About: Hydrological Processes in the Subsurface Investigated by Water Isotopes and Silica     Goto   Sponge   NotDistinct   Permalink

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  • The hillslope rainfall-outflow interactions, groundwater fluxes were examined in the headwater catchment Uhlířská, Czech Republic. A quick communication of the vadose zone with the granitic bedrock via preferential subsurface flowpaths is assumed, in agreement with the observation of storm-caused instant water transformation to outflow through the permeable Cambisol. A quick response of a high magnitude outflow occurs regularly, although the surface runoff is very rare. Standard climatic and hydrological monitoring in the Uhlířská catchment is supplemented by the measurements of processes in the vadose zone and natural tracing of isotope 18O and 2H and SiO2 content in water. Up to 75% of the event catchment runoff was assigned to pre-event water, of which about 50% had been stored in the shallow soil subsurface on the hillslopes. The hillslope soil layers control the distribution of the flow into the groundwater and/or the shallow subsurface flow during the rainfall-runoff episode (en)
  • The hillslope rainfall-outflow interactions, groundwater fluxes were examined in the headwater catchment Uhlířská, Czech Republic. A quick communication of the vadose zone with the granitic bedrock via preferential subsurface flowpaths is assumed, in agreement with the observation of storm-caused instant water transformation to outflow through the permeable Cambisol. A quick response of a high magnitude outflow occurs regularly, although the surface runoff is very rare. Standard climatic and hydrological monitoring in the Uhlířská catchment is supplemented by the measurements of processes in the vadose zone and natural tracing of isotope 18O and 2H and SiO2 content in water. Up to 75% of the event catchment runoff was assigned to pre-event water, of which about 50% had been stored in the shallow soil subsurface on the hillslopes. The hillslope soil layers control the distribution of the flow into the groundwater and/or the shallow subsurface flow during the rainfall-runoff episode
Title
  • Hydrological Processes in the Subsurface Investigated by Water Isotopes and Silica
  • Hydrological Processes in the Subsurface Investigated by Water Isotopes and Silica (en)
skos:prefLabel
  • Hydrological Processes in the Subsurface Investigated by Water Isotopes and Silica
  • Hydrological Processes in the Subsurface Investigated by Water Isotopes and Silica (en)
skos:notation
  • RIV/00020711:_____/10:00003086!RIV13-MZP-00020711
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • P(GA205/06/0375), V, Z(AV0Z20600510), Z(MZP0002071101)
http://linked.open...iv/cisloPeriodika
  • Spec 2
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
  • 318159
http://linked.open...ai/riv/idVysledku
  • RIV/00020711:_____/10:00003086
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • rainfall to runoff response, isotopes, geochemical tracers, streamflow generation, subsurface stormflow (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • CZ - Česká republika
http://linked.open...ontrolniKodProRIV
  • [7DAFE6C7B796]
http://linked.open...i/riv/nazevZdroje
  • Soil and Water Research
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...v/svazekPeriodika
  • 4
http://linked.open...iv/tvurceVysledku
  • Císlerová, Milena
  • Kulasová, Alena
  • Sanda, Martin
http://linked.open...n/vavai/riv/zamer
issn
  • 1801-5395
number of pages
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