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Hydrochemical characteristics and quality assessment of regolith aquifers in Enugu metropolis, southeastern Nigeria

机译:尼日利亚东南部Enugu都会区重生石含水层的水化学特征和质量评估

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Twenty groundwater samples were collected from Enugu metropolis over two seasonal periods in order to characterize the groundwater and to determine its quality for domestic and irrigation purposes. The results show that groundwater of the area is strongly acidic to slightly alkaline in nature and varied from "soft water" to "moderately hard" water type. The major ionic trend is in the order Cl~- > Na~+ > HCO_3~- > K~+ > Mg~(2+) > Ca~(2+) > SO_4~(2-)and Mg~(2+) > Cl~- > Na~+ > K~+ > Ca~(2+) > HCO_3~- > SO_4~(2-) in abundance for dry and rainy seasons, respectively. The results also reveal that there is an increase in trend of the ionic concentrations during the dry season, which arises from weathering of the host rocks and anthropogenic activities. Two hydrochemical facies were identified, namely, Na~+ _-K~+ _-Cl~- _-SO_4~(2-)and Ca~(2+) _-Mg~(2+) _-Cl~-_-SO_4~(2-). with Na~+ _-K~+ _-Cl~- _-SO_4~(2-) as the dominant facies for the two seasons. Groundwater quality ranges from "very poor water" to "good water" and "water unsuitable for drinking purposes" to "good water" for the dry season and rainy season investigations, respectively. The groundwater is suitable for irrigation purposes for the two seasons.
机译:在两个季节从恩努格大都会收集了20个地下水样本,以表征地下水特征并确定其质量,以用于家庭和灌溉目的。结果表明,该地区的地下水本质上是强酸性至​​弱碱性,并且从“软水”到“中等硬”水类型不等。主要离子趋势为Cl〜-> Na〜+> HCO_3〜-> K〜+> Mg〜(2+)> Ca〜(2+)> SO_4〜(2-)和Mg〜(2+ )> Cl〜-> Na〜+> K〜+> Ca〜(2+)> HCO_3〜-> SO_4〜(2-)分别在雨季和雨季丰富。结果还表明,干旱季节离子浓度的趋势有所增加,这是由于宿主岩石的风化和人为活动引起的。确定了两个水化学相,即Na〜+ _-K〜+ _-Cl〜-_-SO_4〜(2-)和Ca〜(2+)_-Mg〜(2+)_-Cl〜-_ -SO_4〜(2-)。 Na〜+ _-K〜+ _-Cl〜-_-SO_4〜(2-)为两个季节的主要相。分别在旱季和雨季调查中,地下水水质从“极差水”到“优质水”,从“不适合饮用的水”到“优质水”。这两个季节的地下水适合灌溉。

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