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Variation of water stage and underground water level in Židlochovice area

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F62156489%3A43210%2F08%3A00128480" target="_blank" >RIV/62156489:43210/08:00128480 - isvavai.cz</a>

  • Result on the web

  • DOI - Digital Object Identifier

Alternative languages

  • Result language

    čeština

  • Original language name

    Kolísání vodních stavů a hladiny podzemní vody v oblasti Židlochovicka

  • Original language description

    In this contribution the impact of river on the level of underground water within one year or long-term period was presented on the example of river flood-plain. Soil type of selected locality is the Gleyic Fluvisols (old Czech name is Wold Soils). ThisSoil type is created in river and creek wold i.e. from floods sediments. These areas were drained in former times and water courses were regulated by human activity as reaction to annual floods. The results of 13 years monitoring of Svratka river dynamics and level of underground water on clay-loam arable soil of maize production region are presented. On experimental area Žabčice (close to Židlochovice) the level oscilation of underground water within one year or long-term period (1995--2007) was shown.Weekly data of underground water level come from drill--hole VB0326 Nosislav (belongs to CHMI network). Weekly data of Svratka water level come from measure point 4620 Židlochovice (also CHMI network). Moisture soil regime of experimenta

  • Czech name

    Kolísání vodních stavů a hladiny podzemní vody v oblasti Židlochovicka

  • Czech description

    In this contribution the impact of river on the level of underground water within one year or long-term period was presented on the example of river flood-plain. Soil type of selected locality is the Gleyic Fluvisols (old Czech name is Wold Soils). ThisSoil type is created in river and creek wold i.e. from floods sediments. These areas were drained in former times and water courses were regulated by human activity as reaction to annual floods. The results of 13 years monitoring of Svratka river dynamics and level of underground water on clay-loam arable soil of maize production region are presented. On experimental area Žabčice (close to Židlochovice) the level oscilation of underground water within one year or long-term period (1995--2007) was shown.Weekly data of underground water level come from drill--hole VB0326 Nosislav (belongs to CHMI network). Weekly data of Svratka water level come from measure point 4620 Židlochovice (also CHMI network). Moisture soil regime of experimenta

Classification

  • Type

    D - Article in proceedings

  • CEP classification

    DF - Pedology

  • OECD FORD branch

Result continuities

  • Project

    <a href="/en/project/2B06101" target="_blank" >2B06101: The optimization of both agricultural and river landscape in the Czech Republic with an emphasis on the biodiversity process.</a><br>

  • Continuities

    P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Others

  • Publication year

    2008

  • Confidentiality

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

Data specific for result type

  • Article name in the collection

    Bioklimatologické aspekty hodnocení procesů v krajině

  • ISBN

    978-80-86690-55-1

  • ISSN

  • e-ISSN

  • Number of pages

    1

  • Pages from-to

  • Publisher name

    ČBkS

  • Place of publication

  • Event location

    Mikulov

  • Event date

    Jan 1, 2008

  • Type of event by nationality

    EUR - Evropská akce

  • UT code for WoS article