4.5 Article

In situ particle size spectra and density of particle aggregates in a dredging plume

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MARINE GEOLOGY
卷 170, 期 3-4, 页码 443-459

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ELSEVIER
DOI: 10.1016/S0025-3227(00)00105-5

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laser in situ scattering and transmissometry; flocculation; floc density; grain-size analysis; settling; suspended sediment

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An in situ laser particle sizer, the LISST-100, was used to describe the spatial variation of beam attenuation coefficient, in situ particle size spectra and aggregate densities in a dredging plume in the sound Oresund between Denmark and Sweden. The results proved that the above mentioned parameters varied significantly within the investigated length of the plume (approximately 2 km). It is shown how the small single primary particles aggregate and change the in situ particle size spectra into a slightly better sorted and coarser size distribution, and at the same time how the mean density of particles/aggregates decreases significantly. This shift in the state in which the particles exist in the water effectively changes the optical response of the mass of particles suspended in the water. It is shown that adequate correlations between mass concentrations and beam attenuation coefficients can only be obtained if parameters describing the in situ quality and state of the mass of particles, e.g. standard deviation of the size spectra and volume concentration, is included in the regression. From the spatial variation in mean density and in situ particle size, it was possible to calculate the spatial difference in settling velocity. It was found that the difference in settling velocity was only about a factor of 1.7, because increasing in situ particle size was counter-balanced by decreasing mean density. Furthermore, the time-scale of flocculation within the plume was found to be in the order of 50 min. (C) 2000 Elsevier Science B.V. All rights reserved.

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