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Long-term changes in soil composition in unmanaged central European mountain spruce forests after decreased acidic deposition and a bark beetle outbreak

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    SYSNO ASEP0583662
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleLong-term changes in soil composition in unmanaged central European mountain spruce forests after decreased acidic deposition and a bark beetle outbreak
    Author(s) Kopáček, Jiří (BC-A) RID, ORCID
    Čapek, P. (CZ)
    Choma, M. (CZ)
    Cudlín, Pavel (UEK-B) RID, SAI, ORCID
    Kaňa, Jiří (BC-A) RID, ORCID
    Kopáček, Marek (BC-A) RID, ORCID
    Porcal, Petr (BC-A) RID, ORCID
    Šantrůčková, H. (CZ)
    Tahovská, K. (CZ)
    Turek, Jan (BC-A)
    Number of authors10
    Article number106839
    Source TitleCatena. - : Elsevier - ISSN 0341-8162
    Roč. 222, Dec (2023)
    Number of pages13 s.
    Languageeng - English
    CountryNL - Netherlands
    Keywordsphosphate sorption ; nitrogen dynamics ; tatra mountains ; plesne lakes ; Exchangeable cations ; Metal oxyhydroxides
    Subject RIVDF - Soil Science
    OECD categorySoil science
    Subject RIV - cooperationGlobal Change Research Institute - Ecology, Behaviour
    R&D ProjectsTO01000220 GA TA ČR - Technology Agency of the Czech Republic (TA ČR)
    GA22-05421S GA ČR - Czech Science Foundation (CSF)
    Method of publishingOpen access
    Institutional supportBC-A - RVO:60077344 ; UEK-B - RVO:86652079
    UT WOS000992648200001
    EID SCOPUS85143488042
    DOI10.1016/j.catena.2022.106839
    AnnotationWe studied the effect of tree mortality on nutrient concentrations and pools in soils of two unmanaged mountain forest catchments (Plesne, PL., and Certovo, CT., Czech Republic) recovering from acidification due to decreasing acidic atmospheric deposition since the late 1980s. Both catchments were situated at similar elevation, and before a bark beetle outbreak were covered by healthy mature Norway spruce (Picea abies) forests. However, differing bedrock [granite (PL) vs mica-schist and quartzite (CT)] resulted in lower concentrations of base cations (except for magnesium), but higher concentrations of aluminium and iron oxyhydroxides in the CT soils, enabling higher phosphorus (P) accumulation. Despite these differences, soils were similarly acidic, with pH(H2O) from 3.5 to 4.3 and cation exchange capacity (CEC) dominated by exchangeable protons (H-ex(+)) and aluminium in both catchments in 2000. In the PL catchment, >75 % of mature spruce trees died after a bark beetle infestation between 2004 and 2008, and all dead biomass was left on site. Forest damage in the CT catchment was minor. Soil concentrations and pools of exchangeable calcium (Ca-ex(2+)), magnesium (Mg-ex(2+)), potassium (K-ex(+)), and H-ex(+) were tightly related to concentrations of organic carbon (C). Following the tree dieback in the PL catchment, we observed significant (p < 0.05) increases in (1) concentrations and pools of Ca-ex(2+), Mg-ex(2+) , and K-ex(+), (2) base saturation (from 30 to similar to 40 %), (3) CEC:C ratios (i.e., CEC of soil organic carbon), (4) pH(H2O), (5) mineral P forms, and (6) total nitrogen (N) in the upper (O and A) soil horizons. Similar changes were less pronounced or negligible in the less impacted CT soils. The elevated litterfall after tree dieback, resulting in the increased input of base cations to forest floor and increased CEC of soil organic C, played a more important role in the decreasing acidity of the PL soils than the continuing decrease in acidic deposition.
    WorkplaceBiology Centre (since 2006)
    ContactDana Hypšová, eje@eje.cz, Tel.: 387 775 214
    Year of Publishing2024
    Electronic addresshttps://doi.org/10.1016/j.catena.2022.106839
Number of the records: 1  

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