Drainage water temperature as a basis for verifying drainage runoff composition on slopes

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60076658%3A12220%2F11%3A43881955" target="_blank" >RIV/60076658:12220/11:43881955 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/60460709:41210/11:52661 RIV/00027049:_____/11:#0000582

Výsledek na webu

<a href="http://dx.doi.org/10.1002/hyp.8039" target="_blank" >http://dx.doi.org/10.1002/hyp.8039</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1002/hyp.8039" target="_blank" >10.1002/hyp.8039</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Drainage water temperature as a basis for verifying drainage runoff composition on slopes

Popis výsledku v původním jazyce

Tile drainage water temperatures and discharge rates were measured in five highland watersheds of which most are underlain by acid crystalline rock. One of them, Deht'aˇre in the Bohemo-Moravian highland (Czech Republic), was studied in greater detail. The aim was to evaluate water temperature monitoring as a means of determining the source and pathway of drainage runoff during high-flow events. Rapid increase in drainage discharge was accompanied by rapid change in water temperature. In winter, the rising limb of the hydrograph was accompanied by a decrease in temperature, and the falling limb was associated with a corresponding temperature increase. In summer, the trends were reversed. These data suggest that the water temperature changes are causedby the fastest component of drainage runoff, water from a precipitation event or snowmelt, which can be separated from the remainder of the hydrograph. Measurements of hydraulic conductivity, soil moisture content, soil temperature, and g

Název v anglickém jazyce

Drainage water temperature as a basis for verifying drainage runoff composition on slopes

Popis výsledku anglicky

Tile drainage water temperatures and discharge rates were measured in five highland watersheds of which most are underlain by acid crystalline rock. One of them, Deht'aˇre in the Bohemo-Moravian highland (Czech Republic), was studied in greater detail. The aim was to evaluate water temperature monitoring as a means of determining the source and pathway of drainage runoff during high-flow events. Rapid increase in drainage discharge was accompanied by rapid change in water temperature. In winter, the rising limb of the hydrograph was accompanied by a decrease in temperature, and the falling limb was associated with a corresponding temperature increase. In summer, the trends were reversed. These data suggest that the water temperature changes are causedby the fastest component of drainage runoff, water from a precipitation event or snowmelt, which can be separated from the remainder of the hydrograph. Measurements of hydraulic conductivity, soil moisture content, soil temperature, and g

Druh

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

CEP obor

DA - Hydrologie a limnologie

OECD FORD obor

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Projekt

<a href="/cs/project/QH82095" target="_blank" >QH82095: Vliv rozmístění druhů pozemků v povodí na odtok a odnos vybraných látek</a><br>

Návaznosti

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Rok uplatnění

2011

Kód důvěrnosti údajů

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

Název periodika

Hydrological Processes (print)

ISSN

0885-6087

e-ISSN

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Svazek periodika

25

Číslo periodika v rámci svazku

20

Stát vydavatele periodika

US - Spojené státy americké

Počet stran výsledku

12

Strana od-do

3204-3215

Kód UT WoS článku

000296276000008

EID výsledku v databázi Scopus

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