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Ponded infiltration in a grid of permanent single-ring infiltrometers: Spatial versus temporal variability

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985874%3A_____%2F17%3A00476340" target="_blank" >RIV/67985874:_____/17:00476340 - isvavai.cz</a>

  • Alternative codes found

    RIV/68407700:21110/17:00306734 RIV/68407700:21720/17:00306734

  • Result on the web

    <a href="http://dx.doi.org/10.1515/johh-2017-0015" target="_blank" >http://dx.doi.org/10.1515/johh-2017-0015</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1515/johh-2017-0015" target="_blank" >10.1515/johh-2017-0015</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Ponded infiltration in a grid of permanent single-ring infiltrometers: Spatial versus temporal variability

  • Original language description

    Temporal variability of the soil hydraulic properties is still an open issue. The present study deals with results of ponded infiltration experiments performed annually in a grid of permanent measurement points (18 spatial and 14 temporal replicates). Single ring infiltrometers were installed in 2003 at a meadow site in the Bohemian Forest highlands, the Czech Republic. The soil at the plot is coarse sandy loam classified as oligotrophic Eutric Cambisol. Soil water flow below infiltration rings has distinctly preferential character.nThe results are marked with substantial interannual changes of observed infiltration rates. Considering just the results from the initial four years of the study, the temporal variability did not exceed the spatial variability detected in individual years. In later years, a shift to extremely high infiltration rates was observed. We hypothesize that it is related to structural changes of the soil profile possibly related to combined effect of soil biota activity, climatic conditions and experimental procedure. Interestingly, the temporal changes can partly be described as fluctuations between seemingly stable infiltration modes. This phenomenon was detected in the majority of rings and was found independent of the initial soil moisture conditions.

  • 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

    10501 - Hydrology

Result continuities

  • Project

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

  • 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

    Journal of Hydrology and Hydromechanics

  • ISSN

    0042-790X

  • e-ISSN

  • Volume of the periodical

    65

  • Issue of the periodical within the volume

    3

  • Country of publishing house

    SK - SLOVAKIA

  • Number of pages

    10

  • Pages from-to

    244-253

  • UT code for WoS article

    000406362800005

  • EID of the result in the Scopus database

    2-s2.0-85010476897