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Widespread Increases in Iron Concentration in European and North American Freshwaters

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F86652079%3A_____%2F17%3A00481710" target="_blank" >RIV/86652079:_____/17:00481710 - isvavai.cz</a>

  • Alternative codes found

    RIV/00025798:_____/17:00000100

  • Result on the web

    <a href="http://dx.doi.org/10.1002/2017GB005749" target="_blank" >http://dx.doi.org/10.1002/2017GB005749</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1002/2017GB005749" target="_blank" >10.1002/2017GB005749</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Widespread Increases in Iron Concentration in European and North American Freshwaters

  • Original language description

    American Geophysical Union. All Rights Reserved. Recent reports of increasing iron (Fe) concentrations in freshwaters are of concern, given the fundamental role of Fe in biogeochemical processes. Still, little is known about the frequency and geographical distribution of Fe trends or about the underlying drivers. We analyzed temporal trends of Fe concentrations across 340 water bodies distributed over 10 countries in northern Europe and North America in order to gain a clearer understanding of where, to what extent, and why Fe concentrations are on the rise. We found that Fe concentrations have significantly increased in 28% of sites, and decreased in 4%, with most positive trends located in northern Europe. Regions with rising Fe concentrations tend to coincide with those with organic carbon (OC) increases. Fe and OC increases may not be directly mechanistically linked, but may nevertheless be responding to common regional-scale drivers such as declining sulfur deposition or hydrological changes. A role of hydrological factors was supported by covarying trends in Fe and dissolved silica, as these elements tend to stem from similar soil depths. A positive relationship between Fe increases and conifer cover suggests that changing land use and expanded forestry could have contributed to enhanced Fe export, although increases were also observed in nonforested areas. We conclude that the phenomenon of increasing Fe concentrations is widespread, especially in northern Europe, with potentially significant implications for wider ecosystem biogeochemistry, and for the current browning of freshwaters.

  • 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

    <a href="/en/project/GA15-08124S" target="_blank" >GA15-08124S: Response of forest ecosystem biogeochemistry under future scenarios of acid deposition, eutrofication, forestry and climate change</a><br>

  • Continuities

    P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)<br>I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

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

    Global Biogeochemical Cycles

  • ISSN

    0886-6236

  • e-ISSN

  • Volume of the periodical

    31

  • Issue of the periodical within the volume

    10

  • Country of publishing house

    US - UNITED STATES

  • Number of pages

    13

  • Pages from-to

    1488-1500

  • UT code for WoS article

    000416625200002

  • EID of the result in the Scopus database

    2-s2.0-85031758536