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Studies on the sorption of iron group elements from sea water by the radiotracer method

  • Trace Radiochemistry
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Abstract

The methods of radioactive labelling the sea water and the conditions for reaching the equivalence of physico-chemical states of radiotracers and corresponding stable nuclides in sea water are analyzed. The process of bioassimilation, the uptake and release of radionuclides by plankton organisms, is considered as the way of fast stabilization of physicochemical forms of radiotracers in sea water. The data are presented on the sorption of iron, cobalt, nickel and manganese by typical ocean bottom sediments (deep-water red clay, diatomic coze, carbonate deposit).

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Authors and Affiliations

  1. Institute of Physical Chemistry, USSR Academy of Sciences, Moscow, (USSR)

    V. V. Gromov

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  1. V. V. Gromov
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Gromov, V.V. Studies on the sorption of iron group elements from sea water by the radiotracer method. J. Radioanal. Chem. 30, 181–195 (1976). https://doi.org/10.1007/BF02516629

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  • DOI: https://doi.org/10.1007/BF02516629

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