The Comparison of Water and Matter Flows in Three Small Catchments in the Šumava Mountains

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60076658%3A12220%2F09%3A00010875" target="_blank" >RIV/60076658:12220/09:00010875 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/25173154:_____/09:#0000100

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

The Comparison of Water and Matter Flows in Three Small Catchments in the Šumava Mountains

Popis výsledku v původním jazyce

The comparisons of water and matter flows have been evaluated in three small catchments with different land uses in the Šumava Mountains in the south-west of the Czech Republic since 1999. The catchment of the Mlýnský stream was artificially drained, theareas of the catchment retaining the character of drained, semi-intensive pasture. The catchment of the Horský stream is covered with forest, mowed meadows, and locations with natural succession (wetlands). The catchment of the Bukový stream is coveredwith forest, mostly with spruce monoculture. The highest amount of water was discharged from the drained Mlýnský catchment whereas the amounts of water discharged from the Horský and Bukový catchments were lower. The runoff maxima in the hydrologic yearof 2002 were recorded in the Mlýnský stream catchment in august ? at the time of the catastrophic floods. On the other hand, the maximum discharges in the Horský and Bukový stream catchments in august 2002 were comparable with those that

Název v anglickém jazyce

The Comparison of Water and Matter Flows in Three Small Catchments in the Šumava Mountains

Popis výsledku anglicky

The comparisons of water and matter flows have been evaluated in three small catchments with different land uses in the Šumava Mountains in the south-west of the Czech Republic since 1999. The catchment of the Mlýnský stream was artificially drained, theareas of the catchment retaining the character of drained, semi-intensive pasture. The catchment of the Horský stream is covered with forest, mowed meadows, and locations with natural succession (wetlands). The catchment of the Bukový stream is coveredwith forest, mostly with spruce monoculture. The highest amount of water was discharged from the drained Mlýnský catchment whereas the amounts of water discharged from the Horský and Bukový catchments were lower. The runoff maxima in the hydrologic yearof 2002 were recorded in the Mlýnský stream catchment in august ? at the time of the catastrophic floods. On the other hand, the maximum discharges in the Horský and Bukový stream catchments in august 2002 were comparable with those that

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

EH - Ekologie – společenstva

OECD FORD obor

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Projekt

<a href="/cs/project/2B06023" target="_blank" >2B06023: Vývoj metody stanovení toků energie a látek ve vybraných ekosystémech, návrh a ověření principů hodnocení hospodářských zásahů pro zajištění podmínek autoregulace a rozvoje biodiverzity</a><br>

Návaznosti

Z - Vyzkumny zamer (s odkazem do CEZ)

Rok uplatnění

2009

Kód důvěrnosti údajů

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

Název periodika

Soil and Water Research

ISSN

1801-5395

e-ISSN

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Svazek periodika

4

Číslo periodika v rámci svazku

2

Stát vydavatele periodika

CZ - Česká republika

Počet stran výsledku

8

Strana od-do

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Kód UT WoS článku

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EID výsledku v databázi Scopus

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