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首页> 外文期刊>Desalination and water treatment >Evaluation of the physico-chemical quality of groundwater in arid areas: case study (watershed of the Oued Bechar) in Bechar- Kenadsa Region
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Evaluation of the physico-chemical quality of groundwater in arid areas: case study (watershed of the Oued Bechar) in Bechar- Kenadsa Region

机译:干旱地区地下水的理化质量评估:以贝查尔-基纳德萨地区为例(Oued Bechar流域)

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This work is based on the characterization of the physico-chemical parameters in the groundwater of the Bechar-Kenadsa region in southwest Algeria. To achieve this goal, we have collected a database of a water sampling survey that has been done by the National Hydric Resources Agency (ANRH) of the different water points located in the study area according to recognized standards for the collection and analysis protocols of water samples. We extracted the pH, EC, TDS, Ca+2, Mg+2, Na+, K+, Cl-, HCO3-, SO4 and NO3- parameters, we used these physical and hydro chemical characteristics to evaluate the parameters of the sodium content (Na %), Kelly's rate and permeability index. The results showed that just small portion of the groundwater was drinkable. We also used diagrams like Piper's to distinguish that the main water quality is of the Mg-Cl-SO4 class. The Durov's diagram helped us to know that most of this water is concentrated in the area, of magnesium-dominance, characterized by two main classes of water (Mg-Cl-SO4 and Mg-Ca-Cl-SO4). The Gibbs diagram was used to assess the mechanisms controlling the chemistry of water. We noticed that the quality of the water was influenced by the precipitation process in the first row. According to the Wilcox diagram, it was noted that most of groundwater in the study area is characterized by high salinity under three main classes (C4-S1, C4-S2 and C4-S3). We can than conclude that the groundwater in the study area is of poor quality for drinking and irrigation and requires serious treatment to be exploited.
机译:这项工作的基础是对阿尔及利亚西南部Bechar-Kenadsa地区地下水中的理化参数进行表征。为了实现这一目标,我们收集了水采样调查数据库,该数据库由国家水利资源管理局(ANRH)根据公认的水收集和分析协议标准对位于研究区域内的不同水位进行样品。我们提取了pH,EC,TDS,Ca + 2,Mg + 2,Na +,K +,Cl-,HCO3-,SO4和NO3-参数,我们使用这些物理和水化学特征来评估钠含量的参数( Na%),凯利速率和渗透率指数。结果表明,只有一小部分地下水是可饮用的。我们还使用了类似Piper的图表来区分主要水质为Mg-Cl-SO4类。杜罗夫图帮助我们了解到,这些水大部分集中在以镁为主的区域,其特征是两大类水(Mg-Cl-SO4和Mg-Ca-Cl-SO4)。吉布斯图用于评估控制水化学反应的机理。我们注意到水的质量受第一行降水过程的影响。根据Wilcox图,应注意的是,研究区域的大多数地下水在三个主要类别(C4-S1,C4-S2和C4-S3)下具有高盐度的特征。我们可以得出结论,研究区域的地下水饮用水和灌溉质量较差,需要进行认真的处理。

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