1992
DOI: 10.1007/bf00026196
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Flocculation and its effect on the vertical transport of fine-grained sediments

Abstract: Recent experimental and theoretical work on flocculation and settling speeds of flocs is reviewed. On the basis of this work, an accurate and computationally efficient model of the aggregation and disaggregation of fine-grained sediments is proposed . This model is then used to predict flocculation times and steady-state floc sizes for a wide range of environmental conditions. The predicted flocculation times are smaller, sometimes by as much as two orders of magnitude, than those predicted by mono-disperse th… Show more

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Cited by 61 publications
(29 citation statements)
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“…Flocculation is a dynamic process where rates of aggregation and disaggregation depend on local environmental variables such as fluid shear, particle concentration, salinity, dissolved chemicals, pH, temperature and organisms (Lick et al 1992). Accordingly in an early study, Mulholland (1981) found that the addition of Ca ?2 and Mg ?2 to a softwater lake caused an increase in the rate of POM formation as a result of a rapid physicochemical flocculation process.…”
Section: Introductionmentioning
confidence: 99%
“…Flocculation is a dynamic process where rates of aggregation and disaggregation depend on local environmental variables such as fluid shear, particle concentration, salinity, dissolved chemicals, pH, temperature and organisms (Lick et al 1992). Accordingly in an early study, Mulholland (1981) found that the addition of Ca ?2 and Mg ?2 to a softwater lake caused an increase in the rate of POM formation as a result of a rapid physicochemical flocculation process.…”
Section: Introductionmentioning
confidence: 99%
“…e c is an efficiency parameter describing the possibility of the collisions that will result in flocculation. As discussed by Lick, Lick, and Ziegler (1992), e c is a variable of floc size and floc density and at the present difficult to determine and therefore e c is assumed to be constant for simplicity. e d is a parameter describing the turbulent diffusion.…”
Section: Floc Development Modelmentioning
confidence: 99%
“…Organic-rich sediment is typically composed of aggregates of detrital organic material and bacteria joined with varied types and sizes of mineral material (Lick et al, 1992;Sterling et al, 2005). Flocculation significantly influences fluxes and redistribution of sediment and associated nutrients or contaminants (Walling and Moorhead, 1989;Droppo, 2003Droppo, , 2004.…”
Section: Physical-biological Interactions In River and Floodplain Cormentioning
confidence: 99%