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Please use this identifier to cite or link to this item: http://ir.futminna.edu.ng:8080/jspui/handle/123456789/2263
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dc.contributor.authorAlhassan, Musa-
dc.contributor.authorMesaiyete, Ebun-
dc.contributor.authorAlhaji, Mustapha Mohammed-
dc.date.accessioned2021-06-08T20:14:14Z-
dc.date.available2021-06-08T20:14:14Z-
dc.date.issued2012-
dc.identifier.citationAlhassan. M., Mesaiyete, E. and Alhaji, M. M. (2012). Clay Mineralogy of Lateritic Soils Derived from Granite Basement – A Case Study of Minna Lateritic Soils. Electronic Journal of Geotechnical Engineering, Oklahoma, USA, vol. 17(M), pp. 1897–1903en_US
dc.identifier.urihttp://www.ejge.com/2012/JourTOC17M.htm-
dc.identifier.urihttp://repository.futminna.edu.ng:8080/jspui/handle/123456789/2263-
dc.description.abstractLateritic soils samples taken from four different locations around Minna were subjected to clay mineralogical analysis using X-ray diffraction method. The results show three of the soil samples containing mostly kaolinite as their main clay mineral, while the fourth sample shows the presence of a mineral of the chlorite group. The study shows that kaolinite is the predominant clay mineral present within lateritic soil profiles found around Minna.en_US
dc.language.isoenen_US
dc.publisherElectronic Journal of Geotechnical Engineering, Oklahoma, USAen_US
dc.relation.ispartofseriesvol. 17(M);-
dc.subjectLateritic soil; Clay mineral; X-ray diffractionen_US
dc.titleClay Mineralogy of Lateritic Soils Derived from Granite Basement – A Case Study of Minna Lateritic Soilsen_US
dc.typeArticleen_US
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