Assessment of Frequency and Areal Extent of Overland Flow Generation in a Forested Mountain Catchment

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68407700%3A21110%2F11%3A00189497" target="_blank" >RIV/68407700:21110/11:00189497 - isvavai.cz</a>

Výsledek na webu

<a href="http://www.agriculturejournals.cz/publicFiles/35841.pdf" target="_blank" >http://www.agriculturejournals.cz/publicFiles/35841.pdf</a>

DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Assessment of Frequency and Areal Extent of Overland Flow Generation in a Forested Mountain Catchment

Popis výsledku v původním jazyce

Short time rainfall and throughfall measurements in the period May-October 2009, and the calculated saturated hydraulic conductivities of soils and isotopic hydrograph separations in August 2009 were used to estimate the frequency of the infiltration excess overland flow generation and the extent of saturated areas producing the saturation excess overland flow in the forested mountain catchment of the Jalovecký Creek, Western Tatra Mountains, northern Slovakia. The rainfall intensities exceeding 0.2 mmper 10 min occured only in 2-4% of all data measured. Saturated hydraulic conductivities (KS) of soils were calculated by means of four methods based on the relationship between KS and soil texture. The comparison of KS with the measured rainfall intensities indicated that the infiltration excess overland flow could have been generated for 0-10% of the rainfall intensities measured.

Název v anglickém jazyce

Assessment of Frequency and Areal Extent of Overland Flow Generation in a Forested Mountain Catchment

Popis výsledku anglicky

Short time rainfall and throughfall measurements in the period May-October 2009, and the calculated saturated hydraulic conductivities of soils and isotopic hydrograph separations in August 2009 were used to estimate the frequency of the infiltration excess overland flow generation and the extent of saturated areas producing the saturation excess overland flow in the forested mountain catchment of the Jalovecký Creek, Western Tatra Mountains, northern Slovakia. The rainfall intensities exceeding 0.2 mmper 10 min occured only in 2-4% of all data measured. Saturated hydraulic conductivities (KS) of soils were calculated by means of four methods based on the relationship between KS and soil texture. The comparison of KS with the measured rainfall intensities indicated that the infiltration excess overland flow could have been generated for 0-10% of the rainfall intensities measured.

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

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Návaznosti

Z - Vyzkumny zamer (s odkazem do CEZ)

Rok uplatnění

2011

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

2011 (1)

Číslo periodika v rámci svazku

6

Stát vydavatele periodika

CZ - Česká republika

Počet stran výsledku

11

Strana od-do

43-53

Kód UT WoS článku

000305504800005

EID výsledku v databázi Scopus

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