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Event water detection in tile drainage runoff using stable isotopes and a water temperature in small agricultural catchment in Bohemian-Moravian Highlands, Czech Republic

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00027049%3A_____%2F16%3AN0000013" target="_blank" >RIV/00027049:_____/16:N0000013 - isvavai.cz</a>

  • Result on the web

    <a href="http://link.springer.com/journal/12665" target="_blank" >http://link.springer.com/journal/12665</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1007/s12665-016-5561-1" target="_blank" >10.1007/s12665-016-5561-1</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Event water detection in tile drainage runoff using stable isotopes and a water temperature in small agricultural catchment in Bohemian-Moravian Highlands, Czech Republic

  • Original language description

    The tile drainage runoff composition during rainfall–runoff (R-R) events was examined in a small agricultural catchment Dehtáře (Bohemian-Moravian Highlands, Czech Republic). Drainage systems in this region of crystalline bedrock are typically built in slopes and they have complicated runoff generation. For runoff separation, analysis of stable isotopes 18O and 2H was used and compared to sudden changes in drainage water temperature. The analysis of eighteen hydrographs showed that the drainage runoff was composed of 1%–58% event water during summer events, with a maximum temporary share of 11% and 88%. During winter events, the pre-event water significantly dominated. In all cases when event water was detected in the drainage runoff, a rapid change in the drainage water temperature was observed as well. Its values during R-R events converged toward the temperature of the precipitation, which was very similar to that of the air (R2=0.98%). As the magnitude of the water temperature change was proportional to the event water portion in the drainage runoff (R2=0.91), it is possible to state that a sudden change in drainage water temperature indicates the presence of event water in the drainage runoff and it is possible to use water temperature successfully to separate the runoff components.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)

  • CEP classification

    DA - Hydrology and limnology

  • OECD FORD branch

Result continuities

  • Project

  • 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

    Environmental earth sciences

  • ISSN

    1866-6299

  • e-ISSN

  • Volume of the periodical

    neuveden

  • Issue of the periodical within the volume

    75

  • Country of publishing house

    DE - GERMANY

  • Number of pages

    14

  • Pages from-to

    1-13

  • UT code for WoS article

  • EID of the result in the Scopus database