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Part of the book series: Monographiae Biologicae ((MOBI,volume 29))

Abstract

Two characteristics of water from the lower Nile long attracted attention-that it was of excellent quality for drinking and irrigation, and that it seasonally contained high concentrations of silt. The systematic, scientific exploration of the general subject developed but slowly over the last hundred years. An essential element in this was a direct parallel to geographical exploration, namely the tracing upstream of sources of the materials and properties observed below. Geography and geology dictate that a blending of very different types of water must occur in the headwaters and middle reaches, with contributions from dissimilar lakes and highland tributaries. These sources also have different seasonal flows, and so influence the seasonal composition of water downstream. Further seasonal influences include the annual impoundment of water by dams in the Sudan, and the chemical activities of plankton in the impounded water. Unlike many rivers, the Nile is little affected by pollution. However, the extensive Sudd swamps on the Upper White Nile can introduce deoxygenation and its chemical consequences.

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Julian Rzóska

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Talling, J.F. (1976). Water Characteristics. In: Rzóska, J. (eds) The Nile, Biology of an Ancient River. Monographiae Biologicae, vol 29. Springer, Dordrecht. https://doi.org/10.1007/978-94-010-1563-9_39

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  • DOI: https://doi.org/10.1007/978-94-010-1563-9_39

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