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Soil mercury distribution in adjacent coniferous and deciduous stands highly impacted by acid rain in the Ore Mountains, Czech Republic

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F86652079%3A_____%2F16%3A00464595" target="_blank" >RIV/86652079:_____/16:00464595 - isvavai.cz</a>

  • Alternative codes found

    RIV/67985831:_____/16:00464595 RIV/60460709:41210/16:71273 RIV/00025798:_____/16:00000288

  • Result on the web

    <a href="http://dx.doi.org/10.1016/j.apgeochem.2016.10.005" target="_blank" >http://dx.doi.org/10.1016/j.apgeochem.2016.10.005</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1016/j.apgeochem.2016.10.005" target="_blank" >10.1016/j.apgeochem.2016.10.005</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Soil mercury distribution in adjacent coniferous and deciduous stands highly impacted by acid rain in the Ore Mountains, Czech Republic

  • Original language description

    Forests play a primary role in the cycling and storage of mercury (Hg) in terrestrial ecosystems. This study aimed to assess differences in Hg cycling and storage resulting from different vegetation at two adjacent forest stands - beech and spruce. The study site Načetín in the Czech Republic's Black Triangle received high atmospheric loadings of Hg from coal combustion in the second half of the 20th century as documented by peat accumulation rates reaching 100 μg m-2 y1. In 2004, the annual litterfall Hg flux was 22.5 μg m2 y1 in the beech stand and 14.5 μg m2 y1 in the spruce stand. Soil concentrations and pools of Hg had a strong positive relation to soil organic matter and concentrations of soil sulfur (S) and nitrogen (N). O-horizon Hg concentrations ranged from 245 to 495 μg kg1 and were greater in the spruce stand soil, probably as a result of greater dry Hg deposition. Mineral soil Hg concentrations ranged from 51 to 163 μg kg1 and were greater in the beech stand soil due to its greater capacity to store organic carbon (C). The Hg/C ratio increased with depth from 0.3 in the O-horizon to 3.8 μg g1 in the C horizon of spruce soil and from 0.7 to 2.7 μg g1 in beech soil. The Hg/C ratio was greater at all mineral soil depths in the spruce stand. The organic soil Hg pools in beech and spruce stands (6.4 and 5.7 mg m2, respectively) were considerably lower than corresponding mineral soil Hg pools (39.1 and 25.8 mg m2). Despite the important role of S in Hg cycling, differences in soil Hg distribution at both stands could not be attributed to differences in soil sulfur speciation.

  • 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

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

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2016

  • Confidentiality

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

Data specific for result type

  • Name of the periodical

    Applied Geochemistry

  • ISSN

    0883-2927

  • e-ISSN

  • Volume of the periodical

    75

  • Issue of the periodical within the volume

    December

  • Country of publishing house

    GB - UNITED KINGDOM

  • Number of pages

    13

  • Pages from-to

    63-75

  • UT code for WoS article

    000390084900007

  • EID of the result in the Scopus database

    2-s2.0-84994310446