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Hydrogeochemical Investigation of Groundwater Resources in Umunya and Environs of the Anambra Basin, Nigeria

机译:尼日利亚安马布拉盆地乌南和周围地下水资源的水文地球化学调查

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The study area falls within the Anambra Basin in southeastern Nigeria. The lithostratigraphic units within the study area are the Imo Shale (Paleocene) and the Ameki Formation (Eocene). This paper takes a closer look at the physico-chemical analyses of the groundwater discharge from the prolific Nanka Sands reservoir.A total of twenty-one (21) water samples were obtained from the groundwater sources and were analyzed for their physico-chemical characteristics with the aim of assessing their quality and usability. Result of some physical and hydrochemical parameters show mean values of 5.75 pH, 46.98 mg/l TDS; 10.86 mg/l Ca~(2+) , 7.50 mg/l Na~+ ; 3.29 mg/l K~+ , 1.46 mg/l Mg~(2+), 25.74 mg/l HCO_3; 16.70 mg/l Cl~- , 0.09 mg/l Fe~(2+), 4.65 mg/l NO~(3-) and 72.36 μs/cm conductivity. The water hardness and Sodium Absorption Ratio (SAR) are respectively, 34.74 mg/l and 0.73. Statistical analyses, using the product moment coefficient of correlation, indicate very strong correlation between the following pairs of parameters: Total Hardness and TDS (r = 0.94); TDS and EC (r = 0.99); Ca~(2+) and HCO_3~- (r = 0.83); Ca~(2+) and Mg~(2+) (r = 0.70) ; Na~+ and K~+ (r = 0.57); pH and TH (r = 0.52) while negative correlation was observed between pH and Cl~- (r = - 0.77).Five water groups were identified based on characterization in the piper trilinear diagram. These include Ca-Na+K-HCO_3, Na+K-HCO_3, Na+K-HCO_3-Cl, Ca-Cl-HCO_3, and Ca-Na+K-SO_4. They reflect diverse effects of bedrock lithologies, base exchange processes, precipitation and weathering. The groundwater source is strongly to weakly acidic fresh water with the exception of water sample (WS2) showing slightly alkaline fresh water. The water samples are generally soft with low sodium content. The groundwater quality is good and satisfies the World Health Organization (WHO) guidelines and the Nigeria Standards for Drinking Water Quality (NSDWQ) for domestic, agricultural and other industrial uses requiring minor treatment.
机译:该研究区落在尼日利亚东南部的Anambra盆地内。研究区内的岩石岩石术单位是IMO页岩(古)和Ameki形成(eocene)。本文仔细研究了从多产南卡砂储层的地下水排放的物理化学分析。从地下水来源获得二十一(21)个水样的总共,并分析了它们的物理化学特性目的是评估他们的质量和可用性。一些物理和水化学参数的结果显示5.75 pH,46.98mg / L TDS的平均值; 10.86 mg / l Ca〜(2+),7.50 mg / L na〜+; 3.29 mg / l k〜+,1.46 mg / l mg〜(2+),25.74 mg / l HCO_3; 16.70mg / L Cl〜 - ,0.09 mg / L Fe〜(2+),4.65mg / L no〜(3-)和72.36μs/ cm电导率。水硬度和钠吸收比(SAR)分别为34.74mg / L和0.73。统计分析,使用产物矩系数的相关系数表示以下参数对之间的非常强的相关性:总硬度和TDS(r = 0.94); TDS和EC(r = 0.99); CA〜(2+)和HCO_3〜 - (r = 0.83); Ca〜(2+)和mg〜(2+)(r = 0.70); na〜+和k〜+(r = 0.57); pH和Th(r = 0.52),同时在pH和Cl〜 - (r = - 0.77)之间观察到负相关性。基于吹笛者三线性图中的表征鉴定了水基。这些包括Ca-Na + K-HCO_3,Na + K-HCO_3,Na + K-HCO_3-C1,Ca-Cl-HCO_3和Ca-Na + K-So_4。它们反映了基岩岩性,基础交换过程,降水和风化的多样化效果。除水样(WS2)外,地下水源强烈地呈弱酸淡水,呈浅碱性淡水。水样通常柔软,含量低。地下水质量是良好的,满足世界卫生组织(世卫组织)指导方针和尼日利亚饮用水质量标准(NSDWQ),用于国内,农业和其他工业用途需要轻微治疗。

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