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Climate change increasing calcium and magnesium leaching from granitic alpine catchments

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60077344%3A_____%2F17%3A00479732" target="_blank" >RIV/60077344:_____/17:00479732 - isvavai.cz</a>

  • Alternative codes found

    RIV/00216208:11310/17:10336670

  • Result on the web

    <a href="http://dx.doi.org/10.1021/acs.est.6b03575" target="_blank" >http://dx.doi.org/10.1021/acs.est.6b03575</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1021/acs.est.6b03575" target="_blank" >10.1021/acs.est.6b03575</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Climate change increasing calcium and magnesium leaching from granitic alpine catchments

  • Original language description

    Climate change can reverse trends of decreasing calcium and magnesium [Ca + Mg] leaching to surface waters in granitic alpine regions recovering from acidification. Despite decreasing concentrations of strong acid anions (-1.4 mu eq L-1 yr(-1)) during 2004-2016 in nonacidic alpine lakes in the Tatra Mountains (Central Europe), the average [Ca + Mg] concentrations increased (2.5 mu eq L-1 yr(-1)), together with elevated terrestrial export of bicarbonate (HCO3-, 3.6 mu eq L-1 yr(-1)). The percent increase in [Ca + Mg] concentrations in nonacidic lakes (0.3-3.2% yr(-1)) was significantly and positively correlated with scree proportion in the catchment area and negatively correlated with the extent of soil cover. Leaching experiments with freshly crushed granodiorite, the dominant bedrock,showed that accessory calcite and (to a lesser extent) apatite were important sources of Ca. We hypothesize that elevated terrestrial export of [Ca + Mg] :and HCO3- resulted from increased weathering caused by accelerated physical erosion of rocks due to elevated climate-related mechanical forces (an increasing frequency of days with high precipitation amounts and air temperatures fluctuating around 0 degrees C) during the last 2-3 decades. These climatic effects on water chemistry are especially strong in catchments where fragmented rocks are more exposed to weathering, and their position is less stable than in soil.

  • 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

    10503 - Water resources

Result continuities

  • Project

    <a href="/en/project/GA14-09231S" target="_blank" >GA14-09231S: Disentangling the effects of changing environmental chemistry and climate on biogeochemistry and biodiversity of natural alpine soils and waters</a><br>

  • 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

    Environmental Science and Technology

  • ISSN

    0013-936X

  • e-ISSN

  • Volume of the periodical

    51

  • Issue of the periodical within the volume

    1

  • Country of publishing house

    US - UNITED STATES

  • Number of pages

    8

  • Pages from-to

    159-166

  • UT code for WoS article

    000391346900018

  • EID of the result in the Scopus database

    2-s2.0-85017524556