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Importance of sediments in understanding nutrient cyclings in lakes

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Sediment/Water Interactions

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

Abstract

Inorganic and organic nutrients are continuously transported to lake bottoms by sedimentation. By various biological, physical, chemical and mechanical processes quantities of certain nutrients can be brought back to the free water again. This cycling between the sediments and water may occur according to various schemes dependent on lake type and bottom conditions. Lake morphology, temperature regimes, trophic level and sediment type can all strongly influence the size of nutrient pools and rates of turnover.

The various activities of bacteria, benthic algae, macrophytes, benthic invertebrates and fish, in conjunction with influences of temperature, pH-values, Eh-values, water content, organic matter and elemental sediment composition, lead to the extremely complex nature of nutrient cycling. Three essential components of aquatic ecosystems are discussed, namely carbon, nitrogen and phosphorus.

The objective of this paper is to illustrate in condensed form the heterogeneous nature of nutrient cycling processes. In addition, the importance of sediments in understanding nutrient cycling is discussed from a water management perspective.

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© 1989 Kluwer Academic Publishers

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Forsberg, C. (1989). Importance of sediments in understanding nutrient cyclings in lakes. 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_24

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  • DOI: https://doi.org/10.1007/978-94-009-2376-8_24

  • Publisher Name: Springer, Dordrecht

  • Print ISBN: 978-94-010-9007-0

  • Online ISBN: 978-94-009-2376-8

  • eBook Packages: Springer Book Archive

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