摩洛哥穆卢亚弗里蒂萨地区地下水灌溉适宜性评估

Moulay Ahmed Ben Driss, Abdelhadi Ifliliss, Said Ettazarini, Yousef Hahou, Larbi Boudad, Mohamed El Amrani, Said Courba
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摘要

在摩洛哥许多地区的干旱和半干旱气候条件下,水的供应和质量是农业区可持续发展的主要关键。在摩洛哥东北部覆盖中穆卢亚和部分下穆卢亚的弗里蒂萨地区,在人口大幅增长和水资源有限的环境下,灌溉是农业活动的必要条件。这项研究的主要目的是评估地下水的质量及其是否适合灌溉,并确定可能影响地下水化学性质的水岩相互作用过程。该方法基于 94 个地下水样本的主要离子含量分析和质量指数计算,即 pH 值、电导率 (EC)、总溶解固体 (TDS)、总硬度 (TH)、钠百分比 (Na%)、残留碳酸钠 (RSC)、钠吸附比 (SAR) 和渗透指数 (PI)。皮珀分类法用于确定水的化学面,而常用的分布图和地球化学图则有助于讨论水与含水层岩石之间可能的相互作用过程。所研究的地下水显示了不同的 pH 值(5.8-8.8)、盐度(367-3301 毫克/升)和总硬度(15-186 毫克/升,以 CaCO3 计)。发现了 Ca-Mg-HCO3、Ca-Mg-SO4-Cl 和混合水层类型,还有一个样本显示了 Na-K-SO4-Cl 层。在吉布斯图中绘制的样品表明,水与岩石之间可能存在相互作用,地球化学分布图证实了这一点。威尔科克斯图显示,大多数水样属于优至良和良至允许类别,而美国盐度危害图显示钠危害较低,盐度水平较低、中等和较高。如果考虑到一些预防措施,按照目前的国际标准,地下水适合用于灌溉。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Assessment of groundwater suitability for irrigation purposes in the Fritissa region, Moulouya, Morocco
Under arid and semi-arid climate conditions, as is the case in many Moroccan regions, the availability and quality of water are the main keys to the sustainable development of agricultural zones. In the Fritissa region covering Middle Moulouya and a part of Lower Moulouya, North-eastern Morocco, irrigation practices are necessary for agricultural activities, in an environment with significant population growth, and limited water resources. The main aim of this study is to assess the quality of groundwater and its suitability for irrigation purposes, and to determine the possible water-rock interaction processes that influence the groundwater chemistry. The approach is based on the analysis of major ions contents and the calculation of quality indices namely pH, Electrical conductivity (EC), Total Dissolved Solids (TDS), Total Hardness (TH), Sodium Percentage (Na%), Residual Sodium Carbonate (RSC), Sodium Adsorption Ratio (SAR) and Permeability Index (PI) for 94 groundwater samples. Piper classification is used to determine the chemical water facies, while commonly used distribution and geochemical diagrams helped to discuss the possible interaction processes between water and aquifer rocks. The studied groundwater showed varying values for pH (5.8–8.8), salinity (367–3301 mg/L) and total hardness (15–186 mg/l as CaCO3). Ca-Mg-HCO3, Ca-Mg-SO4-Cl, and mixed water facies types are found, while one sample showed Na-K-SO4-Cl facies. The plotting of samples in Gibbs diagrams suggests possible water-rock interactions, that are confirmed by geochemical distribution diagrams. The Wilcox diagram showed that most of the water samples are of excellent to good and good to permissible categories, while the US salinity Hazard diagram revealed low sodium hazard and low, medium and high levels of salinity. Groundwater is suitable for irrigation according to current international standards if some precautions are considered.
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