About: Soil water movement during the extreme precipitation in the Šumava Mts. and in the Krkonoše Mts. in August 2002     Goto   Sponge   NotDistinct   Permalink

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Description
  • The objective of this study was to assess an impact of plant cover on hydrophysical characteristics of sandy soil at the locality Mláky II at Sekule (southwest Slovakia). Three sites were demarcated at the locality, with mainly grass species at site 1 (Meadow soil), pine forest at site 2 (Forest soil), and mainly moss species at site 3 (Glade soil). Almost pure sand, occurring at the depth of 50 cm at site 3 (Pure sand), was used as a blank sample where no impact of plant cover was detected. It was found that both the water drop penetration time WDPT and index of water repellency R decreased in the order: Forest soil - Glade soil - Meadow soil - Pure sand. In the same order there increased the sorptivity for water and the hydraulic conductivity: Forest soil - Glade soil - Meadow soil - Pure sand. The saturated hydraulic conductivity Ks increased in the order: Meadow soil - Glade soil - Forest soil - Pure sand.
  • The objective of this study was to assess an impact of plant cover on hydrophysical characteristics of sandy soil at the locality Mláky II at Sekule (southwest Slovakia). Three sites were demarcated at the locality, with mainly grass species at site 1 (Meadow soil), pine forest at site 2 (Forest soil), and mainly moss species at site 3 (Glade soil). Almost pure sand, occurring at the depth of 50 cm at site 3 (Pure sand), was used as a blank sample where no impact of plant cover was detected. It was found that both the water drop penetration time WDPT and index of water repellency R decreased in the order: Forest soil - Glade soil - Meadow soil - Pure sand. In the same order there increased the sorptivity for water and the hydraulic conductivity: Forest soil - Glade soil - Meadow soil - Pure sand. The saturated hydraulic conductivity Ks increased in the order: Meadow soil - Glade soil - Forest soil - Pure sand. (en)
Title
  • Soil water movement during the extreme precipitation in the Šumava Mts. and in the Krkonoše Mts. in August 2002
  • Soil water movement during the extreme precipitation in the Šumava Mts. and in the Krkonoše Mts. in August 2002 (en)
skos:prefLabel
  • Soil water movement during the extreme precipitation in the Šumava Mts. and in the Krkonoše Mts. in August 2002
  • Soil water movement during the extreme precipitation in the Šumava Mts. and in the Krkonoše Mts. in August 2002 (en)
skos:notation
  • RIV/68378289:_____/08:00341876!RIV10-MZP-68378289
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • P(1QS200420562), P(GA205/06/0375), P(GA205/08/1174), P(GA526/08/1016), P(SP/1A6/151/07), Z(AV0Z20600510), Z(AV0Z30420517)
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
  • 395764
http://linked.open...ai/riv/idVysledku
  • RIV/68378289:_____/08:00341876
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • mountain hydrology; extreme rain; soil-water movement (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...ontrolniKodProRIV
  • [4C7B2A2797A3]
http://linked.open...v/mistoKonaniAkce
  • Cracow
http://linked.open...i/riv/mistoVydani
  • Cracow
http://linked.open...i/riv/nazevZdroje
  • Hydrological Extremes in Small Basins
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
  • Polívka, Jiří
  • Tesař, Miroslav
  • Šír, Miloslav
  • Fišák, Jaroslav
  • Krejča, M.
http://linked.open...vavai/riv/typAkce
http://linked.open.../riv/zahajeniAkce
http://linked.open...n/vavai/riv/zamer
number of pages
http://purl.org/ne...btex#hasPublisher
  • IGIP
https://schema.org/isbn
  • 978-83-88424-38-0
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