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Recovery from acidification alters concentrations and fluxes of solutes from Czech catchments

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F86652079%3A_____%2F17%3A00476536" target="_blank" >RIV/86652079:_____/17:00476536 - isvavai.cz</a>

  • Alternative codes found

    RIV/67985831:_____/17:00476536 RIV/67985874:_____/17:00476536 RIV/00025798:_____/17:00000040

  • Result on the web

    <a href="http://dx.doi.org/10.1007/s10533-017-0298-9" target="_blank" >http://dx.doi.org/10.1007/s10533-017-0298-9</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1007/s10533-017-0298-9" target="_blank" >10.1007/s10533-017-0298-9</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Recovery from acidification alters concentrations and fluxes of solutes from Czech catchments

  • Original language description

    Changes in atmospheric deposition, stream water chemistry, and solute fluxes were assessed across 15 small forested catchments. Dramatic changes in atmospheric deposition have occurred over the last three decades, including a 70% reduction in sulphur (S) deposition. These changes in atmospheric inputs have been associated with expected changes in levels of acidity, sulphate and base cations in streams. Soil retention of S appeared to partially explain rates of chemical recovery. In addition to these changes in acid–base chemistry we also observed unexpected changes in nitrogen (N) biogeochemistry and nutrient stoichiometry of stream water, including decreased stream N concentrations. Among all catchments the average flux of dissolved inorganic nitrogen (DIN) was best predicted by average runoff, soil chemistry (forest floor C/N) and levels of acid deposition (both S and N). The rate of change in stream DIN flux, however, was much more closely correlated with reductions in rates of S deposition rather than those of DIN. Unlike DIN fluxes, the average concentrations as well as the rates of decline in streamwater nitrate (NO3) concentration over time were tightly linked to stream dissolved organic carbon/dissolved organic nitrogen ratios DOC/DON and DON/TP rather than catchment characteristics. Declines in phosphorus adsorption with increasing soil pH appear to contribute to the relationship between C, N, and P in our study catchments. Our observations suggest that catchment P availability and its alteration due to environmental changes (e.g. acidification) might have profound effects on N cycling and catchment N retention that have been largely unrecognized.

  • 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

    10511 - Environmental sciences (social aspects to be 5.7)

Result continuities

  • Project

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

  • Continuities

    P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Others

  • Publication year

    2017

  • Confidentiality

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

Data specific for result type

  • Name of the periodical

    Biogeochemistry

  • ISSN

    0168-2563

  • e-ISSN

  • Volume of the periodical

    132

  • Issue of the periodical within the volume

    3

  • Country of publishing house

    NL - THE KINGDOM OF THE NETHERLANDS

  • Number of pages

    22

  • Pages from-to

    215-272

  • UT code for WoS article

    000396123500002

  • EID of the result in the Scopus database

    2-s2.0-85012864680