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Denitrification at two nitrogen-polluted, ombrotrophic Sphagnum bogs in Central Europe: Insights from porewater N2O-isotope profiles

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60076658%3A12310%2F15%3A43888738" target="_blank" >RIV/60076658:12310/15:43888738 - isvavai.cz</a>

  • Alternative codes found

    RIV/67985556:_____/15:00439538 RIV/00025798:_____/15:00000020

  • Result on the web

    <a href="http://www.sciencedirect.com/science/article/pii/S003807171400368X" target="_blank" >http://www.sciencedirect.com/science/article/pii/S003807171400368X</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1016/j.soilbio.2014.10.021" target="_blank" >10.1016/j.soilbio.2014.10.021</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Denitrification at two nitrogen-polluted, ombrotrophic Sphagnum bogs in Central Europe: Insights from porewater N2O-isotope profiles

  • Original language description

    Measurements of nitrogen isotope ratios (delta N-15) along vertical porewater profiles are instrumental in localizing sources and sinks of nitrous oxide (N2O) in wetland ecosystems. We present the first N2O concentration and isotope data for porewaters of ombrotrophic, mountain-top bogs. Our two study sites, situated in the Czech Republic at elevations higher than 1000 m, have been affected by atmospheric N pollution for more than 100 years. In recent decades, the northeastern site KB received over 30 kg N ha(-1) yr(-1) via atmospheric deposition, the southwestern site BS was 3 times less polluted. Both peat bogs were surrounded by defoliated, dead spruce stands. We hypothesized that elevated nitrate (NO3-) inputs in rain-fed bogs may cause sizeable N2O emissions. Porewater N2O concentrations in the studied ombrotrophic bogs were 400-800 times higher, compared to fens in nearby Bavaria (Germany). The highest N2O concentrations and the lowest delta N-15-N2O values were found at the bottom of the sampled porewater profiles, 40-60 cm below surface. Low delta N-15-N2O values resulted from a N isotope fractionation associated with denitrification. The site with the lower historical N pollution, BS, exhibited up to 7 times higher porewater N2O concentrations than KB, possibly due to a higher denitrification potential determined as abundance of nirK and nirS genes. Upcore, N2O abundance decreased and delta N-15 -N2O increased, indicating N2O reduction. Processes of N2O formation and consumption at different depths were integrated by measuring N2O fluxes across the peat - atmosphere interface. These fluxes were minute (<0.02 mu mol N2O m(-2) h(-1)). We even observed scavenging of air-borne N2O by the bog substrate. Nitrogen pollution of ombrotrophic bogs led to vigorous N cycling, manifested by extremely high peat porewater N2O concentrations. However, effective in-situ consumption of the produced N2O greatly reduced its warming potential.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)

  • CEP classification

    DD - Geochemistry

  • OECD FORD branch

Result continuities

  • Project

    <a href="/en/project/GAP504%2F12%2F1782" target="_blank" >GAP504/12/1782: Relationship between atmospheric N deposition and N accumulation in rain-fed peat bogs: Insights from a 210Pb-15N isotope study</a><br>

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2015

  • Confidentiality

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

Data specific for result type

  • Name of the periodical

    Soil Biology &amp; Biochemistry

  • ISSN

    0038-0717

  • e-ISSN

  • Volume of the periodical

    81

  • Issue of the periodical within the volume

    FEB 2015

  • Country of publishing house

    GB - UNITED KINGDOM

  • Number of pages

    10

  • Pages from-to

    48-57

  • UT code for WoS article

    000350524700006

  • EID of the result in the Scopus database