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  • Within the framework of the research of preferential flow in clay-loam soil at Valecov site in Bohemo-Moravian highland, field ponded infiltration experiment monitored by TDR and resistivity tomography. TDR method was able to detect slow water content increase throughout the infiltration; however, it was not able to detect all the water added to the soil right from the start of the experiment. The resistivity tomography was performed using ARES system. The results imply that the measuring technique in its present state is not suitable for the clay soil. The outputs of the geophysical methods were found inconclusive. At the end of the infiltration experiment, a dye tracer and excavation was used to visualize the flow paths. The tracer was found to infiltrate about 4 times deeper than predicted based on the tracer volume, assuming flow in fully saturated soil. The findings from the field measurements were validated in laboratory experiments using undisturbed samples of the soil.
  • Within the framework of the research of preferential flow in clay-loam soil at Valecov site in Bohemo-Moravian highland, field ponded infiltration experiment monitored by TDR and resistivity tomography. TDR method was able to detect slow water content increase throughout the infiltration; however, it was not able to detect all the water added to the soil right from the start of the experiment. The resistivity tomography was performed using ARES system. The results imply that the measuring technique in its present state is not suitable for the clay soil. The outputs of the geophysical methods were found inconclusive. At the end of the infiltration experiment, a dye tracer and excavation was used to visualize the flow paths. The tracer was found to infiltrate about 4 times deeper than predicted based on the tracer volume, assuming flow in fully saturated soil. The findings from the field measurements were validated in laboratory experiments using undisturbed samples of the soil. (en)
Title
  • Geophysical Methods in a Study of the Infiltration Process in Clay Soil
  • Geophysical Methods in a Study of the Infiltration Process in Clay Soil (en)
skos:prefLabel
  • Geophysical Methods in a Study of the Infiltration Process in Clay Soil
  • Geophysical Methods in a Study of the Infiltration Process in Clay Soil (en)
skos:notation
  • RIV/68407700:21110/06:00126714!RIV11-GA0-21110___
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • P(GA103/04/0663)
http://linked.open...vai/riv/dodaniDat
http://linked.open...aciTvurceVysledku
http://linked.open.../riv/druhVysledku
http://linked.open...iv/duvernostUdaju
http://linked.open...titaPredkladatele
http://linked.open...dnocenehoVysledku
  • 477040
http://linked.open...ai/riv/idVysledku
  • RIV/68407700:21110/06:00126714
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • ERT; Ponded infiltration; TDR; Vadose zone (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...ontrolniKodProRIV
  • [024A05BCE10B]
http://linked.open...v/mistoKonaniAkce
  • Vídeň
http://linked.open...i/riv/mistoVydani
  • Strasbourg Ceres
http://linked.open...i/riv/nazevZdroje
  • Geophysical Research Abstracts: Volume 8, 2006
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...cetTvurcuVysledku
http://linked.open...vavai/riv/projekt
http://linked.open...UplatneniVysledku
http://linked.open...iv/tvurceVysledku
  • Císlerová, Milena
  • Jelínková, Vladimíra
  • Votrubová, J.
http://linked.open...vavai/riv/typAkce
http://linked.open.../riv/zahajeniAkce
issn
  • 1029-7006
number of pages
http://purl.org/ne...btex#hasPublisher
  • European Geosciences Union
http://localhost/t...ganizacniJednotka
  • 21110
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