1994
DOI: 10.1016/0025-3227(94)90009-4
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inssev: An instrument to measure the size and settling velocity of flocs in situ

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Cited by 209 publications
(103 citation statements)
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“…In situ settling velocities of fine-grained sediments are most commonly obtained using various settling column systems (Owen 1976;Dyer et al 1996), some of which are equipped with video cameras (Van Leussen and Cornelisse 1993;Fennessy et al 1994). Video-equipped settling columns usually provide floc size and settling velocity data, and several relationships between in situ floc size and settling velocity have been published Sternberg et al 1999;Mikkelsen and Pejrup 2001).…”
mentioning
confidence: 99%
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“…In situ settling velocities of fine-grained sediments are most commonly obtained using various settling column systems (Owen 1976;Dyer et al 1996), some of which are equipped with video cameras (Van Leussen and Cornelisse 1993;Fennessy et al 1994). Video-equipped settling columns usually provide floc size and settling velocity data, and several relationships between in situ floc size and settling velocity have been published Sternberg et al 1999;Mikkelsen and Pejrup 2001).…”
mentioning
confidence: 99%
“…Video-equipped settling columns usually provide floc size and settling velocity data, and several relationships between in situ floc size and settling velocity have been published Sternberg et al 1999;Mikkelsen and Pejrup 2001). Assuming Stokes Law, the densities of the flocs as a function of their size can subsequently be calculated and particle mass and/or settling fluxes can be derived for individual floc size classes (Syvitski et al 1995;Fennessy et al 1997;Hill et al 1998;Sternberg et al 1999;Manning and Dyer 2002).…”
mentioning
confidence: 99%
“…These microflocs can develop into large, but low dense flocs called macroflocs which behave very differently. Macroflocs have a diameter larger than 100 µm and a settling velocity between 1-15 mm/s (Fennessy et al 1994;Manning and Dyer 1999;Manning 2001;Manning et al 2013). …”
Section: Introductionmentioning
confidence: 99%
“…The flocculation process mainly occurs in the very low salinity region (between 1 and 2.5 ppt) (Wollast 1988), and it is affected by hydrodynamic changes which can alter the suspended sediment particle by modifying its effective particle size, shape, porosity, density and composition. Numerous studies have been carried out to investigate the flocculation phenomenon in the laboratory, such as (Serra et al 1997;Manning and Dyer 1999;Mikes et al 2004;Maggi 2005) and in situ (Fennessy et al 1994;Syvitski et al 1995;van Leussen and Cornelisse 1996). Due to the complexity of the natural system, many simplifications are made in laboratory studies in order to control the different variable parameters in the flocculation process.…”
Section: Introductionmentioning
confidence: 99%
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