埃及东埃尔米尼亚省中始新世灰岩含水层的多元统计和视觉模型水文地球化学评价

Abdel-Aziz A. Abdel-Aziz, Alaa Mostafa, Salman A. Salman, Ramadan S. A. Mohamed, Esam A. Ismail
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引用次数: 0

摘要

东米亚被认为是最有希望建立许多可持续发展项目的地区之一。中始新世灰岩含水层是这些工程建设所需的主要水源。因此,从不同的井中采集32个样本,进行化学分析,确定该水是否适合饮用和灌溉,并通过水化学图的应用和统计分析,提到控制水质的各种因素。研究水样的TDS值为271 ~ 2328 ppm,表明近93.8%的研究水样可用于饮用;总硬度值为32.19 ~ 1035.44,表明93.8%的研究水样可用于生活。统计分析、Gibbs图和End-member图表明,除人为活动外,水岩相互作用、地球化学过程(氧化还原)是地下水化学成分的主要影响因素。因此,根据计算的钠危害和盐度,所研究的水适合灌溉。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Hydrogeoochemical Evaluation Of Middle Eocene Limestone Aquifer Using Multivariate Statistics And Visual Models, East El Minia Governorate, Egypt
East Minia is considered as one of the most promising areas for the establishment of numerous sustainable development projects. The Middle Eocene Limestone aquifer is the main water source needed for the establishment of these projects. Therefore, 32 collected samples from different wells and chemically analyzed to determine the suitability of that water for drinking and irrigation, as well as mentioned to the various factors controlling the water quality through the application of hydrochemical diagrams and statistical analysis. TDS value of the studied water samples was ranged from 271 to 2328 ppm which indicates that nearby is 93.8% of the investigated water samples are acceptable for drinking uses, while total hardness value ranged from 32.19 to 1035.44 which indicates that there is 93.8% of the studied groundwater samples are suitable for domestic uses. Statistical analyses, Gibbs and End-member diagrams indicate that the water-rock interactions, geochemical process (Redox), besides anthropogenic activities are the essential contributor to the investigated groundwater chemical composition. Thus, the studied water is suitable for irrigation purposes based on the calculated sodium hazards and salinity.
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