GLOBAL JOURNAL OF EARTH AND ENVIRONMENTAL SCIENCE
Integrity Research Journals

ISSN: 2636-6002
Model: Open Access/Peer Reviewed
DOI: 10.31248/GJEES
Start Year: 2016
Email: gjees@integrityresjournals.org


Review of variability of radiogenic heat properties of some rock types as a basis for geothermal characterization in Nigeria

https://doi.org/10.31248/GJEES2020.073   |   Article Number: 51974B771   |   Vol.5 (4) - October 2020

Received Date: 02 June 2020   |   Accepted Date: 13 July 2020  |   Published Date: 30 October 2020

Authors:  Sedara, S. O.* and Asere, A. M.

Keywords: Heat flow, heat production, geophysical exploration, geothermal resources, thermal structure.

The southwestern part of Nigeria is one of the three known regions in Nigeria with geothermal prospect. It is characterized by distinctly different thermal state and surface thermal manifestations. Although a number of geophysical explorations have been undertaken, but studies on fundamental geothermal theory remain scarce, including a lack of high-quality heat flow determinations and thermal structure studies. Heat production and heat flow properties play a very critical role in the study of thermal structure in a region. In this report, heat production and heat flow data of rock samples from published studies from some localities in Nigeria was compiled. To optimize this data, the rock-type denominations from the original studies was classified. This was used to characterize the thermal structure of the areas for possible geothermal exploration and radiogenic heat production distribution for the different rock types in the region. This gave some useful guidelines to lithospheric thermal modeling. From the heat production data, there is a wide range in values with igneous rocks having a maximum 11.17 µWm-3 and the metamorphic rocks having 131.37 µWm-3 as maximum value. The metamorphic rocks have higher values than the igneous rocks while the heat flow compiled for the country area has a minimum of 29 mWm-2 and a maximum of 130 mWm-2 with a mean value of 80 mWm-2. The high heat flow observed from data of the southwest zones may suggest the existence of anomalous heat source body in crust due to the radiogenic heat of the solid crust. This work is also an appraisal to direct attention to the lack of thermal properties investigations in the southwestern part of Nigeria and the need to improve on the heat flow database of Nigeria. Hence some parts of the study areas could be further explored for geothermal energy using appropriate geophysical techniques.

Abraham, E. M., Lawal, K. M., Ekwe, A. C., Alile, O., Murana, K. A., & Lawal, A. A. (2014). Spectral analysis of aeromagnetic data for geothermal energy investigation of Ikogosi Warm Spring-Ekiti State, southwestern Nigeria. Geothermal Energy, 2, Article Number 6.
Crossref
 
Abraham, E. M., Obande, E. G., Chukwu, M., Chukwu, C. G., & Onwe, M. R. (2015). Estimating depth to the bottom of magnetic sources at Wikki Warm Spring region, northeastern Nigeria, using fractal distribution of sources approach. Turkish Journal of Earth Sciences, 24(5), 494-512.
Crossref
 
Adegbuyi, O, Abimbola, A. F. (1997). Energy resource potential of Ikogosi Warm Spring Area, Ekiti State, Southwestern Nigeria. African Journal of Science, 1(2), 111-117.
 
Adegbuyi, O., Ajayi, O. S., & Odeyemi, I. B. (1996). Prospect of a hot-dry-rock (HDR) geothermal energy resource around the Ikogosi-Ekiti Warm Spring in Ondo State. Nigeria Journal Renewable Energy, 4(1), 58-64.
 
Adetona, A. A., Salako, K. A., & Rafiu, A. A. (2017). Curie depth and geothermal gradient from spectral analysis of aeromagnetic data over Upper Anambra and Lower Benue Basin, Nigeria. Nigerian Journal of Technological Research, 12(2), 20-26.
Crossref
 
Ajayi, O. S., Adegbuyi, O., Farai, P., & Ajayi, I. R. (1996). Determination of natural radionuclides in rocks of the Ikogosi Ekiti warm spring area, Ekiti State, Nigeria. Nigerian Journal of Science, 30(2), 15-21.
 
Alabi, O. O., Akinluyi, F. O., Ojo, M. O., & Adebo, B. A. (2007). Radiogenic heat production of rock from three rivers in Osun state of Nigeria. Journal of Applied Science, 7(12), 1661-1663.
Crossref
 
Ali, S., & Orazulike, D. M. (2010). Well logs-derived radiogenic heat production in the sediments of the Chad Basin, NE Nigeria. Journal of Applied Science, 10(10), 786-800.
Crossref
 
Anakwuba, E. K., Onwuemesi, A. G., Chinwuko, A. I., Onuba, L. N., (2011). The interpretation of aeromagnetic anomalies over Maiduguri-Dikwa depression, Chad Basin Nigeria: A structural view. Archives of Applied Science Research, 3(4), 499-508.
 
Anomohanran, O. (2004). The use of third degree polynomial for accurate conversion of Seismic time to depth and vice versa. Journal of the Nigerian Association of Mathematical Physics, 8, 241-246.
Crossref
 
Avbovbo A. A., (1978). Geothermal gradients in the southern Nigerian basin. Bulletin of Canadian Petroleum Geology, 26(2), 268-274.
 
Ayuba, R. A., & Nur, A. (2018). Determination of curie depth isotherm and geothermal studies over parts of Nasarawa and environs, North Central Nigeria. International Journal of Energy and Environmental Science, 3(4), 69-81.
Crossref
 
Bea, F., Montero, P., & Zinger, T. (2003). The nature, origin, and thermal influence of the granite source layer of Central Iberia. The Journal of Geology, 111(5), 579-595.
Crossref
 
Beardsmore, G. R., & Cull, J. P. (2001). Crustal heat flow: A guide to measurement and modelling. Cambridge University Press, City.
Crossref
 
Bello, O. A., Özgür, N., & Çalışkan, T. A. (2017). Hydrogeological, hydrogeochemical and isotope geochemical features of Geothermal waters in Simav and environs, Western Anatolia, Turkey. Procedia Earth and Planetary Science, 17, 29-32.
Crossref
 
Boboye, O. A., Adeyemi, M. S., & Madukwe, H. Y. (2018). Lithostratigraphy and Inorganic Geochemical Studies of Cretaceous-Tertiary Lithofacies from Nigerian Three Inland Basin. Open Journal of Geology, 8(7), 711-736.
Crossref
 
Brigaud, F., & Lucazeau, F., (1985). Heat flow from the West African shield. Geophysical Research Letters, 12(9), 549-552.
Crossref
 
Brown, G. C., & Mussett, A. E. (1993). The inaccessible earth: An integrated view to its structure and composition (2nd edition). Chapman & Hall, London.
Crossref
 
Clauser, C. (2006). Geothermal Energy. In: Heinloth, K. (Ed.), LandoltBörnstein, Group VIII, Advanced Materials and Technologies. Energy Technologies, Sub volume: C Renewable Energies, Vol. 3. Springer Verlag, Heidelberg-Berlin. Pp. 480-595.
 
Clauser, C., & Huenges, E. (1995). Thermal conductivity of rocks and minerals. In: Ahrens, T.J. (Ed.), Rock Physics and Phase Relations -a Handbook of Physical Constants. AGU Reference Shelf, 3, 105-126.
Crossref
 
Dieokuma, T., Gu, H. M., & Uko, E. D. (2013). Preliminary estimation of thermal conductivity in Bornu-Chad Basin, Nigeria. European Scientific Journal, 9(30), 300-309.
 
Doveton, J. H., & Prensky, S. E. (1992). Geological applications of wireline logs: A synopsis of developments and trends. The Log Analyst, 33(3), 286-303.
 
Emujakporue, G. O. (2017). Subsurface temperature distribution from heat flow conduction equation in part of Chad Sedimentary Basin, Nigeria. Egyptian Journal of Petroleum, 26(2), 519-524.
Crossref
 
Emujakporue, G. O., & Ekine, A. S. (2014). Determination of geothermal gradient in the Eastern Niger Delta Sedimentary Basin from bottom hole temperatures. Journal of Earth Sciences and Geotechnical Engineering, 4(3), 109-114.
 
Faweya, E. B. (2008). Radiogenic heat production in pebble from rocks in Ekiti State, Nigeria. Jurnal Fizik Malaysia. 29(1&2), 21-24.
 
Hamza, V. M., & Beck, A. E. (1972). Terrestrial heat flow: The neutrino problem of vertical distance heat production in the east alps and a possible energy source in the core. Nature, 240, 343-344.
Crossref
 
Harðarson, B. S., (2007). Geothermal exploration and development of the Hengill high-temperature field (presentation). In: Georgsson, L. S., Holm, D. H., Simiyu, S. M., & Ofwona, C. (eds). Short course II on surface exploration for geothermal resources. UNU-GTP & KenGen, Naivasha, Kenya, UNU-GTP CD SC-05, 29p.
 
Jaupart, C., & Mareschal, J. C (2003) Constraints on crustal heat production from heat flow data. In: Treatise of geochemistry (3): The crust. Rudnick, Elsevier. Pp. 65-84.
Crossref
 
Jessop, A. M. (1990). Thermal Geophysics. Elsevier, Amsterdam.
 
Joshua, E. O., & Alabi, O.O. (2012). Pattern of radiogenic heat production in rock samples of Southwestern Nigeria. Journal of Earth Sciences and Geotechnical Engineering, 2(2), 25-38.
 
Kappelmeyer, O., & Haenl, R. (1974). Geothermics. Borntraeger, Berlin, 238p.
 
Kasidi, S., & Nur, A. (2012). Analysis of Aeromagnetic data over Mutum-biyu and environs, Northeastern Nigeria. Research Journal of Engineering and Applied Science, 2(1), 142-148.
 
Kurowska, E., & Schoeneich, K. (2010). Geothermal exploration in Nigeria. Proceedings of World Geothermal Congress. Bali, Indonesia, 25-29 April 2010. Pp. 1-5
 
Kwaya, M. Y., Kurowska, E., & Arabi, A. S. (2016). Geothermal Gradient and Heat Flow in the Nigeria Sector of the Chad Basin, Nigeria. Computational Water, Energy, and Environmental Engineering, 5(2), 70-78.
Crossref
 
Lapworth, D. J., Knights, K. V., Key, R. M., Johnson, C. C., Ayoade, E., Adekanmi, M. A., Arisekola, T. M., Okunlola, O.A., Backman, B., Eklund, M., Everett, P. A., Lister, R. T., Ridgway, J., Watts, M. J., Kemp, S. J., & Pitfield, P. E. J. (2012). Geochemical mapping using stream sediments in west-central Nigeria: Implications for environmental studies and mineral exploration in West Africa. Applied Geochemistry, 27(6), 1035-1052.
Crossref
 
Lee, W. H., & Uyeda, S. (1965). Review of heat flow data. Terrestrial Heat Flow, 8, 87-190.
Crossref
 
Loehnert, E. P. (1985). Hydrochemical and isotope data on Ikogosi warm spring, southwestern Nigeria. In Geothermics, thermal-mineral waters and hydrogeology (pp. 97-109). Theophratus, Athens.
 
Megwara, J. U., Udensi, E. E., Olasehinde, P. I., Daniyan, M. A., & Lawal, K. M. (2013). Geothermal and radioactive heat studies of parts of southern Bida basin, Nigeria and the surrounding basement rocks. International Journal of Basic and Applied Sciences, 2(1), 125-139.
Crossref
 
Nwachukwu, S. O. (1976). Approximate geothermal gradients in Niger Delta sedimentary basin. AAPG Bulletin, 60(7), 1073-1077.
Crossref
 
Nwankwo, L. I., & Sunday, A. J. (2017). Regional estimation of Curie-point depths and succeeding geothermal parameters from recently acquired high-resolution aeromagnetic data of the entire Bida Basin, north-central Nigeria. Geothermal Energy Science, 5(1), 1-9.
Crossref
 
Nwankwo, L. I., Olasehinde, P. I., & Akoshile, C. O. (2011). Heat flow anomalies from the spectral analysis of airborne magnetic data of Nupe Basin, Nigeria. Asian Journal of Earth Sciences, 4(1), 20-28.
Crossref
 
Nwankwo, N. C., Anthony, A. S., & Nwosu, L. I. (2009). Estimation of the heat flow variation in the Chad Basin Nigeria. Journal of Applied Sciences and Environmental Management, 13(1), 73-80.
Crossref
 
Nwobodo, A. N., Ezema, P. O., & Ugwu, G. Z. (2018). Determination of the curie point depth, geothermal gradient and heat flow of Guzabure and its environs, Chad Basin, Nigeria using Aeromagnetic data. International Journal of Scientific and Engineering Research, 9(3), 1876-1889.
 
Odumodu, C. F. R., & Mode, A. W. (2016). Geothermal gradients and heat flow variations in parts of the eastern Niger delta, Nigeria. Journal of the Geological Society of India, 88, 107-118.
Crossref
 
Ofor, N. P., & Udensi, E. E. (2014). Determination of the heat flow in the Sokoto basin, Nigeria using spectral analysis of aeromagnetic data. Journal of Natural Sciences Research, 4(6), 83-93.
 
Ojo, J. S., Olorunfemi, M. O., & Falebita, D. E. (2011). An appraisal of the geologic structure beneath the Ikogosi warm spring in south-western Nigeria using integrated surface geophysical methods. Earth Sciences Research Journal, 15(1), 27-34.
 
Okeyode, I. C. (2012). Radiogenic heat production due to natural radionuclides in the sediments of Ogun River, Nigeria. Journal of Environment and Earth Science, 2(10), 196-207.
 
Okeyode, I. C., & Akanni, A. O. (2009). Determination of some physical parameters of Olumo rock, Abeokuta Ogun-State, Nigeria. Indian Journal of Science and Technology, 2(7), 6-10.
Crossref
 
Oladipo, A. A., Oluyemi, E. A., Tubosun, I. A., Fasisi, M. K., & Ibitoye, F. I. (2005). Chemical examination of Ikogosi warm spring in south western Nigeria. Journal of Applied Sciences, 5(1), 75-79.
Crossref
 
Oladunjoye, M. A., Akinmosin, A., & Ekugum, U. K. (2014). Distribution of radioactive elements of some rocks in South-Western Nigeria. RMZ-M&G, 61, 231-240.
 
Olorunfemi, M. O., Adepelumi, A. A., Falebita, D. E., & Alao, O. A. (2013). Crustal thermal regime of Ikogosi warm spring, Nigeria inferred from aeromagnetic data. Arabian Journal of Geosciences, 6(5), 1657-1667.
Crossref
 
Omokenu, E. G., & Nwosu, L. I. (2016). Statistical analysis of geothermal data of an oil field in parts of Niger Delta, Nigeria. Current Research in Geoscience, 6(2), 91-97.
Crossref
 
Onuoha, K. M., & Ekine, A. S. 2009. Subsurface temperature variations and heat flow in the Anambra Basin, Nigeria. Journal of African Earth Sciences, 28(3), 641-652.
Crossref
 
Onyedim, G., & Awoyemi, M. O. (2015). Geothermal and Hydrocarbon implications of Curie point depths determined from spectral analysis of high resolution aeromagnetic data over parts of Chad basin, Nigeria. Proceedings in International Conference on Green Energy & Expo, September 21-23, 2015, Orlando, USA.
 
Ozoko, D. C., & Ifediegwu, S.I. (2016). Temperature characteristics of boreholes in Umulokpa and environs, Enugu State, Southeastern Nigeria. International Journal of Innovative Science, Engineering and Technology, 3(2), 386-391.
 
Pollack, H. N., Hurter, S. J, & Johnson, J. R. (1993) Heat flow from the earth's interior: analysis of global data set, Reviews of Geophysics, 31:267-280.
Crossref
 
Ray, L., Bhattacharya, A., & Roy, S. (2007). Thermal conductivity of higher Himalayan crystallines from Garhwal Himalaya, India. Tectonophysics, 434(1-4), 71-79.
Crossref
 
Rogers, A. S., Imevbore, A. M. A., &Adegoke, O. S. (1969). Physical and chemical properties of Ikogosi Warm Spring, western Nigeria. Nigeria Journal of Mining Geology, 4, 1-2.
 
Roy, R. F., Beck, A. E., Touloukian, Y. S. (1981). Thermophysical properties of rocks. In: Touloukian, Y.S., Judd, R.R., Roy, R.F. (Eds.). Physical properties of rocks and minerals. McGraw Hill, New York, Pp. 409-502.
 
Rybach, L. (1988). Determination of heat production rate. In: Handbook of terrestrial heat-flow density determination (pp. 125-142). Kluwer Academic Publishers, Dordrecht.
 
Sandiford, M., & McLaren, S. (2005). Thermo-mechanical Controls on Heat Production Distributions and the Long-term Evolution of the Continents. In: Brown, M., & Rushmer, T. (eds.) Evolution and Differentiation of the Continental Crust (pp. 67-92). Cambridge University Press, Cambridge.
 
Sedara, S. O., & Adelowo, A. (2015). Assessment of radiogenic heat production in soil samples around Ife steel rolling mill site in Southwestern Nigeria. International Journal of Innovation and Scientific Research, 13(1), 249-256.
 
Sedara, S. O., Ray, L., & Ojoawo, A. I. (2020). Thermal prospect of the rocks and heat flow estimates in the southwest Nigeria by indirect method: Possibility of geothermal prospect. Unpublished article in press.
 
Sharma, P. V. (2004). Environmental and engineering geophysics. Cambridge University Press, Cambridge. Pp. 357-359.
 
Taylor, S. R. and McLennan, S. M. (1985). The Continental Crust: Its Composition and Evolution, Blackwell, Oxford, p. 312.
 
Verheijen, P. J. T., & Ajakaiye, D. E. (1979). Heat-flow measurements in the Ririwai ring complex, Nigeria. Tectonophysics, 54(1-2), T27-T32.
Crossref