尼日尔西南部奥肖博地下复合区部分地区地下水水质评价

Olukayode Adeyinka Falana, Olanrewaju Akinfenwa Akanbi
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摘要

随着奥肖博大都市人口的不断增加,人类产生的废物和环境污染也随之增加,人们开始对可用地下水的质量进行评估。因此,饮用水必须符合理想的质量和标准,并有必要对可供饮用的水质进行彻底监测。从钻入基底复杂岩体的钻孔中随机抽取了20个水样。水样温度范围为26 ~ 29℃,平均27.9℃。pH值为6.7 ~ 7.8,平均值为7.2,为中性水。TDS较低,在21.3 ~ 50.5 mg/l之间,平均值为35.8 mg/l。钙的浓度在1.3 - 7.2mg/l之间。镁的浓度在1.5mg/l到18mg/l之间,钠的浓度在1.2mg/l到8.9mg/l之间,钾的浓度在1.2mg/l到4.3mg/l之间。氯化物浓度范围为2.1mg/l至8.2mg/l,硫酸盐浓度范围为0.4mg/l至12.0mg/l,碳酸氢盐浓度范围为3.7mg/l至14.3mg/l。正离子和阴离子地球化学数据均显示:Mg>Na>Ca>K, HCO3>SO4>Cl。Mg-HCO3占分析水类型的30%,Mg-Cl占15%,Ca-HCO3占25%,Mg-SO4占30%。水相的主要阳离子表明,钙和镁是地成因的,是水与下伏岩石相互作用的结果,反映了基岩溶蚀作用。Cl-、HCO3-和so42的浓度可归因于大都市内不断增长的人口和工业增长,尽管与世卫组织标准和尼日利亚标准相比,浓度不是理想的和允许的限值。
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Groundwater quality assessment from parts of the basement complex area of oshogbo, southwestern nigeri
The increasing population in Oshogbo metropolis with the attending rise in human generated waste and environmental pollution has created a quest in assessing the quality of the available groundwater. Therefore, drinking water must meet the desirable quality and standards, and there is need for thorough monitoring of the quality available for drinking purposes. A total of twenty (20) samples of water were randomly collected from borehole drilled into the basement complex rocks. The temperature of water samples ranges between 26°C and 29°C and an average of 27.9°C. The range of pH is from 6.7 to 7.8 with mean value of 7.2 which indicated that the water is neutral. The TDS was low and ranges between 21.3 to 50.5 mg/l with a mean value of 35.8 mg/l. Calcium has concentration ranging between 1.3mg/l and 7.2mg/l. Concentration of Magnesium  ranges between 1.5mg/l and 18mg/l while concentration of sodium ranges from 1.2mg/l to 8.9mg/l and Potassium ranges from 1.2mg/l to 4.3mg/l. Chloride concentration ranges from 2.1mg/l to 8.2mg/l and Sulfate concentration ranges between 0.4mg/l and 12.0mg/l while Bicarbonate ranges from 3.7mg/l to 14.3mg/l. The geochemical data for both cation and anion shows that: Mg>Na>Ca>K and HCO3>SO4>Cl. Mg-HCO3 occupied 30% of the water type analyzed, Mg-Cl took 15%, Ca-HCO3 took 25%, while Mg-SO4 took 30%.  The major cations from the water facies indicate that Calcium and Magnesium are geogenic in origin and are as a result of interaction of water and the underlying rocks are reflective of bedrock dissolution. . Concentration of Cl-, HCO3- and SO42-can be attributed to increasing population and industrial growth within the metropolis, although the concentration is not when compared with WHO standard and Nigeria Standard standard desirable and permissible limits.
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