Delineation of Lithology-based Radiogenic Heat Production from the Analysis of Airborne Radiometric Data of Azara and Environs, North-Central Nigeria

Sunday Ogayi  Egede; Oke Israel  Okwokwo; John Mathew  Sawuta; Fidelis Iorzua Kwaghhua; Adegoke Blessing  Adekemi; Taiwo  Adewumi

doi:10.62050/ljsir2026.v4n1.755

Auteur/ices

Sunday Ogayi Egede
Department of Physics, Federal University of Lafia, Nigeria
Oke Israel Okwokwo
Department of Physics, University of Abuja, FCT, Nigeria
https://orcid.org/0000-0003-3451-7545
John Mathew Sawuta
National Space Research and Development Agency, NASRDA, Abuja, Nigeria
Fidelis Iorzua Kwaghhua
fidelisik@gmail.com

Department of Geophysics, Federal University of Technology, Minna, Nigeria
https://orcid.org/0009-0003-5954-9073
Adegoke Blessing Adekemi
Department of Physics, Federal University of Lafia, Nigeria
Taiwo Adewumi
Department of Physics, Federal University of Lafia, Nigeria
https://orcid.org/0000-0002-5936-4285

Mots-clés :

radioelement , radiogenic heat production , radiometric data , lithology , Geothermal energy

Résumé

This study offers new insights into naturally occurring radioactive minerals in the Azara area and its environs, focusing on their impact on radiogenic heat production (RHP) for exploration geothermal energy. The radiometric data were analysed in relation to the lithology of the study area to determine the contribution of each lithologic unit to the estimated RHP. The study assessed radioelement concentrations, spatial distributions, and statistical summaries for each lithologic unit. Using radiometric data, the study mapped and analysed the spatial occurrence of potassium (K), thorium (eTh), and uranium (eU). The results show average concentrations of 1.23 % for K, 12.15 ppm for eTh, and 3.38 ppm for eU. Compared with crustal averages, K levels were lower, while eTh and eU levels were slightly higher. Radioelement abundance varied across rock types, with the highest concentrations in shales, siltstones, and sandstones. Estimated RHP values ranged from 0.90 to 2.70 uWm⁻³, with an average of 1.70 uWm⁻³. The estimated RHP value falls within the typical crustal range but is below the 4.0 uWm⁻³ threshold for a viable geothermal energy source.

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Delineation of Lithology-based Radiogenic Heat Production from the Analysis of Airborne Radiometric Data of Azara and Environs, North-Central Nigeria

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