Thermodynamic and Microbial Constraints on Redox-Induced Mobilization of Redox-Sensitive Metal(loid)s in Shallow Aquifers of Enugu

Authors

  • Ezeugwu Innocent Onyebuchi Department of Geology and Mining, Faculty of Physical Sciences, Enugu State University of Science and Technology, Agbani, Enugu, Nigeria
  • Ifunanya C. Ikegbunam Department of civil engineering, Akanu – Ibiam Federal Polythechnic Unwana, Afikpo, Ebonyi State
  • Ezenwali Moses Obinna Department of Biochemistry, Faculty of Biological Sciences, Enugu State University of Science and Technology, Agbani, Enugu, Nigeria

DOI:

https://doi.org/10.58885/ijees.v2i1.17.eo

Keywords:

Redox-sensitive metals, Groundwater contamination, Microbial metal reduction, Enugu aquifers, Arsenic mobilization, Thermodynamic modeling, Iron and manganese oxides, Environmental geochemistry.

Abstract

This study investigates the thermodynamic and microbial factors controlling the redox-induced mobilization of redox-sensitive metal(loid)s—iron (Fe³⁺), manganese (Mn), and arsenic (As)—in shallow aquifers across Enugu metropolis, Nigeria. A total of 25 water and sediment samples were collected from hand-dug wells and streams across five geographical areas: Ologo, Trans-Ekulu, Amechi, Ajali River/9th Mile and Centenary geographical areas. Samples were collected using sterile bottles, stored under cool conditions, and analyzed in the laboratory using Atomic Absorption Spectrophotometry (AAS) and Inductively Coupled Plasma Mass Spectrometry (ICP-MS), following standard EPA analytical methods. All analyses were performed in triplicate, and results were reported as mean concentrations in milligrams per liter (mg/L). Results reveal spatial variability in metal concentrations influenced by local hydrogeochemical conditions. In the Ologo area, iron ranged from 0.300 to 0.390 mg/L, manganese from 0.154 to 0.300 mg/L, and arsenic from 0.029 to 0.068 mg/L. Amechi samples showed iron levels between 0.250 and 0.355 mg/L, manganese concentrations remained stable (0.150–0.165 mg/L), and arsenic ranged narrowly from 0.043 to 0.049 mg/L. In the Ajali River/9th Mile region, iron and manganese were elevated (0.301–0.420 mg/L and 0.220–0.260 mg/L, respectively), with arsenic ranging from 0.028 to 0.035 mg/L. Centenary Water sites recorded lower iron concentrations (0.180–0.290 mg/L), moderate manganese (0.150–0.190 mg/L), and low arsenic (0.020–0.027 mg/L). Trans-Ekulu exhibited the highest iron variability (0.220–0.718 mg/L), consistent manganese (0.225–0.229 mg/L), and low arsenic levels (0.013–0.016 mg/L). These findings indicate heterogeneous redox conditions influencing metal mobilization, with certain areas exceeding recommended iron limits for drinking water. The data contribute to understanding metal distribution patterns in Enugu’s aquifers and underscore the need for continuous monitoring to safeguard public health.

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Published

2017-05-15

How to Cite

Ezeugwu Innocent Onyebuchi, Ifunanya C. Ikegbunam, & Ezenwali Moses Obinna. (2017). Thermodynamic and Microbial Constraints on Redox-Induced Mobilization of Redox-Sensitive Metal(loid)s in Shallow Aquifers of Enugu. International Journal of Earth & Environmental Sciences (IJEES), 2(1), 17–31. https://doi.org/10.58885/ijees.v2i1.17.eo

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