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Hydrochemistry of shallow groundwater and surface water in the Ndop plain, North West Cameroon

机译:喀麦隆西北恩多普平原浅层地下水和地表水的水化学

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This study was conducted on the hydrochemistry of shallow groundwater and surface water in the Ndop plain, North West Cameroon. The objectives were to determine the physico-chemical characteristics of water, controls on water chemistry and suitability for drinking and irrigation. Forty-six shallow groundwater and 26 surface water samples were investigated. Field measurements of physical parameters were preceded by chemical analyses of the samples for major ions and F-.About 69% of the water sources had pH values below 6.5, classifying the water as barely acidic. Electrical conductivity (282 µS/cm) and total dissolved solids (183 mg/l) were low suggesting low-mineralised and freshwater. The relative abundance of major ions (meq/l) was Na2+Ca2+Mg2+K+for cations and HCO3-NO3-≥Cl-SO42-for anions. Major ion concentrations were low, and within the WHO guidelines for drinking water, but F-concentrations were much lower (0.39 mg/l) and below guideline value. Main water types and proportions were Na-HCO3(53 %), Ca-HCO3(35 %) and a mixed Na-Ca-HCO3(11%). Predominant processes influencing water chemistry were incongruent dissolution of silicate minerals and cation-exchange of Na+in rocks for Ca2+in water. The low major ion concentrations indicated low water-rock interactions and short residence time. The analysed water was suitable for irrigation.
机译:这项研究是对喀麦隆西北部恩多普平原浅层地下水和地表水的水化学性质进行的。目的是确定水的理化特性,水化学控制以及饮用水和灌溉的适用性。调查了46个浅层地下水和26个地表水样品。在对物理参数进行现场测量之前,先对样品中的主要离子和F-进行化学分析。大约69%的水源的pH值低于6.5,将水分类为弱酸性。电导率(<282 µS / cm)和总溶解固体(<183 mg / l)低,表明矿化度低和淡水低。主要阳离子的相对丰度(meq / l)为Na2 +> Ca2 +> Mg2 +> K +,阴离子为HCO3-NO3-≥Cl-> SO42-。主要离子浓度很低,并且符合WHO的饮用水准则,但F浓度要低得多(<0.39 mg / l),并且低于准则值。主要水类型和比例为Na-HCO3(53%),Ca-HCO3(35%)和混合的Na-Ca-HCO3(11%)。影响水化学的主要过程是硅酸盐矿物的不溶性溶解以及岩石中Na +在水中对Ca2 +的阳离子交换。低的主要离子浓度表明低的水-岩相互作用和短的停留时间。分析的水适合灌溉。

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