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首页> 外文期刊>Journal of African Earth Sciences >Evaluation of groundwater chemistry and its impact on drinking and irrigation water quality in the eastern part of the Central Arabian graben and trough system, Saudi Arabia
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Evaluation of groundwater chemistry and its impact on drinking and irrigation water quality in the eastern part of the Central Arabian graben and trough system, Saudi Arabia

机译:沙特阿拉伯中部阿拉伯grab沟系统东部的地下水化学评估及其对饮用水和灌溉水质量的影响

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The present study deals with the assessment of groundwater with respect to the main hydrological processes controlling its chemistry and its subsequent impact on groundwater quality for drinking and irrigation purposes in the eastern part of the Central Arabian graben and trough system. Groundwater samples were collected from 73 bore wells tapping the Cretaceous Biyadh and Wasia sandstone aquifers. The main groundwater facies in the area belong to the mixed Ca-Mg-SO4/Cl type and the SO4-Cl type. Prolonged rock water interaction has resulted in high TDS (average of 2131 mg/l) and high EC (average of 2725 mu S/cm) of the groundwater. The average nitrate (5638 mg/l) value in the area is higher than the WHO prescribed limits of 50 mg/l in drinking water and is attributed to agricultural activities. The Drinking Water Quality Index (DWQI) shows that 33% of the water samples fall within the excellent to good category whereas the remaining samples fall in the poor to unsuitable for drinking category. In terms of Sodium Adsorption Ratio (SAR), Sodium percentage (Na %) and Residual Sodium Carbonate (RSC) the groundwater is suitable for irrigation however the high salinity values can adversely affect the plant physiology. (C) 2016 Elsevier Ltd. All rights reserved.
机译:本研究涉及对地下水的主要水文过程进行评估,这些过程控制着化学过程及其对中部阿拉伯grab沟系统东部饮用水和灌溉目的地下水质量的影响。从白垩纪比亚德和瓦西亚砂岩含水层上攻下的73口井中收集了地下水样品。该地区的主要地下水相属于混合Ca-Mg-SO4 / Cl型和SO4-Cl型。长时间的岩水相互作用导致地下水的TDS高(平均2131 mg / l)和EC高(平均2725μS / cm)。该地区的平均硝酸盐(5638 mg / l)值高于WHO规定的饮用水中50 mg / l的限值,这归因于农业活动。饮用水水质指数(DWQI)显示,有33%的水样本属于“优至良”类别,而其余样本属于“差”至“不适合”类别。就钠吸附率(SAR),钠百分比(Na%)和残留碳酸钠(RSC)而言,地下水适合灌溉,但是高盐度值可能会对植物生理产生不利影响。 (C)2016 Elsevier Ltd.保留所有权利。

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