Effect of the particle size and surface area on attachment to mineral particles in fresh water.

The objective of this study was to assess the effects of the particle size and specific surface area (SSA) on the attachment of to sediment particles. To exclude the effect of different sediment mineral compositions, pure minerals were used, and three typical suspended sediment (<62 μm) components, quartz, K-feldspar and calcite, were separated into four groups with different grain size distributions. Equilibrium attachment experiments covering common concentrations in surface water were conducted for each group. The results show that the finer fractions of each pure mineral had the greatest attachment capacity. Different mineral properties were measured, as well as an author-defined parameter (SSA_a), which was calculated by integrating the particle size distribution and only reflected the microscopic surface areas accessible to cells (∼1 μm) while excluding the effects of nanoscopic pores (5-10 nm). Pearson correlation and partial correlation analyses suggested that the partition coefficient () was positively correlated with the clay content (CC) and SSA_a ( < 0.01). Stepwise multiple regression analysis suggested that SSA_a was the dominant factor ( < 0.01) and was a better explanatory variable than CC. Moreover, in addition to SSA_a, the zeta potential and SSA also partially explained the results ( < 0.05).