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Forest growth responds more to air pollution than soil acidification

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    SYSNO ASEP0571049
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleForest growth responds more to air pollution than soil acidification
    Author(s) Hruška, Jakub (UEK-B) RID, SAI, ORCID
    Oulehle, Filip (UEK-B) RID, ORCID, SAI
    Chuman, Tomáš (UEK-B) RID, SAI, ORCID
    Kolář, T. (CZ)
    Rybníček, M. (CZ)
    Trnka, Miroslav (UEK-B) RID, ORCID, SAI
    McDowell, W. H. (US)
    Number of authors7
    Article numbere0256976
    Source TitlePLoS ONE. - : Public Library of Science - ISSN 1932-6203
    Roč. 18, č. 3 (2023)
    Number of pages21 s.
    Languageeng - English
    CountryUS - United States
    Keywordsspruce picea -abies ; norway spruce ; magic model ; nitrogen ; deposition ; carbon ; chemistry ; turnover ; decline ; sulfur
    Subject RIVGK - Forestry
    OECD categoryForestry
    R&D ProjectsEF16_019/0000797 GA MŠMT - Ministry of Education, Youth and Sports (MEYS)
    GC21-22810J GA ČR - Czech Science Foundation (CSF)
    Research InfrastructureCzeCOS IV - 90248 - Ústav výzkumu globální změny AV ČR, v. v. i.
    Method of publishingOpen access
    Institutional supportUEK-B - RVO:86652079
    UT WOS000948775000035
    EID SCOPUS85149806100
    DOI10.1371/journal.pone.0256976
    AnnotationThe forests of central Europe have undergone remarkable transitions in the past 40 years as air quality has improved dramatically. Retrospective analysis of Norway spruce (Picea abies) tree rings in the Czech Republic shows that air pollution (e.g. SO2 concentrations, high acidic deposition to the forest canopy) plays a dominant role in driving forest health. Extensive soil acidification occurred in the highly polluted ,,Black Triangle,, in Central Europe, and upper mineral soils are still acidified. In contrast, acidic atmospheric deposition declined by 80% and atmospheric SO2 concentration by 90% between the late 1980s and 2010s. In this study we oserved that annual tree ring width (TRW) declined in the 1970s and subsequently recovered in the 1990s, tracking SO2 concentrations closely. Furthermore, recovery of TRW was similar in unlimed and limed stands. Despite large increases in soil base saturation, as well as soil pH, as a result of repeated liming starting in 1981, TRW growth was similar in limed and unlimed plots. TRW recovery was interrupted in 1996 when highly acidic rime (originating from more pronounced decline of alkaline dust than SO2 from local power plants) injured the spruce canopy, but recovered soon to the pre-episode growth. Across the long-term site history, changes in soil chemistry (pH, base saturation, Bc/Al soil solution ratio) cannot explain observed changes in TRW at the two study sites where we tracked soil chemistry. Instead, statistically significant recovery in TRW is linked to the trajectory of annual SO2 concentrations or sulfur deposition at all three stands.
    WorkplaceGlobal Change Research Institute
    ContactNikola Šviková, svikova.n@czechglobe.cz, Tel.: 511 192 268
    Year of Publishing2024
    Electronic addresshttps://journals.plos.org/plosone/article?id=10.1371/journal.pone.0256976
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