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Using the dye tracer experiment for characterisation of parameters of the dual-permeability model
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SYSNO ASEP 0353933 Druh ASEP C - Konferenční příspěvek (mezinárodní konf.) Zařazení RIV D - Článek ve sborníku Název Using the dye tracer experiment for characterisation of parameters of the dual-permeability model Tvůrce(i) Kodešová, R. (CZ)
Němeček, K. (CZ)
Jirků, V. (CZ)
Nikodem, A. (CZ)
Fér, M. (CZ)
Jakšík, O. (CZ)
Kočárek, M. (CZ)
Žigová, Anna (GLU-S) RID, SAI, ORCIDZdroj.dok. 19th World Congress of Soil Science : soil solutions for a changing world, Brisbane, Australia, 1-6 August 2010 : proceedings. - Brisbane : International Union of Soil Sciences.; Australian Society of Soil Science, 2010 / Gilkes R. J. ; Pragongkep N. - ISBN 978-0-646-53783-2 Rozsah stran s. 117-120 Poč.str. 4 s. Forma vydání WWW ; DVD ROM - WWW ; DVD ROM Akce World Congress of Soil Science /19./ Datum konání 01.08.2010-06.08.2010 Místo konání Brisbane Země AU - Austrálie Typ akce WRD Jazyk dok. eng - angličtina Země vyd. AU - Austrálie Klíč. slova soil structure ; preferential flow ; dye tracer experiment ; micromorphological images ; parameter optimisation Vědní obor RIV DF - Pedologie CEP GA526/08/0434 GA ČR - Grantová agentura ČR CEZ AV0Z30130516 - GLU-S (2005-2011) Anotace This study is focused on the visualization of the preferential flow in different soil types using the dye tracer experiment. The field ponding dye infiltration experiments were performed in two soil types: Haplic Luvisol and Haplic Cambisol. The tension disc infiltrometer and the Guelph permeameter measurements were performed in the field at various horizons. In addition, the thin soil sections were made and micromorphological images were used to study soil aggregate structure and dye distribution at a microscale. While preferential flow in Haplic Luvisol was caused by soil aggregation and biopores, preferential flow in Haplic Cambisol was caused only by biopores and large gravitational soil fractures. Information about the dual-domain geometry and the dual-permeability models in HYDRUS-1D and HYDRUS 2/3D were then used to simulate preferential flow in studied soil types. Pracoviště Geologický ústav Kontakt Jana Popelková, popelkova@gli.cas.cz, Sabina Janíčková, Tel.: 233 087 272 Rok sběru 2012
Počet záznamů: 1