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Applied and Environmental Soil Science
Volume 2018 (2018), Article ID 8562698, 12 pages
Research Article

Quantification and Evaluation of Soil Erosion in the Estuaries of Cameroon, Gulf of Guinea: Case of Nylon Area

1Department of Mechanical and Electrical Engineering, ENSET, University of Douala, P.O. Box 1872, Douala, Cameroon
2Department of Energy Engineering, IUT, University of N'gaoundere, P.O. Box 455, N'gaoundere, Cameroon
3Department of Civil Engineering, ENSET, University of Douala, P.O. Box 1872, Douala, Cameroon

Correspondence should be addressed to Eric Flavien Mbiakouo-Djomo; rf.oohay@cire_ouokaibm

Received 14 May 2017; Revised 20 November 2017; Accepted 22 November 2017; Published 11 February 2018

Academic Editor: Paul Voroney

Copyright © 2018 Eric Flavien Mbiakouo-Djomo et al. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.


The area of Nylon represents a sensible and vulnerable environment where water erosion is the cause of many soil losses contributing to the production and movement of sediments from the upstream to the lowest depths. The high level of rainfall in this town, soil texture (sand-clay-silt), and the anarchic occupation of the area play a part in the important deterioration of the bare ground on the upstream of the catchment area. This causes with time an instability of structures and living places which can lead to their progressive disappearance. In order to assess the quantities of displaced sediments, the studies on the quantification of soil moved annually by water erosion are carried out. A direct method is used consisting in using a minisimulator of rain (NEME) in order to understand the phenomena involved and assess the quantity of sediments which can be moved. It helps in assessing erosion caused by the rain and extrapolating results over the catchment area of the chosen field of study. USLE relation has permit to make an extrapolation of the quantity of soil affected, and the result shows that the average potential of loss of soil is 153.57 t/ha/annum.