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Description
  • Není k dispozici (cs)
  • Uhlířská (1.87 km2), is a typical watershed with the crystalline bedrock forming Cambisols as 60% of the area of the Czech Basin. It is situated in a humid mountainous region where soils are typically shallow and highly permeable. Quantitative hydrological measurements performed here lack the information about the nature of the transformation in space and time.New multielectrode geophysical method was employed in the watershed scale to specify the closer image of the examined subsurface. Due to the fact that the behavior of flow of water in the heterogeneous porous media and highly heterogeneous hydrogeological structure is not fully understood, a targeted study of these phenomena in the field scale becomes very urgent. Study of the water dynamics by means of natural tracers is targeted to employ effects of stable oxygen isotope 18O (and silica as SiO2 within the elements of the hydrological cycle. (en)
  • Uhlířská (1.87 km2), is a typical watershed with the crystalline bedrock forming Cambisols as 60% of the area of the Czech Basin. It is situated in a humid mountainous region where soils are typically shallow and highly permeable. Quantitative hydrological measurements performed here lack the information about the nature of the transformation in space and time.New multielectrode geophysical method was employed in the watershed scale to specify the closer image of the examined subsurface. Due to the fact that the behavior of flow of water in the heterogeneous porous media and highly heterogeneous hydrogeological structure is not fully understood, a targeted study of these phenomena in the field scale becomes very urgent. Study of the water dynamics by means of natural tracers is targeted to employ effects of stable oxygen isotope 18O (and silica as SiO2 within the elements of the hydrological cycle.
Title
  • Tracing of the water flowpath in the soil profile of the mountainous wateshed by means of natural elements
  • Tracing of the water flowpath in the soil profile of the mountainous wateshed by means of natural elements (en)
  • Detekce cest proudění v půdním profilu horského povodí pomocí přirozených prvků (cs)
skos:prefLabel
  • Tracing of the water flowpath in the soil profile of the mountainous wateshed by means of natural elements
  • Tracing of the water flowpath in the soil profile of the mountainous wateshed by means of natural elements (en)
  • Detekce cest proudění v půdním profilu horského povodí pomocí přirozených prvků (cs)
skos:notation
  • RIV/68407700:21110/06:01126003!RIV07-GA0-21110___
http://linked.open.../vavai/riv/strany
  • 131 ; 132
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • P(GA205/06/0375)
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
  • 504111
http://linked.open...ai/riv/idVysledku
  • RIV/68407700:21110/06:01126003
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • Crystalline bedrock; Hillslope; Natural tracers; Soil profile; Watershed (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...ontrolniKodProRIV
  • [2036AB7F808D]
http://linked.open...v/mistoKonaniAkce
  • Luxembourg
http://linked.open...i/riv/mistoVydani
  • Luxemburk
http://linked.open...i/riv/nazevZdroje
  • Proceedings of the Eleventh Biennial conference of the Euromediterranean Network of experimental and representative basins (ERB)
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
  • Novák, Lukáš
  • Šanda, Martin
  • Hrnčíř, Miroslav
http://linked.open...vavai/riv/typAkce
http://linked.open.../riv/zahajeniAkce
number of pages
http://purl.org/ne...btex#hasPublisher
  • CRP - Gabriel Lippmann
https://schema.org/isbn
  • 2-919900-06-4
http://localhost/t...ganizacniJednotka
  • 21110
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