In Search of Portable Water Supplies within a Brine and Mine Water-Invaded Region for Serving Some Communities around Ishiagu, Afikpo and Environs in Abakaliki Basin, Southeast Nigeria
- 1 Department of Geology, University of Nigeria, Nsukka, Nigeria
Abstract
The study investigates the hydrogeochemical characteristics of some towns in the Abakaliki Basin, comprising, Ishiagu, Aka Eze, Amaseri, Afikpo and Ok posi communities, with the aim of sourcing for portable water in the area. The basin is underlain by Albian sediments, essentially shales, in the low lands, which were affected by low - grade metamorphism that had produced slates. The highlands comprise basic intrusives from episodes of magmatism and metallic ore mineralisation. Injection of brines into the aquifer system and low, seasonal aquifer recharge from rainfall result s in poor water quality in the area. The study analyz es t he geochemical distribution in water sources in the area and identif ies sources of pollutants to guide the better choice of portable water. Results of hydrogeochemical analysis of both surface and groundwater from the communities were compared with World Health Organization to identify portable water locations in the area. While the salt lake at Okposi is the main source of brine intrusion in the study area, the Pb/Zn mine at Ishiagu is the main source of mine-water pollution in the study area. Most chemical parameters, (especially Cl - , Na + , Ca 2+ , Mg 2+ , SO 4 2- , HCO 3 - ) maintain high concentrations within the salt lake area, with the values de clin ing away from the salt lake. The main anthropogenic source of pollution in the area, especially at Ishiagu, is the indiscriminate surface mining of lead-zinc without proposer waste management practices. Possible sourcing for porta ble water in the study area include s a deep borehole at Ishiagu, away from l ead-zinc intrusives. At the Okposi axis, searching for portable water in bore holes should target shallower aquifers that do not communicate with the deeper-seated brine zones, likewise targeting zones fa r ther away from these brine - invaded areas. A controlled pumping rate could potentially ensure that the cone of depression was not low enough to reach the brine zone at depth. In addition, desalination could also potentially render the salt water drinkable if properly handled to eliminate the high concentration of salts in the water to the level of acceptable limit by the WHO. Based on the study, the best area to target for portable water in the study area is Afikpo, with most geochemical elements naturally occurring within WHO’s standard concentration while portable water could be harnessed in areas further away from mining sites, especially at deep groundwater.
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