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Statements

Subject Item
n2:RIV%2F68407700%3A21110%2F12%3A00201318%21RIV13-GA0-21110___
rdf:type
n10:Vysledek skos:Concept
dcterms:description
Variation of quasi steady state flow rates was observed during recurrent ponded infiltration experiments on three small undisturbed samples of coarse sandy loam. Two main flow irregularities typical for soil under study were detected for two soil samples during recurrent ponding experiment: (1) Gradual decrease of the quasi-saturated hydraulic conductivity (Kqs) soon after outflow appeared and (2) lower Kqs during the second infiltration run. The third sample didn't produce similar variability. Series of neutron tomography images of the sample taken during quasi-steady state stage of the first infiltration run have detected trapping of the air bubbles in many of large pores and cavities. Furthermore, the volume of many of entrapped air bubbles increased during the course of the first infiltration run. Further entrapped air redistribution has been detected during the second run. The fraction of the entrapped air was calculated for series of tomography images taken during each experiment. The increase of entrapped air bubbles volumetric fraction by only 0.005 was accompanied by decrease of quasi-saturated hydraulic conductivity by up to 50% of the initial value. The experimental results support the hypothesis that the effect of the gradual decrease of Kqs is caused by entrapped air redistribution and build-up of bubbles in preferential pathways. The trapped air may thus restrict the preferential flow pathways and cause lower infiltration and outflow flux rates. This behavior however occurred only in samples with well-connected vertical structures. Variation of quasi steady state flow rates was observed during recurrent ponded infiltration experiments on three small undisturbed samples of coarse sandy loam. Two main flow irregularities typical for soil under study were detected for two soil samples during recurrent ponding experiment: (1) Gradual decrease of the quasi-saturated hydraulic conductivity (Kqs) soon after outflow appeared and (2) lower Kqs during the second infiltration run. The third sample didn't produce similar variability. Series of neutron tomography images of the sample taken during quasi-steady state stage of the first infiltration run have detected trapping of the air bubbles in many of large pores and cavities. Furthermore, the volume of many of entrapped air bubbles increased during the course of the first infiltration run. Further entrapped air redistribution has been detected during the second run. The fraction of the entrapped air was calculated for series of tomography images taken during each experiment. The increase of entrapped air bubbles volumetric fraction by only 0.005 was accompanied by decrease of quasi-saturated hydraulic conductivity by up to 50% of the initial value. The experimental results support the hypothesis that the effect of the gradual decrease of Kqs is caused by entrapped air redistribution and build-up of bubbles in preferential pathways. The trapped air may thus restrict the preferential flow pathways and cause lower infiltration and outflow flux rates. This behavior however occurred only in samples with well-connected vertical structures.
dcterms:title
Investigating the fate of entrapped air bubbles during quasi-saturated flow in natural soil Investigating the fate of entrapped air bubbles during quasi-saturated flow in natural soil
skos:prefLabel
Investigating the fate of entrapped air bubbles during quasi-saturated flow in natural soil Investigating the fate of entrapped air bubbles during quasi-saturated flow in natural soil
skos:notation
RIV/68407700:21110/12:00201318!RIV13-GA0-21110___
n10:predkladatel
n18:orjk%3A21110
n4:aktivita
n11:S n11:P
n4:aktivity
P(GA103/08/1552), S
n4:dodaniDat
n13:2013
n4:domaciTvurceVysledku
n5:5902320 n5:4388860 n5:1873601 n5:6594050
n4:druhVysledku
n9:O
n4:duvernostUdaju
n15:S
n4:entitaPredkladatele
n12:predkladatel
n4:idSjednocenehoVysledku
142860
n4:idVysledku
RIV/68407700:21110/12:00201318
n4:jazykVysledku
n8:eng
n4:klicovaSlova
neutron tomography; infiltration; multiphase flow
n4:klicoveSlovo
n16:neutron%20tomography n16:multiphase%20flow n16:infiltration
n4:kontrolniKodProRIV
[8BF7A9D60BED]
n4:obor
n6:DF
n4:pocetDomacichTvurcuVysledku
4
n4:pocetTvurcuVysledku
4
n4:projekt
n17:GA103%2F08%2F1552
n4:rokUplatneniVysledku
n13:2012
n4:tvurceVysledku
Císlerová, Milena Sněhota, Michal Sobotková, Martina Jelínková, Vladimíra
n14:organizacniJednotka
21110