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The study investigates the sedimentary processes and mechanisms that lead to the braiding of gravel-bed rivers using small-scale hydraulic models. Four primary processes were identified: deposition and accumulation of central bars, chute cutoffs of point bars, conversion of transverse unit bars to braid bars, and dissection of multiple bars, with the chute cutoff being the most common. The onset of braiding is primarily driven by local aggradation and loss of flow competence, influenced by sediment mobility

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toufiq952251

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EN