INFLUÊNCIA DA COBERTURA DO SOLO NAS PERDAS DE ÁGUA E DESAGREGAÇÃO DO SOLO EM ENTRESSULCOS
2009
Sandro Augusto Bezerra | José Ramon Barros Cantalice
The process of water erosion soil involves the detachment of particles soil by raindrop impact, the transport and consequently your deposition, by overland flow of water on the soil. This drainage happens in the flow form to laminate shallow what characterizes the interrill erosion. The work evaluated the efficiency in the different ways of soil cover provided by the sugarcane in the control of the losses of water and of the rates of detachment of the soil. The appraised treatments were: bary soil, residue under surface; dossal of the sugarcane and the added effect of the residue + dossal. The regime of found drainage, to laminate slow, it characterizes the interril erosion. The vegetable covering promoted by the culture of the sugarcane it promoted reduction in the rates of detachment of the soil. The residue in direct contact with soil and with the drainage it was responsible for the increment of the rugosidade, however, it provided low infiltration rates with consequent increase of the rates of loss of water, for constituting in a vegetable layer that hindered the infiltration. The dossal of the cane of suugarcane promoted a larger interception of the rain, delaying the beginning of the drainage, checking the largest infiltration rates obtained.
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