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The particle size characteristics of fluvial suspended sediment: an overview

  • Conference paper
Sediment/Water Interactions

Part of the book series: Developments in Hydrobiology ((DIHY,volume 50))

Abstract

The particle size characteristics of suspended sediment are of fundamental importance in understanding its role in a variety of environmental processes. Existing knowledge concerning the spatial and temporal variability of the grain size composition of suspended sediment is, however, relatively limited. At the global scale, major contrasts may exist between individual rivers in the calibre of their suspended load and this may be related to a number of controls including climate, catchment geology and basin scale. Any attempt to understand the precise relationship between the grain size characteristics of suspended sediment and those of its source material must also take account of the selectivity of erosion and delivery processes. A local case study undertaken by the authors in the 1500 km2 basin of the River Exe in Devon, UK is used to illustrate the considerable spatial variability that may occur within a relatively small area and the complexity of the associated controls.

Available evidence concerning the temporal variability of the grain size characteristics of suspended sediment emphasises the diverse patterns of behaviour that may exist and the complexity of the controls involved. In some rivers the sediment may become coarser as flow increases, in others it may become finer, whilst in others it may exhibit a relatively constant grain size composition. Data from the local case study in the Exe basin are again used to highlight the considerable diversity in response to changing discharge that may occur within a relatively small area.

Any attempt to understand the dynamics of sediment movement through a river system must also take account of the potential contrast between the ultimate and effective particle size distribution of suspended sediment in response to aggregation. Results from the Exe basin study indicate that even in rivers with relatively low solute concentrations, almost an order of magnitude difference may exist between the median particle size associated with the ultimate and effective grain size distributions.

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Authors and Affiliations

  1. Department of Geography, University of Exeter, Exeter, EX4 4RJ, UK

    D. E. Walling & P. W. Moorehead

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  1. D. E. Walling
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  2. P. W. Moorehead
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Editors and Affiliations

  1. Rawson Academy of Aquatic Science, 404 - 1 Nicholas Street, K1N 7B7, Ottawa, Ontario, Canada

    Peter G. Sly

  2. Stream Ecology Centre, Chisholm Institute of Technology, 3145, Caulfield East, Victoria, Australia

    Barry T. Hart

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© 1989 Kluwer Academic Publishers

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Walling, D.E., Moorehead, P.W. (1989). The particle size characteristics of fluvial suspended sediment: an overview. In: Sly, P.G., Hart, B.T. (eds) Sediment/Water Interactions. Developments in Hydrobiology, vol 50. Springer, Dordrecht. https://doi.org/10.1007/978-94-009-2376-8_12

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  • DOI: https://doi.org/10.1007/978-94-009-2376-8_12

  • Publisher Name: Springer, Dordrecht

  • Print ISBN: 978-94-010-9007-0

  • Online ISBN: 978-94-009-2376-8

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