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Tree water uptake enhances nitrogen acquisition in a fertilized boreal forest but not under nitrogen-poor conditions

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    SYSNO ASEP0559316
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleTree water uptake enhances nitrogen acquisition in a fertilized boreal forest but not under nitrogen-poor conditions
    Author(s) Henriksson, N. (SE)
    Lim, H. (SE)
    Marshall, John David (UEK-B) RID, SAI
    Franklin, O. (SE)
    McMurtrie, R. E. (AU)
    Lutter, R. (EE)
    Magh, R. (SE)
    Lundmark, T. (SE)
    Nasholm, T. (SE)
    Number of authors9
    Source TitleNew Phytologist - ISSN 0028-646X
    Roč. 232, č. 1 (2021), s. 113-122
    Number of pages10 s.
    Languageeng - English
    CountryGB - United Kingdom
    Keywordsn-15 ; deuterium ; diffusion ; isotope ; mass flow ; nitrogen uptake ; Pinus sylvestris (Scots pine) ; water uptake
    Subject RIVEF - Botanics
    OECD categoryPlant sciences, botany
    Method of publishingOpen access
    Institutional supportUEK-B - RVO:86652079
    UT WOS000675530300001
    EID SCOPUS85110986635
    DOI10.1111/nph.17578
    AnnotationUnderstanding how plant water uptake interacts with acquisition of soil nitrogen (N) and other nutrients is fundamental for predicting plant responses to a changing environment, but it is an area where models disagree. We present a novel isotopic labelling approach which reveals spatial patterns of water and N uptake, and their interaction, by trees. The stable isotopes N-15 and H-2 were applied to a small area of the forest floor in stands with high and low soil N availability. Uptake by surrounding trees was measured. The sensitivity of N acquisition to water uptake was quantified by statistical modelling. Trees in the high-N stand acquired twice as much N-15 as in the low-N stand and around half of their N uptake was dependent on water uptake (H-2 enrichment). By contrast, in the low-N stand there was no positive effect of water uptake on N uptake. We conclude that tree N acquisition was only marginally dependent on water flux toward the root surface under low-N conditions whereas under high-N conditions, the water-associated N uptake was substantial. The results suggest a fundamental shift in N acquisition strategy under high-N conditions.
    WorkplaceGlobal Change Research Institute
    ContactNikola Šviková, svikova.n@czechglobe.cz, Tel.: 511 192 268
    Year of Publishing2023
    Electronic addresshttps://nph.onlinelibrary.wiley.com/doi/10.1111/nph.17578
Number of the records: 1  

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