Biogeochemical migration of Al, Hf, Sc, Th and rare-earth metals in the profile of the deep-seated eutrophic marsh in the interfluve of the Ob and Tom rivers

  • T. T. Efremova
  • S. P. Efremov
  • K. P. Koutzenogii
  • A. I. Smirnova
  • V. F. Peresedov
  • T. M. Ostrovnaya
  • V. P. Chinaeva
Letter to the Editor


Aluminum, Sc, Th, Hf, and lanthanoids belong to groups of elements that are, slightly, very slightly, and moderately captured in marsh ecosystems. In the genesis of the peatbog the biogeochemical migration of elements is mainly determined by the quality of the humus barriers as well as by the capability to form intermetallic compounds of widely varying compositions. In the surface layer (10 cm) of the peatbog the highest content of Al, Hf, Ce, and Sm over the entire history of marsh development was observed. This fact reflects the modern tendency to forming technogenic streams of the above content.


Aluminum Physical Chemistry Migration Inorganic Chemistry Surface Layer 
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  1. 1.
    V. I. Vernadsky, Selected Works, Vol. 5, AS USSR, Moscow, 1960.Google Scholar
  2. 2.
    A. I. Perelman, Geochemistry, Moscow, Higher School, 1989.Google Scholar
  3. 3.
    B. B. Polynov, Doctrine about Landscapes, Selected Works, AS USSR, Moscow, 1956.Google Scholar
  4. 4.
    S. P. Efremov, T. T. Efemova, N. V. Mlentyeva, Carbon in the Ecosystems of Forests and Marshes of Russia, Krasnoyarsk, 1994.Google Scholar
  5. 5.
    N. A. Karavaeva, Swamping and Evolution of Soils, Science, Moscow, 1982.Google Scholar
  6. 6.
    N. I. Pyavchenko, Peatbogs and their Natural and Economic Significance, Science, Moscow, 1985.Google Scholar
  7. 7.
    T. M. Ostrovnaya, L. S. Nefedyeva, V. M. Nazarov et al, in: Acitvation Analysis in Environment Protection, D14-93-325, Dubna, 1993.Google Scholar
  8. 8.
    V. M. Nazarov, V. F. Peresedov, J. Radioanal. Nucl. Chem., 192 (1995) 17.Google Scholar
  9. 9.
    V. M. Nazarov, M. V. Frontasyeva, V. F. Peresedov, V. P. Chinaeva, T. M. Ostronayva, S. F. Gundorina, V. V. Nikonov, J. Radioanal. Nucl. Chem., 192 (1995) 229.Google Scholar
  10. 10.
    V. F. Peresedov, V. P. Chinaeva, S. F. Gundorina, T. M. Ostrovnaya, J. Radioanal. Nucl. Chem., 207 (1996) 295.Google Scholar
  11. 11.
    V. F. Peresedov, S. F. Gundorina, T. M. Ostrovnaya, J. Radioanal. Nucl. Chem., 219 (1997) 105.CrossRefGoogle Scholar
  12. 12.
    V. F. Peresedov, A. D. Rogov, J. Radioanal. Nucl. Chem., 214 (1996) 277; 219 (1997) 105.Google Scholar
  13. 13.
    M. F. Frontasyeva, F. Grass, V. M. Nazarov, E. Steinnes, J. Radional. Nucl. Chem., 192 (1995) 371.Google Scholar
  14. 14.
    T. T. Efremova, News of SB AS USSR (Biological Sciences), Vol. 3, 1983, p. 24.Google Scholar
  15. 15.
    T. T. Efremova, Soil Sci., 12 (1992) 25.Google Scholar
  16. 16.
    T. T. Efremova, Intern. Symp. on Organic Substance of Peat, Minsk, 1995.Google Scholar
  17. 17.
    T. T. Efremova, in: Generation of Structure in Peat Soils, Science, Novosibirsk, 1992, p. 1.Google Scholar
  18. 18.
    Short Chemical Encyclopaedia, Vol. 5, Soviet Encyclopaedia, Moscow, 1967.Google Scholar
  19. 19.
    Short Chemical Encyclopaedia, Vol. 2, Soviet Encyclopaedia, Moscow, 1963.Google Scholar

Copyright information

© Akadémiai Kiadó 1999

Authors and Affiliations

  • T. T. Efremova
    • 1
  • S. P. Efremov
    • 1
  • K. P. Koutzenogii
    • 2
  • A. I. Smirnova
    • 2
  • V. F. Peresedov
    • 3
  • T. M. Ostrovnaya
    • 3
  • V. P. Chinaeva
    • 3
  1. 1.Institute of ForestSiberian Branch RASKrasnoyarskRussia
  2. 2.Institute of Chemical Kinetics and CombustionSB RASNovosibirskRussia
  3. 3.Frank Laboratory of Neutron PhysicsJoint Institute for Nuclear ResearchDubna, Moscow RegionRussia

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