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Statements

Subject Item
n2:RIV%2F68407700%3A21110%2F14%3A00220746%21RIV15-MSM-21110___
rdf:type
skos:Concept n17:Vysledek
dcterms:description
Unsaturated hydraulic conductivity K(h) is key characteristic for numerical modeling of water flow and solute transport in the vadose zone. Tension infiltrometer is advantageous tool to conduct the measurement of unsaturated hydraulic conductivity in the field under near saturated conditions. Manually operated minidisk infiltrometers are often used for performing infiltration experiments, but their disadvantage is that permanent attendance is needed during experiments. Therefore automatization of the tension infiltrometer is desirable. Multidisk infiltrometer has been tested on four experimental locations. Two sites were situated at arable land (Nucice and Kopaninsky stream) and two located in headwater catchments Bohemian Forest and Jizera Mountains). Soils at experimental sites were classified as Dystric Cambisols, Cryptopodzols and Podzols (empirical van Genuchten parameters α and n ranged from 0.020 to 0.048 cm-1 and from 1.11 to 1.55 respectively). The infiltration experiments have confirmed, that the device is suitable and efficient tool for determination of unsaturated hydraulic conductivity in broad range of soils. Unsaturated hydraulic conductivity K(h) is key characteristic for numerical modeling of water flow and solute transport in the vadose zone. Tension infiltrometer is advantageous tool to conduct the measurement of unsaturated hydraulic conductivity in the field under near saturated conditions. Manually operated minidisk infiltrometers are often used for performing infiltration experiments, but their disadvantage is that permanent attendance is needed during experiments. Therefore automatization of the tension infiltrometer is desirable. Multidisk infiltrometer has been tested on four experimental locations. Two sites were situated at arable land (Nucice and Kopaninsky stream) and two located in headwater catchments Bohemian Forest and Jizera Mountains). Soils at experimental sites were classified as Dystric Cambisols, Cryptopodzols and Podzols (empirical van Genuchten parameters α and n ranged from 0.020 to 0.048 cm-1 and from 1.11 to 1.55 respectively). The infiltration experiments have confirmed, that the device is suitable and efficient tool for determination of unsaturated hydraulic conductivity in broad range of soils.
dcterms:title
Temporal Changes of Near-Saturated Hydraulic Conductivity in a Small Arable Catchment Temporal Changes of Near-Saturated Hydraulic Conductivity in a Small Arable Catchment
skos:prefLabel
Temporal Changes of Near-Saturated Hydraulic Conductivity in a Small Arable Catchment Temporal Changes of Near-Saturated Hydraulic Conductivity in a Small Arable Catchment
skos:notation
RIV/68407700:21110/14:00220746!RIV15-MSM-21110___
n3:aktivita
n11:S n11:P
n3:aktivity
P(GP13-20388P), P(TA01021844), S
n3:dodaniDat
n9:2015
n3:domaciTvurceVysledku
n12:8086583 n12:1272888 n12:9106286 n12:4388860
n3:druhVysledku
n13:O
n3:duvernostUdaju
n15:S
n3:entitaPredkladatele
n14:predkladatel
n3:idSjednocenehoVysledku
49758
n3:idVysledku
RIV/68407700:21110/14:00220746
n3:jazykVysledku
n6:eng
n3:klicovaSlova
soil structure; hydraulic conductivity; vadose zone; unsaturated soil; water regime
n3:klicoveSlovo
n4:unsaturated%20soil n4:water%20regime n4:soil%20structure n4:hydraulic%20conductivity n4:vadose%20zone
n3:kontrolniKodProRIV
[107755EFFCA9]
n3:obor
n8:DF
n3:pocetDomacichTvurcuVysledku
4
n3:pocetTvurcuVysledku
4
n3:projekt
n10:TA01021844 n10:GP13-20388P
n3:rokUplatneniVysledku
n9:2014
n3:tvurceVysledku
Klípa, Vladimír Zumr, David Sněhota, Michal Dohnal, Michal
n16:organizacniJednotka
21110