The study determined the physical properties and comminution work index of Ebiti phosphate rock and analysed its particle size and mineralogical properties. These were with a view to generating data baseline for further advanced characterisation of the rock for use in some industrial engineering applications. The phosphate rocks were sourced from Ebiti Village, Ifo Local Government Area, Ogun State. The rocks were crushed and ground with Pascal Engineering crusher and ball mill, respectively. Textural forms, colour, water absorption capacity, specific gravity, Moh hardness tests were performed to determine their physical properties. Comminution work index was also caried out to determine the energy required to reduce the phosphate rock samples to a specific particle size. Thereafter, petrographic analysis was performed to determine their mineralogical and textural features. The study showed that Ebiti phosphate rock occurs as nodular and versicular form with dead white or creamy colour. It has 5.0 hardness on the Moh’s Scale, which indicates a medium resistance to abrasion and crushing. Its apparent specific gravity was 2.65 and water absorption capacity was 12.74%. Particle size analysis showed that percentage of cumulative weight retained increases down the sieve series. Thin Section Microscopy revealed nodules, vesicles with dark spots. The study concluded that Ebiti phosphate rock is sedimentary and has comminution work index of 16.97 Kwh/tons.
References
[1]
Ryszko, U., Rusek, P. and Kołodyńska, D. (2023) Quality of Phosphate Rocks from Various Deposits Used in Wet Phosphoric Acid and P-Fertilizer Production. Materials, 16, Article 793. https://doi.org/10.3390/ma16020793
[2]
El Bamiki, R., Raji, O., Ouabid, M., Elghali, A., Khadiri Yazami, O. and Bodinier, J. (2021) Phosphate Rocks: A Review of Sedimentary and Igneous Occurrences in Morocco. Minerals, 11, Article 1137. https://doi.org/10.3390/min11101137
[3]
Fayiga, A.O. and Nwoke, O.C. (2016) Phosphate Rock: Origin, Importance, Environmental Impacts, and Future Roles. EnvironmentalReviews, 24, 403-415. https://doi.org/10.1139/er-2016-0003
[4]
Obaje, S.O., Okosun, E.A., Amoka, I.S. and Kwaha, J.Z. (2014) Geochemical Characterization and Ore Dressing Potential of Sokoto Phosphate Rock, Northwestern Nigeria. UniversalJournalofGeoscience, 2, 187-194. https://doi.org/10.13189/ujg.2014.020701
[5]
Fayiga, A.O. and Obigbesan, G.O. (2017) Physico-Chemical Characterization of Ogun and Sokoto Phosphate Rocks. GlobalJournalofPureandAppliedSciences, 23, 27-34. https://doi.org/10.4314/gjpas.v23i1.4
[6]
Adesanwo, O.O., Dunlevey, J.N., Adetunji, M.T., Adesanwo, J.K., Diatta, S. and Osiname, O.A. (2010) Geochemistry and Mineralogy of Ogun Phosphate Rock. AfricanJournalofEnvironmentalScienceandTechnology, 4, 698-708.
[7]
Olanipekun, T. and Bolarinwa, A. (2020) Petrographic Analysis of the Palaeocene-Eocene Phosphate-Bearing Rocks of Eastern Dahomey Basin, Southwestern Nigeria. Research Square, 1-11.
[8]
Fuerstenau, M.C. and Han, K.N. (2003) Principles of Mineral Processing. Society for Mining, Metallurgy, and Exploration, Englewood, CO, 185-188.
[9]
Adeleke, A.A. (2023) Mineral Processing Technology. CRC Press. https://doi.org/10.1201/9781003323433
[10]
Oji, E.O., Omah, A.D. and Onymisi, Y.H. (2023) Ddetermination of Bond Work Index of Bagega Gold Mineral Deposit of Zamfara State, Nigeria. NigerianJournalofTechnology, 42, 244-248. https://doi.org/10.4314/njt.v42i2.12
[11]
Umar, A.H., Yaro, S.A., Abdulwahab, M. and Dodo, M.R. (2016) Characterization of Sokoto Phosphate Rock for Beneficiation. JournalofRawMaterialsResearch, 10, 74-93.
[12]
Tikpangi, K.M. and Olonkwoh, S.S. (2015) Major Oxides and Trace Elements Composition of Phosphate-Bearing Sedimentary Rocks. AmericanJournalofEnvironmentalProtection, 3, 106-111.
[13]
ASTM (2023) C128-15 Standard Test Method for Relative Density (Specific Gravity) and Absorption of Fine Aggregate.
[14]
Berry, R.C. and Bruce, W. (1966) Work Index Determination and Grinding Efficiency. TransactionsoftheInstitutionofMiningandMetallurgy, SectionC, 75, C56-C65.