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In small fluvial channels in forested areas, huge amounts of leaves, branches and trunks fall and strongly interfere in the streamflow. Sedimentation zones are created in the small lakes formed by dams of organic matter and when they collapse, loads of sediment are released and carried downstream again. Thus, sediment transport occurs as a pulsating process. Furthermore, the organic matter spreads along the channel creating a friction force that decreases streamflow velocity. This paper shows the influence of organic matter on streamflow in first order channels, such as occurred in the small basins of the Tijuca massif (RJ).

INFLUÊNCIA DA VEGETAÇÃO NOS PROCESSOS FLUVIAIS DE BACIAS DE 1ª ORDEM