Number of the records: 1  

Using the dye tracer for visualization of preferential flow in macro and micro-scale

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    SYSNO ASEP0343077
    Document TypeA - Abstract
    R&D Document TypeThe record was not marked in the RIV
    R&D Document TypeNení vybrán druh dokumentu
    TitleUsing the dye tracer for visualization of preferential flow in macro and micro-scale
    Author(s) Kodešová, R. (CZ)
    Němeček, K. (CZ)
    Kodeš, V. (CZ)
    Fér, M. (CZ)
    Jirků, V. (CZ)
    Nikodem, A. (CZ)
    Žigová, Anna (GLU-S) RID, SAI, ORCID
    Jakšík, O. (CZ)
    Kočárek, M. (CZ)
    Source TitleGeophysical Research Abstracts - ISSN 1607-7962
    Roč. 12, - (2010)
    Number of pages1 s.
    ActionEuropean Geosciences Union General Assembly 2010
    Event date02.05.2010-07.05.2010
    VEvent locationWienna
    CountryAT - Austria
    Event typeWRD
    Languageeng - English
    CountryUS - United States
    Keywordsdye tracer ; preferential flow ; micromorphology
    Subject RIVDF - Soil Science
    R&D ProjectsGA526/08/0434 GA ČR - Czech Science Foundation (CSF)
    CEZAV0Z30130516 - GLU-S (2005-2011)
    AnnotationStudy was performed in the Haplic Luvisol in Hněvčeves and the Haplic Cambisol in Humpolec in the Czech Republic. The 100 (Haplic Luvisol) and 50 (Haplic Cambisol) litres of solute of dye Brilliant Blue FCF (5 g/litre) was infiltrated on a 1x1 m plot (applying an initial ponding depth of 10 and 5 cm, respectively) immediately after the wheat harvest. The 3-D image od the dye distribution was created. In addition, the thin soil section were made and micromorphological images were used to study a soil aggregate structure and dye disrtibution in microscale. Images of the Haplic Luvisol showed that while dye tracer was partly regularly transported and only some isolated domains were visible in the surface Ap1 horizon, the preferential flow occured in the subsurface horizons. Images of the Haplic Cambisol showed that dye tracer transport in the Haplic Cambisol was in all horizons (Ap, Bw, C) mainly affected by the preferential flow caused by the gravitational fractures and biopores.
    WorkplaceInstitute of Geology
    ContactJana Popelková, popelkova@gli.cas.cz, Sabina Janíčková, Tel.: 233 087 272
    Year of Publishing2011
Number of the records: 1  

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