Using hydrogeochemical and geographic information system methods as an environmental approach for evaluating of coastal aquifers in west northern coast of Egypt

Mahmoud Elazhary, H. Sabet, A. A. Abu Khatita, Ahmed Shehata, Soheir T. El-Hemamy
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Abstract

The objective of the current investigation is to get sufficient understanding of the groundwater's geochemical peculiarities and its quality at the area of Egypt's coastline in the northwest. 14 Samples of groundwater have been gathered from 14 wells in various sections of the investigation region, and examined. The pH level within the samples of groundwater reflecting slightly alkaline nature while salinity varies widely from slightly, moderately to very saline water. The spatial distributions of the major ions, except HCO 3− demonstrate an overall increase in the center of the region being researched while HCO 3 − increases in the direction of the northwest (Ghemama area). The major cations in the samples of groundwater decrease in the following order: Na + > Ca 2+ > Mg 2+ > K + while the major anions following order: Cl − > SO 42− > HCO 3− . The spatial distribution of studied heavy metals decrease toward center of the area being researched and slightly increase toward east, and west which could be brought on by local human influence. The heavy metals that were examined for the samples of groundwater can be ordered as follow, Zn > Ba > As > Pb > Ni > Cd > Co > Mn > Cr > Cu. Based on Piper and Schoeller diagram, the samples of groundwater reflect the marine origin. An evaluation quality of the water for the purposes of irrigation and drinking reveals that the samples of groundwater in the research region are not appropriate for irrigation and drinking. Where the concentrations of Cd, Pb and As in the samples of groundwater reveal higher values than those advised by Egyptian and Worldwide Health Organization. Those increased concentrations may be attributed to agrochemical effects and human activities in the research area.
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利用水文地球化学和地理信息系统方法对埃及北部西部海岸含水层进行环境评价
本次调查的目的是充分了解埃及西北部海岸线地区地下水的地球化学特性及其质量。从调查区不同地段的14口井中采集了14份地下水样本,并进行了检测。地下水样本内的pH值反映了微碱性,而盐度则从微盐水、中度盐水到极盐水变化很大。除hco3−外,主要离子的空间分布在研究区域的中心呈整体增加趋势,而hco3−在西北方向(Ghemama地区)呈增加趋势。地下水样品中主要阳离子的减少顺序为Na + > ca2 + > Mg 2+ > K +,主要阴离子的减少顺序为Cl−> so42−> hco3−。研究区重金属的空间分布呈向中心减小、向东、向西小幅增大的趋势,这可能是受局地人为影响所致。地下水样品中重金属含量为Zn > Ba > as > Pb > Ni > Cd > Co > Mn > Cr > Cu。根据Piper和Schoeller图,地下水样品反映了海洋来源。通过对研究区灌溉饮用水水质的评价,发现该区地下水样品不适合灌溉饮用。地下水样本中Cd、Pb和As的浓度高于埃及和世界卫生组织建议的值。这些浓度的增加可归因于研究地区的农用化学品效应和人类活动。
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