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Carbon storage in post-mining forest soil, the role of tree biomass and soil bioturbation

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    SYSNO ASEP0328550
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleCarbon storage in post-mining forest soil, the role of tree biomass and soil bioturbation
    Author(s) Frouz, Jan (BC-A) RID, ORCID
    Pižl, Václav (BC-A) RID
    Cienciala, E. (CZ)
    Kalčík, Jiří (BC-A)
    Source TitleBiogeochemistry. - : Springer - ISSN 0168-2563
    Roč. 94, č. 2 (2009), s. 111-121
    Number of pages11 s.
    Languageeng - English
    CountryNL - Netherlands
    Keywordssoil formation ; bioturbation ; carbon cycling
    Subject RIVEH - Ecology, Behaviour
    R&D Projects2B08023 GA MŠMT - Ministry of Education, Youth and Sports (MEYS)
    1QS600660505 GA AV ČR - Academy of Sciences of the Czech Republic (AV ČR)
    CEZAV0Z60660521 - UPB-H, BC-A (2005-2011)
    UT WOS000266644300002
    DOI10.1007/s10533-009-9313-0
    AnnotationCarbon storage in aboveground tree biomass and soil organic matter (in depth of A layer development i.e., up to 20 cm) was studied in 22-32 year-old post-mining sites in the northwest of the Czech Republic. Four replicated sites afforested with different tree species (spruce, pine, larch, oak, lime or alder) were compared with sites left to natural regeneration which were dominated by aspen, birch and willow. No topsoil was applied at the sites; hence carbon accumulation resulted from in situ soil development on alkaline tertiary clays that were dumped on the heaps. Carbon storage in the soil was positively correlated with aboveground tree biomass. Soil carbon was equivalent to 98.1% of the carbon found in aboveground tree biomass at lime dominated sites, but only 21.8% at sites with natural regeneration. No significant correlation was found between C storage in soil and aboveground litter input.
    WorkplaceBiology Centre (since 2006)
    ContactDana Hypšová, eje@eje.cz, Tel.: 387 775 214
    Year of Publishing2010
Number of the records: 1  

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