Pohyb půdní vody při extrémních srážkách na Šumavě a v Krkonoších v srpnu 2002

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68378289%3A_____%2F08%3A00321060" target="_blank" >RIV/68378289:_____/08:00321060 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/67985874:_____/08:00321060 RIV/68378289:_____/08:00341876 RIV/67985874:_____/08:00341876

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Soil water movement during the extreme precipitation in the Šumava Mts. and in the Krkonoše Mts. in August 2002

Popis výsledku v původním jazyce

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: Forestsoil - Glade soil - Meadow soil - Pure sand. The saturated hydraulic conductivity Ks increased in the order: Meadow soil - Glade soil - Forest soil - Pure sand.

Název v anglickém jazyce

Soil water movement during the extreme precipitation in the Šumava Mts. and in the Krkonoše Mts. in August 2002

Popis výsledku anglicky

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: Forestsoil - Glade soil - Meadow soil - Pure sand. The saturated hydraulic conductivity Ks increased in the order: Meadow soil - Glade soil - Forest soil - Pure sand.

Druh

D - Stať ve sborníku

CEP obor

DA - Hydrologie a limnologie

OECD FORD obor

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Projekt

Výsledek vznikl pri realizaci vícero projektů. Více informací v záložce Projekty.

Návaznosti

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)<br>Z - Vyzkumny zamer (s odkazem do CEZ)

Rok uplatnění

2008

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název statě ve sborníku

Hydrological Extremes in Small Basins

ISBN

978-83-88424-38-0

ISSN

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e-ISSN

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Počet stran výsledku

4

Strana od-do

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Název nakladatele

IGIP

Místo vydání

Cracow

Místo konání akce

Cracow

Datum konání akce

18. 9. 2008

Typ akce podle státní příslušnosti

WRD - Celosvětová akce

Kód UT WoS článku

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