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Dissolved and gaseous nitrogen losses in forests controlled by soil nutrient stoichiometry

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985831%3A_____%2F21%3A00543408" target="_blank" >RIV/67985831:_____/21:00543408 - isvavai.cz</a>

  • Alternative codes found

    RIV/60076658:12310/21:43903368 RIV/86652079:_____/21:00543408 RIV/00025798:_____/21:00000115 RIV/67985874:_____/21:00543408

  • Result on the web

    <a href="https://iopscience.iop.org/article/10.1088/1748-9326/ac007b" target="_blank" >https://iopscience.iop.org/article/10.1088/1748-9326/ac007b</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1088/1748-9326/ac007b" target="_blank" >10.1088/1748-9326/ac007b</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Dissolved and gaseous nitrogen losses in forests controlled by soil nutrient stoichiometry

  • Original language description

    Global chronic nitrogen (N) deposition to forests can alleviate ecosystem N limitation, with potentially wide ranging consequences for biodiversity, carbon sequestration, soil and surface water quality, and greenhouse gas emissions. However, the ability to predict these consequences requires improved quantification of hard-to-measure N fluxes, particularly N gas loss and soil N retention. Here we combine a unique set of long-term catchment N budgets in the central Europe with ecosystem N-15 data to reveal fundamental controls over dissolved and gaseous N fluxes in temperate forests. Stream leaching losses of dissolved N corresponded with nutrient stoichiometry of the forest floor, with stream N losses increasing as ecosystems progress towards phosphorus limitation, while soil N storage increased with oxalate extractable iron and aluminium content. Our estimates of soil gaseous losses based on N-15 stocks averaged 2.5 +/- 2.2 kg N ha(-1) yr(-1) and comprised 20% +/- 14% of total N deposition. Gaseous N losses increased with forest floor N:P ratio and with dissolved N losses. Our relationship between gaseous and dissolved N losses was also able to explain previous N-15-based N loss rates measured in tropical and subtropical catchments, suggesting a generalisable response driven by nitrate (NO3 (-)) abundance and in which the relative importance of dissolved N over gaseous N losses tended to increase with increasing NO3 (-) export. Applying this relationship globally, we extrapolated current gaseous N loss flux from forests to be 8.9 Tg N yr(-1), which represent 39% of current N deposition to forests worldwide.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    10501 - Hydrology

Result continuities

  • Project

    Result was created during the realization of more than one project. More information in the Projects tab.

  • Continuities

Others

  • Publication year

    2021

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Environmental Research Letters

  • ISSN

    1748-9326

  • e-ISSN

    1748-9326

  • Volume of the periodical

    16

  • Issue of the periodical within the volume

    6

  • Country of publishing house

    GB - UNITED KINGDOM

  • Number of pages

    11

  • Pages from-to

    064025

  • UT code for WoS article

    000655341900001

  • EID of the result in the Scopus database

    2-s2.0-85107763814