A Saturated Excess Runoff Pedotransfer Function for Vegetated Watersheds
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68407700%3A21110%2F13%3A00213090" target="_blank" >RIV/68407700:21110/13:00213090 - isvavai.cz</a>
Výsledek na webu
<a href="http://vzj.geoscienceworld.org/content/12/4/vzj2013.03.0060.abstract" target="_blank" >http://vzj.geoscienceworld.org/content/12/4/vzj2013.03.0060.abstract</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.2136/vzj2013.03.0060" target="_blank" >10.2136/vzj2013.03.0060</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
A Saturated Excess Runoff Pedotransfer Function for Vegetated Watersheds
Popis výsledku v původním jazyce
Since Hewlett and Hibbert?s publication in 1967, there has been a slow recognition that saturated excess runoff is the main runoff mechanism in vegetated watersheds. Yet, most pedotransfer functions for predicting runoff are based on infiltration excessrunoff. We, therefore, developed a simple pedotransfer function to predict saturation excess runoff, using data from eight watersheds on three continents. The runoff response was very similar for all watersheds, despite differences in climate, size, topography, and land use. Direct storm runoff occurred after a threshold amount of rainfall was exceeded. Runoff was linearly related to rainfall depth, indicating that a nearly constant proportion of the watershed was the source area. Size of source areas decreased with increasing depths of soils. The rainfall threshold was strongly dependent on the initial moisture conditions. The developed pedotransfer function for saturation excess runoff was used to predict water level fluctuation of tw
Název v anglickém jazyce
A Saturated Excess Runoff Pedotransfer Function for Vegetated Watersheds
Popis výsledku anglicky
Since Hewlett and Hibbert?s publication in 1967, there has been a slow recognition that saturated excess runoff is the main runoff mechanism in vegetated watersheds. Yet, most pedotransfer functions for predicting runoff are based on infiltration excessrunoff. We, therefore, developed a simple pedotransfer function to predict saturation excess runoff, using data from eight watersheds on three continents. The runoff response was very similar for all watersheds, despite differences in climate, size, topography, and land use. Direct storm runoff occurred after a threshold amount of rainfall was exceeded. Runoff was linearly related to rainfall depth, indicating that a nearly constant proportion of the watershed was the source area. Size of source areas decreased with increasing depths of soils. The rainfall threshold was strongly dependent on the initial moisture conditions. The developed pedotransfer function for saturation excess runoff was used to predict water level fluctuation of tw
Klasifikace
Druh
J<sub>x</sub> - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
CEP obor
DA - Hydrologie a limnologie
OECD FORD obor
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Návaznosti výsledku
Projekt
<a href="/cs/project/GA205%2F09%2F0831" target="_blank" >GA205/09/0831: Hydrologická odezva povodí: Posouzení hypotézy mechanismu odtoku s uvážením dat o pohybu přirozených stopovačů</a><br>
Návaznosti
Z - Vyzkumny zamer (s odkazem do CEZ)<br>S - Specificky vyzkum na vysokych skolach
Ostatní
Rok uplatnění
2013
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Vadose Zone Journal
ISSN
1539-1663
e-ISSN
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Svazek periodika
12
Číslo periodika v rámci svazku
4
Stát vydavatele periodika
US - Spojené státy americké
Počet stran výsledku
10
Strana od-do
1-10
Kód UT WoS článku
000328628400042
EID výsledku v databázi Scopus
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