Runoff formation in small forested catchments in the Czech Republic.

Kód výsledku v IS VaVaI

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Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Runoff formation in small forested catchments in the Czech Republic.

Popis výsledku v původním jazyce

We dedicate this contribution to the question how the relation of outflow of water from the soil into the transport collector determined by hydropedological methods bears with the discharge at the closure profile of a small forest catchment in the courseof a vegetation season. In connection with this phenomena we investigate how much is such catchment homogenous. The monitored catchments Liz and Albrechtec are sloping, their geological subsoil is formed of impermeable bottom and they don't contain significant parts with ground water level. The soil cover is composed of several horizons with different aquifer properties, but the precipitated water largely infiltrates downwards the soil, so that a surface and subsurface runoff angle wise downhill to thewatercourse is a very rare phenomena which appears at catastrophic rains only. The forest stand is represented by spruce. The both catchments are located in the elevation from 700 to 1000 m a.s.l. in the mountain region of Šumava. Hydrol

Název v anglickém jazyce

Runoff formation in small forested catchments in the Czech Republic.

Popis výsledku anglicky

We dedicate this contribution to the question how the relation of outflow of water from the soil into the transport collector determined by hydropedological methods bears with the discharge at the closure profile of a small forest catchment in the courseof a vegetation season. In connection with this phenomena we investigate how much is such catchment homogenous. The monitored catchments Liz and Albrechtec are sloping, their geological subsoil is formed of impermeable bottom and they don't contain significant parts with ground water level. The soil cover is composed of several horizons with different aquifer properties, but the precipitated water largely infiltrates downwards the soil, so that a surface and subsurface runoff angle wise downhill to thewatercourse is a very rare phenomena which appears at catastrophic rains only. The forest stand is represented by spruce. The both catchments are located in the elevation from 700 to 1000 m a.s.l. in the mountain region of Šumava. Hydrol

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

2002

Kód důvěrnosti údajů

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

Název statě ve sborníku

Interdisciplinary approaches in small catchment hydrology: Monitoring and research.

ISBN

80-968480-6-2

ISSN

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e-ISSN

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Počet stran výsledku

5

Strana od-do

5-9

Název nakladatele

Slovak Committee for Hydrology - NC IHP UNESCO, Institute of Hydrology SAS

Místo vydání

Bratislava

Místo konání akce

Demänovská dolina [SK]

Datum konání akce

25. 9. 2002

Typ akce podle státní příslušnosti

EUR - Evropská akce

Kód UT WoS článku

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