Abstract
The interplay between cohesive sediment flocculation, turbulence, and sediment availability is studied using field observations collected on the muddy Atchafalaya inner shelf, Louisiana, USA. Observations were made at two sites, characterized by surficial sediments of different grain size. At the coarse-sediment site, a negative correlation between floc size and suspended sediment concentration was observed for the first time in a field experiment under energetic wave conditions. This agrees with previous laboratory studies and field observations, and suggests that strong near-bed turbulence associated with significant sediment resuspension also results in the breaking of macro-flocs (230-μm mode). At the fine-sediment site, the relative abundance of clay and fine silt available for flocculation appears to promote persistent macro-flocs of approximately 300-μm. The observations support the assumption that sediment supply and surficial sediment properties, in addition to turbulence and suspended sediment concentration, play an important role in flocculation.
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