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  • 1
    Electronic Resource
    Electronic Resource
    Springer
    Hydrobiologia 176-177 (1989), S. 99-110 
    ISSN: 1573-5117
    Keywords: sediment texture ; fine sediments ; silt/clay ratio ; dispersion ; Great Lakes
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract The dispersion of fine sediment is greatly influenced by factors that induce flocculation, and which thereby determine whether particulates will settle in aggregate form or as discrete grains. The transport and deposition of silt and clay particulates in both marine and non-marine environments may be influenced by flocculation. Because the transport of sediment-associated contaminants is largely influenced by the behaviour of sub sand-size material, it is important to understand the factors which influence patterns of deposition. The silt/clay ratio has been used in an attempt to simplify description of the physical processes of sediment/water interaction, and most examples have been drawn from the Great Lakes. The silt/clay ratio has been related to other characteristics of the total particle-size distribution. As an indicator of many sedimentary conditions, it must be coupled with other measurements of particle-size.
    Type of Medium: Electronic Resource
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  • 2
    Electronic Resource
    Electronic Resource
    Springer
    Hydrobiologia 176-177 (1989), S. 111-124 
    ISSN: 1573-5117
    Keywords: sediment texture ; sand size ; percent mud ; dispersion ; Liverpool Bay ; River Mersey
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract In part 2 of this contribution, examples are drawn from the River Mersey and Liverpool Bay illustrating the use of simple statistical parameters to describe dispersion of sands and muddy sediments. The River Mersey and Liverpool Bay, eastern Irish Sea, were sites of intensive studies on the dispersal of dumped harbour mud and sewage sludge during the mid 1960's–70's. The combined effects of strong tidal scour, wave action and shoreward near-bed residual drift result in shoreward transport of large volumes of sand in the bay. Large amounts of mud (silt/clay mixtures) oscillate in the river estuary, and naturally derived and dumped muds also move shoreward in the bay. Unpublished historic geochemical data have been combined with reprocessed particle size data and both have been used to reassess sedimentological techniques for defining transport and dispersal pathways. River and bay muds have similar size compositions, but river muds have excess Cd 〉 V 〉 U 〉 As = Zn relative to bay muds. The lower relative concentrations of heavy metals in the bay are thought to reflect desorption and degradation of organic matter from the river. Trends in sediment distribution data based on the means of the sand size fraction, alone, provide sensitivities comparable to those of higher order moment measures and are usually easier to interpret than full size spectrum analyses.
    Type of Medium: Electronic Resource
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