Abstract
The mineralogical, chemical, and physical characteristics of sedimentary clay bodies around Share area were studied to establish their potentials as industrial raw materials. The clays occur as interbeds within the Bida Sandstone Formation, which overlies the quartzite-dominated basement rocks of the Northern Bida Basin. Kaolinitic clay samples were collected from six vertical pits and subjected to mineralogical, chemical, and geotechnical analyses. The X-ray diffraction (XRD) mineralogical data show kaolinite (88.17%) as the principal clay mineral, while quartz, muscovite, and paragonite are in minor amounts. The geochemical composition reveals moderate SiO2 (48.58 wt.%) but high Al2O3 (34.34 wt.%) contents, while MgO, CaO, K2O, Na2O, P2O5, Fe2O3, TiO2, MnO, and Cr2O3 contents are generally low in all the samples. The geotechnical parameters indicate a moderate amount of fine particles (64–74%) and plasticity index (6.10–14.45%) and modest bulk density (2.65–2.68 g/cm3) but low shrinkage (2.2–4.3%), loss on ignition (9.90–14.29%), and water absorption capacity (14.04–17.74%). These assessments indicate that the clay bodies around Share area can be used as raw material in ceramic, refractory, paper, paint, plastic, rubber, textile, fertilizer, and petrochemical industries.
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Acknowledgements
The authors are thankful to Olugbenga Fajemila, Olajide Adamolekun, Mikail Olusegun Yusuf, and Abraham Remilekun Adeniyi for analytical and technical support, while the analytical assistance of the technical staff members of the Engineering Geology Laboratory, Department of Applied Geology, The Federal University of Technology Akure, Nigeria, is gratefully acknowledged. The editorial review of the editor-in-chief and two anonymous reviewers are deeply appreciated.
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Olawale Kayode Aromolaran and Abdulrauf Bukola Adebayo carried out the research work and analyzed the data for this work. Olawale Kayode Aromolaran drafted the manuscript. All authors approved the final manuscript.
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Highlights
1. Kaolinitic claystones in Share area occur as lenses and interbeds within the Bida Sandstone Formation.
2. Compositional and physical data show the clays predominantly consist of kaolin minerals that are chemically pure with suitable physical characteristics.
3. Share kaolinitic claystones have exploitable potentials in refractory, paper, paint, fertilizer, petrochemical, and cement industries.
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Aromolaran, O.K., Adebayo, A.B. Mineralogical, geochemical, and industrial appraisal of kaolinitic claystones in Share area, northcentral Nigeria. Arab J Geosci 15, 789 (2022). https://doi.org/10.1007/s12517-022-09825-6
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DOI: https://doi.org/10.1007/s12517-022-09825-6