“…For instance, bimodal FSD with one peak at clay/silt size and the other at sand side indicates either the aggregation of silt and/or clay or intense erosion events of sand (Lee et al, ). Moreover, for realistic sediment modeling, knowledge of FSD is important for the selection of subordinate unimodal lognormal FSDs (e.g., Lee et al, ; Shen, Lee, et al, ; Shen, Toorman, et al, ), and the median floc size ( D 50 ), which is a crucial parameter.…”