“…In principle, flocculation depends on a number of local environmental conditions, for example, turbulence, cation concentration, SPM concentration as a proxy particle number density, mineral composition, POM concentration and composition (e.g., TEP) and microorganism (Dyer, 1989;Keyvani & Strom, 2014;Lai et al, 2018;Manning et al, 2010;Mietta et al, 2009;Zhang et al, 2021). The bulk mineralogical composition of the SPM in the study area is relatively constant and consists of 32%-39% clays, 25%-33% carbonates, 12%-18% quartz, 11%-15% amorphous silicates, and 5%-8% feldspars and accessory minerals (Adriaens et al, 2018). The cation concentrations are high and well above the threshold for salinity induced flocculation so that flocculation in the study area is above all controlled by the OM composition of the SPM, the SPM concentration and the hydrodynamic conditions.…”