Please use this identifier to cite or link to this item: http://repository.futminna.edu.ng:8080/jspui/handle/123456789/9640
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dc.contributor.authorMusa, Alhassan-
dc.contributor.authorEbbun, Mesaiyete-
dc.contributor.authorAlhaji, Mustapha Mohammed-
dc.date.accessioned2021-07-15T15:04:34Z-
dc.date.available2021-07-15T15:04:34Z-
dc.date.issued2012-
dc.identifier.citationM. Alhassan, E. Mesaiyete and M. M. Alhaji (2012), Clay Mineralogy of Lateritic Soils Derived from Granite Basement - A Case study of Minna Lateritic soils, Electronic Journal of Geotechnical Engineering, Vol. 17, Bundle M, Pp 1897-1903en_US
dc.identifier.issn1089-3032-
dc.identifier.urihttp://repository.futminna.edu.ng:8080/jspui/handle/123456789/9640-
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 Minnaen_US
dc.description.sponsorshipSelf sponsoreden_US
dc.language.isoenen_US
dc.publisherElectronic Journal of Geotechnical Engineeringen_US
dc.relation.ispartofseriesVol. 17;Bundle M-
dc.subjectLateritic soilen_US
dc.subjectClay mineral,en_US
dc.subjectX-ray Diffractionen_US
dc.titleClay Mineralogy of Lateritic Soils Derived from Granite Basement - A Case study of Minna Lateritic soilsen_US
dc.typeArticleen_US
Appears in Collections:Civil Engineering

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