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Changes in surface water chemistry caused by natural forest dieback in an unmanaged mountain catchment

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60076658%3A12310%2F17%3A43895539" target="_blank" >RIV/60076658:12310/17:43895539 - isvavai.cz</a>

  • Alternative codes found

    RIV/60077344:_____/17:00479714

  • Result on the web

    <a href="https://ac.els-cdn.com/S0048969717301584/1-s2.0-S0048969717301584-main.pdf?_tid=2465af6c-eccf-11e7-a6fd-00000aab0f01&acdnat=1514576187_aae55bea0ba4f0ab14cfab80ac2ec2af" target="_blank" >https://ac.els-cdn.com/S0048969717301584/1-s2.0-S0048969717301584-main.pdf?_tid=2465af6c-eccf-11e7-a6fd-00000aab0f01&acdnat=1514576187_aae55bea0ba4f0ab14cfab80ac2ec2af</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1016/j.scitotenv.2017.01.148" target="_blank" >10.1016/j.scitotenv.2017.01.148</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Changes in surface water chemistry caused by natural forest dieback in an unmanaged mountain catchment

  • Original language description

    Ionic and nutrient compositions of throughfall, tributaries and lake outlet were analysed in the Plegne catchment lake system (an unmanaged mountain forest in Central Europe) from 1997 to 2016. The aim was to evaluate changes in surface water chemistry after natural forest dieback. In the 2004-2008, 93% of the Norway spruce trees were killed by bark beetle outbreak, and all dead biomass remained in the catchment. Forest dieback changed the chemistry of all water fluxes, and the magnitude, timing, and duration of these changes differed for individual water constituents. The most pronounced decreases in throughfall concentrations occurred for K+, dissolved organic carbon (DOC), Ca2+ and Mg2+, i.e. elements mostly originating from canopy leaching, while concentrations of NH4+ and soluble reactive phosphorus (SRP) remained almost unaffected. In tributaries, the most rapid changes were increases in NO3-, K+, H+ and ionic aluminium (Al-i) concentrations, while terrestrial export of DOC and P forms started more slowly. Immediately after the forest dieback, increase in NO-3 concentrations was delayed by elevated DOC availability in soils. NO3- became the dominant anion, with maximuni concentrations up to 346 mu eq L-1 within 5-7 years after the bark beetle outbreak, and then started to decrease. Terrestrial exports of All, K+, H+, me, and Ca2+ accompanied NO3- leaching, but their trends differed due to their different sources. Elevated losses of SRP, DOC, and dissolved organic nitrogen continued until the end of the study. In the lake, microbial processes significantly decreased concentrations of NO3-, organic add anions, H+ and Ali(,), and confounded the chemical trends observed in tributaries. Our results suggest that terrestrial losses of elements and the deterioration of waters after forest dieback are less pronounced in unmanaged than managed (clear-cut) catchments.

  • 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

    10619 - Biodiversity conservation

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

    Science of the Total Environment

  • ISSN

    0048-9697

  • e-ISSN

  • Volume of the periodical

    584

  • Issue of the periodical within the volume

    APR 15 2017

  • Country of publishing house

    NL - THE KINGDOM OF THE NETHERLANDS

  • Number of pages

    11

  • Pages from-to

    971-981

  • UT code for WoS article

    000399358500094

  • EID of the result in the Scopus database