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Please use this identifier to cite or link to this item: ir.bowen.edu.ng:8181/jspui/handle/123456789/1032
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dc.contributor.authorFalaiye, O. A.-
dc.contributor.authorYakubu, A. T.-
dc.contributor.authorAweda, F. O.-
dc.contributor.authorAbimbola, O. J.-
dc.date.accessioned2023-04-13T13:43:19Z-
dc.date.available2023-04-13T13:43:19Z-
dc.date.issued2013-01-30-
dc.identifier.citationFalaiye, O. A. Yakubu, A. T. Aweda, F. O. & Abimbola, O. J. (2013). Mineralogical characteristics of harmattan dust in Ilorin, Sub-Sahara Africa. Ife Journal of Science, 15 (1), 175-181.en_US
dc.identifier.uriir.bowen.edu.ng:8080/jspui/handle/123456789/1032-
dc.description.abstractMineralogical study was carried out on harmattan dust samples collected over Ilorin (8° 32' N, 4° 34' E) sub-Sahara region of West Africa. Minerals such as quartz [SiO ] (76.5%), gibbsite [Al(OH) ] (7.1%), rutile [TiO ] 2 3 2(5.8%), goethite [Fe O .H O] (4.6%), halloysite [Al Si O (OH) ·8H O] (3.9%) and kaolinite [Al Si O (OH) ] 2 3 2 4 4 10 8 2 4 4 10 8 (2.1%) were detected. Quartz, halloysite, microcline and mica were similarly identified in harmattan dust sampled at Ile-Ife. However, gibbsite, rutile, goethite which were identified at Ilorin were not detected at Ile-Ife, while microcline and mica detected in Ile-Ife were not observed at Ilorin. The mineralogical composition of the harmattan dust at a locality is most probably determined by the source and the distance from the source of the harmattan dust.en_US
dc.language.isoenen_US
dc.publisherIfe Journal of Scienceen_US
dc.subjectBodele depressionen_US
dc.subjectHarmattan dusten_US
dc.subjectMineralogyen_US
dc.subjectIlorinen_US
dc.titleMineralogy characteristics of harmattan dust in Ilorin, Sub-Sahara Africaen_US
dc.typeArticleen_US
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