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Aox-Levels in The River Rhine: 50 Percent of Natural Origin!

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Integrated Soil and Sediment Research: A Basis for Proper Protection

Part of the book series: Soil & Environment ((SOEN,volume 1))

Abstract

AOX (adsorbable organohalogens) levels are routinely measured in the river Rhine for testing water quality. The total AOX load of the river Rhine can be explained only partly by point sources from (industrial) discharges, but the origin of diffusive sources still remain unclear. Calculations show that atmospheric deposition of anthropogenic low-molecular-weight organohalogens cannot be responsible for the rest of the AOX.

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References

  • Asplund, G., Grimvall, A. (1991). Organohalogens in Nature, Environ. Sci. Technol. 25(1991) 8, 1346–1350.

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  • Bericht der Arbeitsgemeinschaft Rhein-Wasserwerke E.V., 44(1987).

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© 1993 Springer Science+Business Media Dordrecht

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Hoekstra, E.J., de Leer, E.W.B. (1993). Aox-Levels in The River Rhine: 50 Percent of Natural Origin!. In: Eijsackers, H.J.P., Hamers, T. (eds) Integrated Soil and Sediment Research: A Basis for Proper Protection. Soil & Environment, vol 1. Springer, Dordrecht. https://doi.org/10.1007/978-94-011-2008-1_19

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  • DOI: https://doi.org/10.1007/978-94-011-2008-1_19

  • Publisher Name: Springer, Dordrecht

  • Print ISBN: 978-94-010-4887-3

  • Online ISBN: 978-94-011-2008-1

  • eBook Packages: Springer Book Archive

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