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Geochemical evaluation of carbonate aquifers in Ngbo and environs,Ebonyi State, southeastern, Nigeria

机译:Ngbo和环境中碳酸盐含水层的地球化学评价,乌尼州,东南,尼日利亚

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The geochemical evaluation of carbonate aquifers in Ngbo and environs has been executed to ascertain the major ion chemistry and quality of waters for domestic and drinking uses. Ten water samples were gathered from pit lakes, hand dug wells, boreholes and rivers. The collected samples were analysed for pH, EC, TDS, Ca~(2+), Mg~(2+), Na+, K+, HCO_3-, Cl-, SO_42-, NO_3- and PO_42- in the laboratory using the standard methods. The results were compared with NDWQS and WHO standards. The physical parameters varied from pH (6.2-8.4), temp. (25.0-26.0 °C), electrical conductivity (4.9-102 |iS/cm) and total dissolved solids (25.5-214.2 mg/l). The analysed results revealed the mean concentration of cations and anions in the following order: Ca~(2+) > Mg~(2+) > Na+ > K+ > Fe~2+ and HCO_3- > CO_32- > SO_42- > Cl-, respectively. Based on the standard limits, about 90% of the waters in the study area is suitable for domestic and drinking purposes. The Piper trilinear, Stiff and Durov diagrams showed that water samples from various locations fall into mixed CaCO32-+HCO3 type. Various ionic ratio plots show that water sources are from dissolution of minerals in the aquifer media. Geochemical parameters such as Cl-, Na+ and K+ show good interrelationship with positive factor loadings among the ions.
机译:碳酸盐含水层的地球化学评价已被执行,以确定国内和饮用用途的主要离子化学和水域质量。从坑湖,手挖井,钻孔和河流收集十个水样。分析收集的样品,用于使用标准在实验室中的pH,EC,TDS,Ca〜(2+),Mg〜(2+),Na +,K +,HCO_3-,CL-,SO_42-,NO_3-和PO_42-方法。结果与NDWQS和谁标准进行了比较。物理参数从pH(6.2-8.4)变化,TEMP变化。 (25.0-26.0°C),电导率(4.9-102)和总溶解固体(25.5-214.2mg / L)。分析的结果表明,下列顺序中的阳离子和阴离子的平均浓度:Ca〜(2+)> mg〜(2+)> Na +> K> Fe〜2 +和HCO_3-> CO_32-> SO_42-> CL- , 分别。根据标准限制,研究区域约有90%的水域适合国内和饮酒。吹笛者三线性,僵硬和Durov图表明,各种位置的水样落入混合的CaCO 32- + HCO3型。各种离子比例表明水源来自含水层介质中的矿物质的溶解。 Cl-,Na +和K +等地球化学参数显示出离子之间的正面系数良好的相互关系。

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