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dc.contributor.authorMwaniki, Mercy W.
dc.contributor.authorAgutu, Nathan O.
dc.contributor.authorMbaka, John G.
dc.contributor.authorNgigi, Thomas G.
dc.contributor.authorWaithaka, Edward H.
dc.date.accessioned2019-08-21T11:24:17Z
dc.date.available2019-08-21T11:24:17Z
dc.date.issued2015
dc.identifier.urihttp://ir.mksu.ac.ke/handle/123456780/4753
dc.description.abstractLandsat series multispectral remote sensing imagery has gained increasing attention in providing solutions to environmental problems such as land degradation which exacerbate soil erosion and landslide disasters in the case of rainfall events. Multispectral data has facilitated the mapping of soils, land-cover and structural geology, all of which are factors affecting landslide occurrence. The main aim of this research was to develop a methodology to visualize and map past landslides as well as identify land degradation effects through soil erosion and land-use using remote sensing techniques in the central region of Kenya. The study area has rugged terrain and rainfall has been the main source of landslide trigger. The methodology comprised visualizing landslide scars using a False Colour Composite (FCC) and mapping soil erodibility using FCC components applying expert based classification. The components of the FCC were: the first independent component (IC1), Principal Component (PC) with most geological information, and a Normalised Difference Index (NDI) involving Landsat TM/ETMþ band 7 and 3. The FCC components formed the inputs for knowledge-based classification with the following 13 classes: runoff, extreme erosions, other erosions, landslide areas, highly erodible, stable, exposed volcanic rocks, agriculture, green forest, new forest regrowth areas, clear, turbid and salty water. Validation of the mapped landslide areas with field GPS locations of landslide affected areas showed that 66% of the points coincided well with landslide areas mapped in the year 2000. The classification maps showed landslide areas on the steep ridge faces, other erosions in agricultural areas, highly erodible zones being already weathered rocks, while runoff were mainly fluvial deposits. Thus, landuse and rainfall processes play a major role in inducing landslides in the study area.en_US
dc.language.isoen_USen_US
dc.publisherPergamonen_US
dc.subjectLandslide scaren_US
dc.subjectSoil erodibility mappingen_US
dc.subjectPrincipal component analysis (PCA)en_US
dc.subjectFalse colour composite (FCC)en_US
dc.subjectIndependent component analysis (ICA)en_US
dc.subjectNormalised difference index (NDI)en_US
dc.subjectNormalised difference mid red (NDMIDR)en_US
dc.titleLandslide scar/soil erodibility mapping using Landsat TM/ETMþ bands 7 and 3 Normalised Difference Index: A case study of central region of Kenyaen_US
dc.typeArticleen_US


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