Following the success of the Acoustic Doppler Current Profiler (ADCP) technology for monitoring river discharge, there has been a growing interest in the last decade in extracting information on Suspended Sediment Concentration (SSC) from acoustic backscatter in rivers. One major advantage of using sonar systems such as ADCPs or Acoustic Backscatter Systems (ABSs) for monitoring SSC in rivers is the capacity of these instruments to provide measurements at a much higher spatial and temporal resolution than traditional water sampling techniques. Despite the efforts recently made to find a relation between SSC and acoustic backscatter in rivers (e.g., Gray & Gartner, 2009;Venditti et al., 2016), most studies remain empirical and site-specific. Such calibrations shift when sediment properties change which requires intensive water sampling to limit the uncertainty in SSC. The development of more general, physically based methods applicable in rivers is needed.The sonar response of suspended sediments is determined by sound backscattering and sound attenuation. Both processes are strongly determined by the characteristics of the suspended scatterers. Bimodal Particle Size Distributions (PSDs) are commonly observed in rivers (e.g., Agrawal & Hanes, 2015;Armijos et al., 2017). The first mode is usually composed of silt and clay sediment particles that are often fairly homogeneously distributed throughout the river cross-section. We do not expect these particles to gather in large flocs (Burban et al., 1989;Droppo, 2001) as rivers often show low organic matter, no salinity, and relatively high turbulence during high sediment load events such as floods. The impact of flocculation on acoustic backscattering has been studied in other contexts (