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2013 | z. 135 | 73--86
Tytuł artykułu

Some Characteristics of Forest-Tundra (West Siberia) Soil Groups Distinguished on The Basis of Thermal Properties

Treść / Zawartość
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
This paper contains the results of the forest-tundra soils studying. The key sites were situated on the permafrost territory, which is under scrutiny in connection with the global climate changes. The soil position in landscape, parent rock texture, vegetation conditions and thickness of organic horizons were taken into account. On the base of seasonal thawing or active layer depth measurements and soil temperature vertical gradients calculating, four main soil groups which are different in their thermal properties were identified. The physical-chemistry properties are rather close in various soil types. Similarities in the profile distribution of humus fractions are also revealed in the soil humus formed under different conditions. Despite of estimated relatively low level of carbon stocks in forest-tundra soils, half of them exist in mobile humus forms, which are less stable. Data on the soil thermal regime types and stocks of different humus forms in soils of various conditions are useful for long-term forecasting of soil status. (original abstract)
Słowa kluczowe
Twórcy
  • Ural Federal University
  • Ural Federal University
autor
  • Ural Federal University
  • Ural Federal University
autor
  • Institut Pierre Simon Laplace, Saclay, CEA-CNRS-UVSQ
Bibliografia
  • Archegova I., 2007, Thermal regime of tundra soils in the restoration conditions of natural vegetation, Soil Science 8, 954-960.
  • Dedkov V., 1995, Soils, Yamal Nature, Science, Ekaterinburg.
  • Dergacheva M., 1984, Soil organic matter: statics and dynamics (on example of Western Siberia), Nauka, Novosibirsk.
  • Epstein H., Raynolds M., Walker D., Bhatt U., Tucker C., Pinzon J., 2012, Dynamics of aboveground phytomass of the circumpolar Arctic tundra during the past three decades, Environmental Research Letters 7, 1-13.
  • Firsova V., Dedkov V., 1983, High latitude Ural mountain soils, USSR Academy of Sciences, Sverdlovsk.
  • Hopmans J., Zimunek J., Bristow K., 2002, Indirect estimation of soil thermal properties and water flux using heat pulse probe measurements: Geometry and dispersion effects, Water Resources Research 1, 1-14.
  • Karelin D., Zamolodchikov D., 2008, Carbon exchange in cryogenic ecosystems, Nauka, Moscow.
  • Mandarov A., Skriabin P., 1979, Thermal conductivity of natural and disturbed soils in the north of Western Siberia, Man-made landscapes of the North and their reclamation, Nauka, Novosibirsk.
  • Mazhitova G., 2008, Soil temperature regimes in the area of not continuous permafrost of the European North-East Russia, Soil Science 1, 54-67.
  • National atlas of Russia. Nature and ecology, 2008, Astrel, Roskartografia, Moskow.
  • Orlov D., 1990, Soil humus acids and general theory of humification, Moscow State University Press, Moscow.
  • Orlov D., Biryukova O., 1998, The soil organic compounds stability and greenhouse gases emission into the atmosphere, Soil Science 7, 783-793.
  • Ponomariova V., Plotnikova T., 1975, Method of determination soil humus content and composition, Leningrad.
  • Rozanov B., 2004, Soil morphology, Academic Project, Moscow.
  • Vasilevskaya V., Ivanov V., Bogatirev A., 1986, The North soils of the Western Siberia, Moscow State University, Moscow.
  • World Reference Base for Soil Resources, 2006, Food and agriculture organization of the United Nations, Rome.
  • Zhuang Q., McGuire A., Clein J., Dargaville R., Kicklighter D., Myneny R., Dong J., Romanovsky V., Harden J., Hobbie J., 2003, Carbon cycling in extratropical terrestrial ecosystems of the Northern Hemisphere during the 20th century: a modeling analysis of the influences of soil thermal dynamics, Tellus, 55B (3), 751-776.
Typ dokumentu
Bibliografia
Identyfikatory
Identyfikator YADDA
bwmeta1.element.ekon-element-000171351363

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