Skip to main content

Advertisement

Log in

Transformation of Organic Matter of the Larch Forest Soils in the Northern Taiga of Nizhne-Tungusskoe Plateau, Central Siberia

  • Published:
Mitigation and Adaptation Strategies for Global Change Aims and scope Submit manuscript

Abstract

The evaluation of biospheric role of the boreal forests in the accumulation of carbon is connected with the evaluation of organic matter (OM) pool in soils. The research sites were larch forests, they are situated on Nizhne-Tungusskoe Plateau. Larch forests of feather-moss and lichen types (110 and 380 years old) were formed on 'ochric podbur' soils. Litter stocks are 3.5–4.5 kg m− 2 with thickness 10–25 cm. Cryomezomorphic northern taiga soils contains 38–73 t (carbon) ha− 1. Pool of fast mineralized OM has average value 38.1 t (carbon) ha− 1, including 20.5 and 6.4 t (Carbon) ha− 1 of labile compounds on surface and in the soil, and 11.2 t (carbon) ha− 1 of mobile OM. Microbial mass reaches 1.78–3.47 t (carbon) ha− 1, its proportion is 3.6–4.9% of the total OM carbon. Zoomass of feather-moss larch forest is 0.20–0.61 * 10− 2, in lichen larch forest −0.01–0.07 * 10− 2 t (carbon) ha− 1. A pool of resistant to biological decomposition and bonded to mineral soil matrix OM is 17.7 t (carbon) ha− 1 and it varies from 18.6 to 29.0 in feather-moss larch forest, and from 6.4 to 17.0 t (carbon) ha− 1 in lichen larch forest. Two-years field experiment has been performed to determine transformation rates of various plant litter fractions and to clarify the role of soil biota in these processes. The results showed participation of all biota groups in the decomposition of plant residues caused weight loss of larch-needles and root mortmass. Isolation of organic matter from all-size invertebrate groups leads to some decrease of decomposition activity.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Institutional subscriptions

Similar content being viewed by others

References

  • Arinushkina, E.V.: 1970, Guidebook of the Soil Chemical Analyses, Moscow, Moscow State University, pp. 136–141 (in Russian).

  • Burikin, A.M. and Zasorina, E.V.: 1989, ‘The processes of mineralization and humifikationof plant residues in the young soils of tecnogenic ecosystems’, Pochvovedenie N2, 61–69 (in Russian and English).

  • Dylis, N.V., Nosova, L.M. and Speranskaya, E.S.: 1975, ‘Peculiarity of accumulation and decomposition of litterfall in the conifer forests in Podmoskov'e’, Lesovedenie N6, 10–17 (in Russian with English summary).

  • Giliarov, M.S. and Striganova, B.R. (ed.): 1987, Quantitative Methods in Soil Zoology, Moscow, Nauka (in Russian).

  • Grishkan, I.B.: 1995, ‘Decomposition of litterfall in the basic ecosystems of the basin Kolima’, Russian Journal of Ecology N1, 9–12. (in Russian and English).

  • Johansson, M.-B.: 1994, ‘Decomposition rates of Scot pine needle litter related to site properties, litter quality, and climate’, Canadian Journal of Forest Research 24(9), 1771–1781.

    Article  Google Scholar 

  • Karpachevskiy, L.O., Borovinskaya, L.B. and Haydapova, D.D.: 1994, ‘The role of root systems in the soilforming in dry steppe’, Pochvovedenie N11, 77–84 (in Russian and English).

  • Karpachevskiy, L.O., Voronin, A.D. and Dmitriev, E.A.: 1980, Soil-Biogicenotic Researches in Forest Biogeocenouses, Moscow, MSU, 160 pp., (in Russian).

  • Klimchenko, A.V. and Fedorov, E.N.: 2000, Accumulation of organic matter in the died plant material in Northern taiga larch forests. Proceedings of the International Conference, “Modern Problems of Soil Science in Siberia,” Tomsk, Tomsk State University, pp. 353–356 (in Russian).

  • Kogut, B.M., D'yakonova, K.V. and Travnikova, L.S.: 1987, ‘The composition and properties of humic acids from different extracts and fractions of typical chernozem’, Pochvovedenie N7, 38–46 (in Russian and English).

  • Kogut, B.M. and Masiutenko, N.P.: 1992, ‘Elementary composition of labile humic acids of chernozems’, Pochvovedenie N1, 91–94 (in Russian and English).

  • Orlov, A.Ya.: 1967, ‘Determination of trees root mass in forest and registration possibility of the annual organic matter gross in the forest soil’, Lesovedenie N1, 64–70 (in Russian with English summary).

  • Ponomareva, V.V. and Plotnikova, T.A.: 1975, Methodic Instructions to Determine Quantity and Composition of Humus in Soils (Mineral and Peaty), Leningrad, Nauka, pp. 27–32 (in Russian).

  • Sharkov, I.N., Bukreeva, S.A. and Danilova, A.A.: 1994, ‘The role of light-mineralized organic matter in stabilization of carbon pools in tilled soils’, Siberian Ecological Journal N4, 363–368 (in Russian and English).

    Google Scholar 

  • Vedrova, E.F.: 1996, ‘The carbon balance in pine forests of Krasnoyarsk forest-steppe’, Lesovedenie N5, 51–59 (in Russian with English summary).

  • Vedrova, E.F.: 1998, ‘Carbon cycle in pine forests of taiga zone in the Krasnoyarskii Kray’, Lesovedenie N6, 3–10 (in Russian with English summary).

  • Zvyagintzev, D.G. (ed.): 1991, Methods of Soil Microbiology and Biochemistry, Moscow, MSU, (in Russian).

Download references

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to L. V. Mukhortova.

Rights and permissions

Reprints and permissions

About this article

Cite this article

Mukhortova, L.V., Bezkorovainaya, I.N. Transformation of Organic Matter of the Larch Forest Soils in the Northern Taiga of Nizhne-Tungusskoe Plateau, Central Siberia. Mitig Adapt Strat Glob Change 11, 191–202 (2006). https://doi.org/10.1007/s11027-006-1020-8

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s11027-006-1020-8

Keywords

Navigation