Non-equilibrium flocculation characteristics of fine-grained sediments in grid-generated turbulent flow

• Published in: Coastal engineering (Amsterdam) Vol. 57; no. 4; pp. 447 - 460
• Main Authors: Cuthbertson, Alan J.S., Dong, Ping, Davies, Peter A.
• Format: Journal Article
• Language: English
• Published: Kidlington Elsevier B.V 01.04.2010; Elsevier
• Subjects: Agglomeration; Aggregation; Cohesive sediment; Earth sciences; Earth, ocean, space; Engineering and environment geology. Geothermics; Engineering geology; Exact sciences and technology; Flocculation; Fluid dynamics; Geomorphology, landform evolution; Kaolin; Marine and continental quaternary; Oscillating grid turbulence; Sand; Sand–mud mixtures; Settling; Shear rate; Surficial geology; Turbulence; Turbulent flow; Aggregation; Cohesive sediment; Oscillating grid turbulence; Flocculation; Sand–mud mixtures; experimental studies; time variations; shear; fine-grained materials; turbulent flow; aggregation; concentration; hydrodynamics; turbulence; flocculation; grains; Sand-mud mixtures; sand; correlation; equilibrium; reduction; mud; suspension
• ISSN: 0378-3839; 1872-7379
• DOI: 10.1016/j.coastaleng.2009.11.011

Results are presented from a series of settling column experiments investigating temporal variations in the flocculation characteristics of purely cohesive (kaolin clay) sediment suspensions and cohesive (kaolin) and non-cohesive (fine sand) sediment fraction mixtures. Experimental runs were conducted under controlled hydrodynamic conditions generated by a rigid array of in-phase oscillating grids. The results indicated that rapid initial floc aggregation occurred under low turbulent shear rates, with peak maximal and root-mean-square (r.m.s.) floc sizes (∼ 400 μm and ∼ 200 μm, respectively) attained after relatively short time periods, before reducing with time. By contrast, lower aggregation rates and smaller floc sizes were observed under higher shear conditions, with flocs retaining suspended in the settling column for longer time scales due to the increased turbulence. The mud input concentration displayed some correlation with maximal and r.m.s. floc sizes at higher shear rates but no correlation was apparent at low shear rates. This observed floc behaviour may be attributed to the differences in concentration gradients at high and low shear rates that affect both floc settling rate and time required for flocs to attain equilibrium size. The addition of the fine sand fraction to the kaolin clay suspension reduced both the initial floc formation (i.e. aggregation) rate and the maximal and r.m.s. floc sizes attained throughout the experiments. The reduction in maximal floc sizes appeared to be enhanced by an increase in the ratio of fine sand to kaolin clay content within the mixture.