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dc.contributor.authorOwido, Seth FO
dc.date.accessioned2013-05-27T07:09:17Z
dc.date.available2013-05-27T07:09:17Z
dc.date.issued1981
dc.identifier.citationDegree of Master of Science in the University of Nairobi,en
dc.identifier.urihttp://erepository.uonbi.ac.ke:8080/xmlui/handle/123456789/26026
dc.descriptionA thesis submitted in partial fulfilment for the Degree of Master of Science in the University of Nairobi, Department of Soil Scienceen
dc.description.abstractThe red soils occupy some parts of Mwea Irrigation Scheme. In particular, the Tebere Section of the Scheme has these. soils occurring at higher elevations than the black cotton soils which occur in the depressions. The black soils are irrigated under rice cultivation. The red soils in Tebere are irrigated to a limited extent. The irrigated plots are grown with vegetable and fruit trees. The red soils (kaolinitic clay loams) have extremely high infiltration rates. The result of their irrigation is that water percolates into deeper layers, consequently finding its way by seepage to lower lying black soils. The main canals which supply irrigation water to Tebere Section also run over the red soils. For all their lengths the canals (left and right branches) are not lined and therefore water losses from them is a possible source on the drainage problems , However, the total surface area of the canal is far less than that of the basin and furrow irrigated plot on which water use efficiency has been studied. Although the present study reveals that canal losses and deep percolation losses contribute substantially to the poor drainage of the black soils, rainfall has also been identified as an important component.en
dc.language.isoenen
dc.publisherUniversity of Nairobien
dc.titleA study of the drainage problems in some part of The Mwea Irrigation Scheme, Kenyaen
dc.typeThesisen
local.publisherDepartment of Soil Scienceen


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