Water infiltration in Model Sandy Substrate with Various Levels of Rooting

Result code in 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>

Result on the web

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DOI - Digital Object Identifier

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Result language

angličtina

Original language name

Water infiltration in Model Sandy Substrate with Various Levels of Rooting

Original language description

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.

Czech name

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Czech description

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Type

J_x - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)

CEP classification

DA - Hydrology and limnology

OECD FORD branch

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Project

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Continuities

S - Specificky vyzkum na vysokych skolach

Publication year

2013

Confidentiality

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

Name of the periodical

Journal of Landscape Management

ISSN

1804-2821

e-ISSN

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Volume of the periodical

3

Issue of the periodical within the volume

2

Country of publishing house

CZ - CZECH REPUBLIC

Number of pages

6

Pages from-to

31-36

UT code for WoS article

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EID of the result in the Scopus database

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