Egypt. This region comprises six governorates (Beni Suef, El Minia, Assiut, Sohag Qena and Aswan) where 40% of the population of Egypt live.
机译:虫族石灰石含水层代表了可再生地下水来源,可用于增强El Minia省东部沙漠格林的可持续农业。目前的研究旨在定量地调查使用Phreeqc码从何种世界中提取的地下水化学组成的物理化学方法进行调查。何世肾上腺地下水的总溶解固体为453至1903mg / 1,表明新鲜为略带脆的水质。雨水(或尼罗河)水与Nubian水之间的模拟表明,血液石灰石含水层系统的雨或尼罗水贡献50%以上,可以解释各种地下水样本的化学成分。这意味着雨或尼罗水浸染到何种含水层的贡献比底层Nubian砂岩含水层的向上泄漏更重要。三重混合过程模拟表明,发现混合的最有效的最终成员是雨水和尼罗河水域,以及在Nubian砂岩含水层遇到的地下水的一些贡献。 75%-95%的雨或尼罗水的蒸发解释了大多数水样的化学含量,这意味着由于升高的空气温度和对地下水的开采,蒸发是El Minia面积的主要物理化学过程。深度。目前地球化学建模研究的结果表明,存在除蒸发和混合之外的过程,影响何种血液含水层的地下水质量(如碳酸盐和硫酸盐矿物溶解)。最后,Phreeqc代码在埃及尼罗河谷地区周围的类似含水层和地区的使用情况。该地区包括六个省(Beni Suef,El Minia,Assiut,Sohag Qena和Aswan),其中40%的埃及人口。

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