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Time variations of the concentration of mobile forms of Fe, Mn, and P in silts of the Mozhaisk Reservoir

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Abstract

Layer-by-layer concentrations of Fe, Mn, and P compounds in the channel silts of the Krasnovidovo Pool, the Mozhaisk Reservoir, was studied in 1970–1971 and 1974–1975. The mean annual concentration of those elements in a sediment column was found to increase by factors of 1.1, 2, and 1.4 for Fe, Mn, and P, respectively. The factors that caused such changes are discussed.

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Authors and Affiliations

  1. Water Problems Institute, Russian Academy of Sciences, ul. Gubkina 3, Moscow, 119333, Russia

    M. V. Martynova

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  1. M. V. Martynova
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Correspondence to M. V. Martynova.

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Original Russian Text © M.V. Martynova, 2015, published in Vodnye Resursy, 2015, Vol. 42, No. 5, pp. 504–509.

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Martynova, M.V. Time variations of the concentration of mobile forms of Fe, Mn, and P in silts of the Mozhaisk Reservoir. Water Resour 42, 652–657 (2015). https://doi.org/10.1134/S0097807815050103

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  • DOI: https://doi.org/10.1134/S0097807815050103

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