Abstract
In this work was monitoring the morphological evolution of a river (Glane) following development thresholds. Erasing the obstacle caused a strong release of fine sediment towards downstream. A change of particle size distribution is well observed in the area with increased downstream fine and coarse appearance of the upstream substrate. In the short term, an improved hydro-morphological characteristic was observed upstream to the arranged threshold. Future measurements campaigns will verify the sustainability of these changes.
Cuvinte cheie
Morphology
sediment transport
flow facies
substrates