Water infiltration in Model Sandy Substrate with Various Levels of Rooting

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F62156489%3A43410%2F13%3A00199061" target="_blank" >RIV/62156489:43410/13:00199061 - isvavai.cz</a>

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Water infiltration in Model Sandy Substrate with Various Levels of Rooting

Popis výsledku v původním jazyce

Water infiltration in soil and saturated hydraulic conductivity represent key factors in water runoff formation. Significant volumes of precipitations infiltrate and run off under the soil surface. The water that does not seep in the soil moves on the surface, which we define as Horton overland flow. Infiltration is decisive for the rate of this flow (e.g. Corradini et al., 1998). It is influenced by a number of factors, among which most authors also mention the contents of soil organic matter (SOM), both dead and living. For example, Franzluebbers (2002) points out that the mere SOM contents is not the only influence but that it is rather horizontal distribution of SOM in the surface soil layer.

Název v anglickém jazyce

Water infiltration in Model Sandy Substrate with Various Levels of Rooting

Popis výsledku anglicky

Water infiltration in soil and saturated hydraulic conductivity represent key factors in water runoff formation. Significant volumes of precipitations infiltrate and run off under the soil surface. The water that does not seep in the soil moves on the surface, which we define as Horton overland flow. Infiltration is decisive for the rate of this flow (e.g. Corradini et al., 1998). It is influenced by a number of factors, among which most authors also mention the contents of soil organic matter (SOM), both dead and living. For example, Franzluebbers (2002) points out that the mere SOM contents is not the only influence but that it is rather horizontal distribution of SOM in the surface soil layer.

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

S - Specificky vyzkum na vysokych skolach

Rok uplatnění

2013

Kód důvěrnosti údajů

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

Název periodika

Journal of Landscape Management

ISSN

1804-2821

e-ISSN

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Svazek periodika

3

Číslo periodika v rámci svazku

2

Stát vydavatele periodika

CZ - Česká republika

Počet stran výsledku

6

Strana od-do

31-36

Kód UT WoS článku

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EID výsledku v databázi Scopus

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