Journal of Geography, Environment and Earth Science International

A total of five borehole samples were collected from five towns in Owerri metropolis, South-eastern Nigeria and subjected to physio-chemical analysis using atomic absorption spectrophotometer (AAS) and other standard equipment with the aim of characterizing and analysing the groundwater quality indicators. These quality indicators are namely: pH, temperature, total hardness, turbidity, electrical conductivity, total dissolved solids, total suspended solids, dissolved oxygen, Ca²⁺, Mg²⁺, Na⁺, K⁺, HCO₃^-, SO₄^2-, Cl^-, NO₃^-, Fe²⁺, Zn²⁺, Pb²⁺, Cu²⁺, Mn²⁺, and Cr²⁺. With the aid of geochemical diagrams acquired using Aquachem 2014.2, we classified the groundwater samples into their respective hydrogeochemical facies, identified their relative similarity and demonstrated the irrigability of the groundwater. The results showed that the groundwater quality indicators occur in the groundwater in amounts that fall within their respective permissible limits as set by World Health Organization (WHO) Drinking Water Standard, and therefore ascertained the groundwater portable and suitable for drinking. The pH of the groundwater has a mean value of 6.7 with a standard deviation of 0.26. The relative abundance of the majority of cations follows this sequence - Na⁺ > Ca²⁺ > K⁺ > Mg²⁺, while that of the anions follow this sequence - HCO₃^- > Cl^- > SO₄^2- > NO₃^-. Heavy metals constituents of the groundwater follow this order of relative abundance - Zn²⁺ > Fe²⁺ > Mn²⁺ > Cu²⁺ > Cr²⁺ > Pb²⁺. Three hydrogeochemical facies were identified in the area and they are: the Na⁺—Cl^- water type, the Mixed Ca²⁺-Na⁺-HCO₃^- water type and the Ca²⁺-Mg²⁺-HCO₃^- water type. Great similarities were identified between the geochemical composition of the samples and they are all evidently suitable for irrigation purposes. The TDS level and concentration of Ca²⁺, Mg²⁺ and Cl^- demonstrated the freshness and softness of the groundwater, with no laxative effects. From series of computations and plots, silicate weathering and seawater intrusion were deduced to be the dominant factors controlling the groundwater chemistry, though there is evidence of poor rock dissolution – immature water-rock equilibrium.