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dc.contributor.authorMati, Bancy M
dc.date.accessioned2013-05-15T06:38:02Z
dc.date.available2013-05-15T06:38:02Z
dc.date.issued1992-03
dc.identifier.citationMati, B.M(1992). The influence of crop cover on soil erosion by splashen
dc.identifier.urihttp://erepository.uonbi.ac.ke:8080/xmlui/handle/123456789/22793
dc.description.abstractThis study involved determining the influence of crop cover on splash erosion. This was done on 16 plots of 4 treatments of maize, beans, intercrop (maize & beans) and bare fallow (control), with 4 replications of each treatment. The highest total amount of splash was recorded on bare fallow land, followed by maize, then beans and intercrop respectively. Soil splash per unit bare space was found to be highest under maize, while beans, intercrop and bare fallow had equal amounts of splash per unit exposed surface area for a given amount of rainfall. The amount of soil splash per mm of rain decreased exponentially with the percent orop cover in all the treatments. For a given percent crop cover, soil splash per mm of rain was constant for maize, beans and intercrop for crop covers less than 40%. For covers exceeding 40%, for a given amount of crop over, splash was highest under maize, followed by beans and intercrop respectively. The amount of splash per mm rain also decreased exponentially with crop height. For a given crop height, splash per mm of rain was highest on maize, followed by intercrop and then beans respectively. The best erosivity factor for splash erosion in this area was the AI45 index, defined as the product of the rainfall amount and its maximum 45-minute intensity, with a correlation coefficient of 0.821. Both the total splash and the splash per exposed area increased with each of the rainfall erosivity indices as power functions. The percent splash transport downslope was found to be unrelated to either rainfall characteristics or crop cover and height. The amount of soil splashed downslope was about 7 times that splashed upslope on bare fallow, and about 6 times on maize cropped plots. For beans and intercrop, power relations existed between upslope and downslope splash, but the overall effect was that the ratio of splash downslope to upslope was less than that for maize and bare fallow plots. The amount of soil splashed downslope decreased with increase in crop cover for all the treatments. For a given percent crop cover, splash downslope was highest under maize, followed by beans and then intercrop respectively. The amount of soil splashed upslope was found to be unrelated to crop cover. The amount of soil splashed both upslope and downslope increased with the rainfall AI~ index. For a given AI~ value, splash downslope was highest on bare fallow, followed by maize, beans and then intercrop respectively. For a given AI45 value, soil splash upslope was highest on bare fallow, and lowest on maize, beans and intercrop equally. statistical. analysis of the basic data showed that replications were not different (a=O.Ol), and daily splash amounts showed highly significant difference (a=O.05). The analysis of variance tests for comparing treatments showed thatJ all treatment pairs were different (a=O.05) except between beans and intercrop. The t-test for the relationships between splash amount and crop cover or rainfall erosivity values, for highly correlated data were all highly significant (a=O.05)en
dc.description.sponsorshipUniversity of Nairobien
dc.language.isoenen
dc.subjectCrop coveren
dc.subjectSoil erosionen
dc.subjectSplashen
dc.titleThe influence of crop cover on soil erosion by splashen
dc.typeThesisen
local.publisherDepartment of Range Management, University of Nairobien


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