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首页> 外文期刊>Universal Journal of Environmental Research and Technology >Hydrogeochemical Assessment of Groundwater Quality in Parts of Ohaji Egbema Eastern Niger Delta, Nigeria
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Hydrogeochemical Assessment of Groundwater Quality in Parts of Ohaji Egbema Eastern Niger Delta, Nigeria

机译:尼日利亚尼日尔东部Ohaji Egbema部分地区的地下水水文地球化学评估

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摘要

Groundwater resource in Ohaji Egbema, was investigated for its quality from which inferences are drawn on its usability, prevalent hydrochemical processes in the water system and probable quality degradation. Results of the field and laboratory analysis indicate a chemical attribute of low pH, total dissolved solids (TDS) and electrical conductivity (EC). Cationic concentrations including Na2+, K+, Ca2+, Mg2+ have values ranging from 5.2 - 20.3, 2 - 8, 0.96 - 9.28, and 0 - 2.3mg/l respectively whilst Anions involve NO3-, Cl-, SO42-, HCO3-, with their respective values as 8.5-20.1, 8.5-24.14, 1.48-45.07 and 8.6-16.5mg/l. Selected heavy metals tested follow the order of Mn2+ > Fe > Zn2+ > Cu2+. The water quality plots reveal a hydrogeochemical process operative within the groundwater system as relating to water-soil interaction and incorporation of leached formation water along the groundwater flow path. Illatively, other parameters suggests a low mineralized soft freshwater having a limited residence time, with an onset of degradation from biochemical related substances resulting from human activities in the area. An interplay of these processes produced a chloride water type (Na(k)Cl and Cl- + SO4-). A comparison of these results with various quality guidelines, suggests that the groundwater maybe usable in its untreated state for crop irrigation but will require pH remediation to upgrade its quality for portability and use in some industries.
机译:对奥哈吉·埃格贝马(Ohaji Egbema)的地下水质量进行了调查,从中得出了其可用性,水系统中普遍的水化学过程以及质量可能下降的推断。现场和实验室分析的结果表明,低pH,总溶解固体(TDS)和电导率(EC)的化学属性。包括Na2 +,K +,Ca2 +,Mg2 +在内的阳离子浓度值分别在5.2-20.3、2-8、0.96-9.28和0-2.3mg / l的范围内,而阴离子则包括NO3-,Cl-,SO42-,HCO3-。它们各自的值为8.5-20.1、8.5-24.14、1.48-45.07和8.6-16.5mg / l。所选的重金属测试顺序为Mn2 +> Fe> Zn2 +> Cu2 +。水质图揭示了在地下水系统中有效的水文地球化学过程,与水-土壤相互作用以及沿地下水流路的浸出地层水的掺入有关。荒谬的是,其他参数表明低矿化的软淡水具有有限的停留时间,并且由于该地区的人类活动而导致生化相关物质开始降解。这些过程的相互作用产生了氯化物水类型(Na(k)Cl和Cl- + SO4-)。将这些结果与各种质量准则进行比较,表明地下水可能在未经处理的状态下可用于作物灌溉,但需要进行pH修复以提高其质量,以便在某些行业中使用和使用。

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