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DC Field | Value | Language |
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dc.contributor.author | Falaiye, O. A. | - |
dc.contributor.author | Yakubu, A. T. | - |
dc.contributor.author | Aweda, F. O. | - |
dc.contributor.author | Abimbola, O. J. | - |
dc.date.accessioned | 2023-04-13T13:43:19Z | - |
dc.date.available | 2023-04-13T13:43:19Z | - |
dc.date.issued | 2013-01-30 | - |
dc.identifier.citation | Falaiye, 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.uri | ir.bowen.edu.ng:8080/jspui/handle/123456789/1032 | - |
dc.description.abstract | Mineralogical 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.iso | en | en_US |
dc.publisher | Ife Journal of Science | en_US |
dc.subject | Bodele depression | en_US |
dc.subject | Harmattan dust | en_US |
dc.subject | Mineralogy | en_US |
dc.subject | Ilorin | en_US |
dc.title | Mineralogy characteristics of harmattan dust in Ilorin, Sub-Sahara Africa | en_US |
dc.type | Article | en_US |
Appears in Collections: | Articles |
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File | Description | Size | Format | |
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Falaiye et al 2013 (Ife Journal of Science).pdf | Research Article | 817.42 kB | Adobe PDF | View/Open |
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