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Recharge and contamination sources of shallow and deep groundwater of pleistocene aquifer in El-Sadat industrial city: isotope and hydrochemical approaches

机译:萨达特工业城市更新世含水层浅层和深层地下水的补给和污染源:同位素和水化学方法

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Hydrochemical and isotopic researches were conducted in El-Sadat City groundwater system to identify groundwater alteration, recharge, residence time and extent of pollution. The groundwater salinity gradually increases as the groundwater moves from northeastern to southwestern parts of the city. Groundwater generally shows mineralization decreasing with depth, indicating that the possibility of recent water penetration far below the surface is limited. Shallow groundwater has an elevated level of nitrate, which is attributed to anthropogenic sources due to intensive agricultural activity. The limit of high nitrate water may mark the maximum penetration of groundwater from the surface, which is found in depths 100 m. The northeastern and southwestern industrial areas are highly contaminated by some heavy metals, which may originate from some local industrial effluents. The sewage oxidation ponds seem to show no effect on groundwater; hence, these ponds are not a point source for these heavy metals. Dissolved ions depict five different hydrochemical facies, and stable isotopes define the recharge mechanisms, the origin of groundwater and the hydraulic confinement of deep groundwater. The deep groundwater is untritiated and has long residence times (in the order of thousands of years). Three different hydrochemical groups have been recognized and mapped in El-Sadat City, based on the chemical and isotopic information of the groundwater. These groups have different levels of contamination. The deep groundwater samples are significantly less impacted by surface activities and it appears that these important water resources have very low recharge rates and would, therefore, be severely impacted by overabstraction. The extensive exploitation of groundwater for drinking water supply would shortly be reflected by a gradual decline of the groundwater table in El-Sadat City. Amelioration of groundwater quality requires further management strategies and efforts in the forthcoming years.
机译:在萨达特市地下水系统中进行了水化学和同位素研究,以确定地下水的变化,补给,停留时间和污染程度。随着地下水从城市的东北向西南移动,地下水的盐度逐渐增加。地下水通常显示出矿化程度随深度降低,这表明近期水渗透到地表以下的可能性是有限的。浅层地下水的硝酸盐含量较高,这归因于农业活动的密集化而导致的人为来源。高硝酸盐水的极限可能标志着地下水从地表的最大渗透,深度<100 m。东北和西南工业区受到一些重金属的高度污染,这些重金属可能来自当地的一些工业废水。污水氧化池似乎对地下水没有影响。因此,这些池塘不是这些重金属的主要来源。溶解的离子描绘了五个不同的水化学相,稳定的同位素定义了补给机制,地下水的来源以及深层地下水的水力约束。深层地下水未经处理,停留时间长(约数千年)。根据地下水的化学和同位素信息,萨尔瓦特市已识别并绘制了三个不同的水化学类别。这些群体的污染程度不同。深层地下水样品受地表活动的影响要小得多,这些重要水资源的补给率很低,因此,过度开采会严重影响它们。萨达特市地下水位的逐渐下降将很快反映出为饮用水供应而广泛开采地下水的情况。改善地下水质量需要在未来几年采取进一步的管理策略和努力。

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