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Haregeweyn, N., Poesen, J., Verstraeten, G., Govers, G., De Vente, J., Nyssen, J., Deckers, J. & Moeyersons, J. 2011. ‘Assessing the performance of a spatially distributed soil erosion and sediment delivery model (SEDEM) in Northern Ethiopia’. land degradation & development. Wiley. DOI: DOI: 10.1002/ldr.1121.
Article in a scientific Journal / Article in a Journal
Most regional‐scale soil erosion models are spatially lumped and hence have limited application to practical problems such as the
evaluation of the spatial variability of soil erosion and sediment delivery within a catchment. Therefore, the objectives of this study were
as follows: (i) to calibrate and assess the performance of a spatially distributed WATEM/SEDEM model in predicting absolute sediment
yield and specific sediment yield from 12 catchments in Tigray (Ethiopia) by using two different sediment transport capacity equations
(original and modified) and (ii) to assess the performance of WATEM/SEDEM for the identification of critical sediment source areas
needed for targeting catchment management.
The performance of the two model versions for sediment yield was found promising for the 12 catchments. For both versions, model
performance for the nine catchments with limited gully erosion was clearly better than the performance obtained when including the three
catchments with significant gully erosion. Moreover, there is no significant difference (alpha 5 per cent) between the performances of the two
model versions.
Cultivated lands were found to be on average five times more prone to erosion than bush–shrub lands. The predicted soil loss values in
most parts of Gindae catchment are generally high as compared with the soil formation rates. This emphasises the importance of
implementing appropriate soil and water conservation measures in critical sediment source areas prioritising the steepest part of the
catchment (i.e. areas with slope >50 per cent).
The applicability of the WATEM/SEDEM model to environments where gully erosion is important requires the incorporation of
permanent gully and bank gully erosion in the model structure. Copyright # 2011 John Wiley & Sons, Ltd.