Microbial Influence on Redox Geochemistry in Enugu Shale Aquifer: Implications for Iron, Manganese, and Arsenic Dynamics

Authors

  • Ezeugwu Innocent Onyebuchi Department of Geology and Mining, Faculty of Physical Sciences, Enugu State University of Science and Technology, Agbani, Enugu, Nigeria
  • Omezi Ifeanyi Department of Petroleum engineering, Nnamdi Azikiwe University, Awka
  • Ifunanya C. Ikegbunam Department of civil engineering, Akanu – Ibiam Federal Polythechnic Unwana, Afikpo, Ebonyi State

DOI:

https://doi.org/10.58885/ijees.v4i1.20.lo

Keywords:

Groundwater quality, Iron, Manganese, Arsenic, Redox processes, Microbial activity, ASS, ICP-MS, WHO guidelines.

Abstract

This study investigates the concentrations of redox-sensitive metals—iron (Fe³⁺), manganese (Mn²⁺), and arsenic (As)—in groundwater from selected locations within Enugu, Southeastern Nigeria. A total of 25 water and sediment samples were collected from hand-dug wells and streams across five geographical areas: Emene, Ugwuaji, New Artisan, Gariki, and Agbani Road. 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). The results revealed widespread exceedance of World Health Organization (WHO) permissible limits for drinking water. In the Emene area, Fe³⁺ ranged from 0.280 to 0.350 mg/L, Mn²⁺ from 0.170 to 0.260 mg/L, and As from 0.018 to 0.035 mg/L. At Ugwuaji, Fe³⁺ levels varied between 0.100 and 0.300 mg/L, Mn²⁺ between 0.120 and 0.210 mg/L, and arsenic peaked at 0.050 mg/L, five times above the WHO limit of 0.01 mg/L. New Artisan samples recorded Fe³⁺ between 0.210 and 0.300 mg/L, Mn²⁺ between 0.180 and 0.270 mg/L, and As from 0.011 to 0.022 mg/L. In Gariki, iron concentrations were especially high, ranging from 0.360 to 0.553 mg/L, with manganese between 0.130 and 0.210 mg/L and arsenic reaching up to 0.074 mg/L. The Agbani Road area showed the highest contamination levels, with Fe³⁺ from 0.520 to 0.740 mg/L, Mn²⁺ from 0.600 to 0.780 mg/L, and arsenic values as high as 0.060 mg/L. The consistently elevated levels of these metals particularly arsenic and manganese, indicate the presence of reducing geochemical conditions in the subsurface, likely influenced by microbial activity and the reductive dissolution of metal-bearing minerals. These findings raise significant concerns regarding the safety of groundwater for domestic use in these areas and highlight the need for regular monitoring and remediation strategies to protect public health.

References

Appelo, C.A.J., and Postma, D. (2005). Geochemistry, Groundwater and Pollution (2nd ed.). A.A. Balkema Publishers.

Chapelle, F. H. (2001). Ground-Water Microbiology and Geochemistry. John Wiley and Sons.

Lovley, D. R., Holmes, D. E., and Nevin, K. P. (2004). Dissimilatory Fe(III) and Mn(IV) reduction. Advances in Microbial Physiology, 49, 219–286.

Edet, A., and Okereke, C. (2001). Hydrogeological and geotechnical characteristics of the Enugu Shale in southeastern Nigeria. Hydrogeology Journal, 9(3), 365–374.

Eze, C.L., and Maduka, C.N. (2021). Hydrogeochemical evaluation and health risk assessment of groundwater quality in parts of Enugu State, Nigeria. Environmental Earth Sciences, 80(19), 1–18. https://doi.org/10.1007/s12665-021-09920-z

Ezeh, H. N. (2012). Hydrogeophysical assessment of groundwater potential in Enugu Metropolis, southeastern Nigeria. International Journal of Physical Sciences, 7(48), 6264–6274.

Ezeh, H. N., and Ugwu, G. Z. (2010). Geochemical and microbial assessment of groundwater quality in Enugu Urban. Environmental Research Journal, 4(3), 276–284.

Islam, F. S., Gault, A. G., Boothman, C., Polya, D. A., Charnock, J. M., Chatterjee, D., and Lloyd, J. R. (2004). Role of metal-reducing bacteria in arsenic release from Bengal delta sediments. Nature, 430(6995), 68–71. https://doi.org/10.1038/nature02638

Lovley, D. R., Holmes, D. E., and Nevin, K. P. (2004). Dissimilatory Fe(III) and Mn(IV) reduction. Advances in Microbial Physiology, 49, 219–286.

Nwajide, C.S. (2013). Geology of Nigeria’s Sedimentary Basins. CSS Press.

Okechukwu, C. and Ikenna, O. (2024). Groundwater quality assessment in Enugu Metropolis: Health implications and sustainable management. Nigerian Journal of Hydrogeology, 15(2), 83–92.

Nwankwoala, H. O., Udom, G. J., and Amadi, A. N. (2016). Geochemical characteristics and health risk implications of trace elements in groundwater of parts of southeastern Nigeria. International Journal of Environmental Science and Technology, 13(3), 905–914. https://doi.org/10.1007/s13762-015-0908-4

Okechukwu, C., and Ikenna, O. (2024). Groundwater quality assessment in Enugu Metropolis: Health implications and sustainable management. Nigerian Journal of Hydrogeology, 15(2), 83–92.

Oremland, R.S., and Stolz, J.F. (2003). The ecology of arsenic. Science, 300(5621), 939–944. https://doi.org/10.1126/science.1081903

Ozoko, D. C., and Ezeugwu, I. O. (2025). Geomicrobiology of Aquifers in Enugu. European Journal of Applied Sciences, 13(2), 184–207.

https://doi.org/10.14738/aivp.132.18517

Ravenscroft, P., Brammer, H., and Richards, K. (2009). Arsenic Pollution: A Global Synthesis. Wiley-Blackwell.

Smedley, P. L., and Kinniburgh, D. G. (2002). A review of the source, behaviour and distribution of arsenic in natural waters. Applied Geochemistry, 17(5), 517–568.

Smedley, P. L., and Kinniburgh, D. G. (2002). A review of the source, behaviour and distribution of arsenic in natural waters. Applied Geochemistry, 17(5), 517–568.

Tebo, B.M., et al. (2004). Biogenic manganese oxides: Properties and mechanisms of formation. Annual Review of Earth and Planetary Sciences, 32, 287–328.

USEPA (1994). Method 200.8: Determination of Trace Elements in Waters and Wastes by ICP-MS. Revision 5.4. United States Environmental Protection Agency, Office of Research and Development, Cincinnati, OH.

USEPA (2014). Test Methods for Evaluating Solid Waste, Physical/Chemical Methods (SW-846), Method 7000B: Flame Atomic Absorption Spectrophotometry. United States Environmental Protection Agency.

Weber, K.A., Achenbach, L.A., and Coates, J.D. (2006). Microorganisms pumping iron: anaerobic microbial iron oxidation and reduction. Nature Reviews Microbiology, 4(10), 752–764. https://doi.org/10.1038/nrmicro1490

WHO (2017). Guidelines for Drinking-water Quality, 4th Edition incorporating the 1st Addendum. World Health Organization, Geneva.

World Health Organization (WHO). (2017). Guidelines for Drinking-water Quality (4th ed.). Geneva: WHO Press.

Zhu, C., and Anderson, G. (2002). Environmental Applications of Geochemical Modeling. Cambridge University Press.

Downloads

Published

2019-04-30

How to Cite

Ezeugwu Innocent Onyebuchi, Omezi Ifeanyi, & Ifunanya C. Ikegbunam. (2019). Microbial Influence on Redox Geochemistry in Enugu Shale Aquifer: Implications for Iron, Manganese, and Arsenic Dynamics. International Journal of Earth & Environmental Sciences (IJEES), 4(1), 20–34. https://doi.org/10.58885/ijees.v4i1.20.lo

Metrics

Most read articles by the same author(s)