Using Oxygen-18 to Study the Role of Preferential Flow in the Formation of Hillslope Runoff
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68407700%3A21110%2F10%3A00168050" target="_blank" >RIV/68407700:21110/10:00168050 - isvavai.cz</a>
Result on the web
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DOI - Digital Object Identifier
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Alternative languages
Result language
angličtina
Original language name
Using Oxygen-18 to Study the Role of Preferential Flow in the Formation of Hillslope Runoff
Original language description
The oxygen-18 isotope, monitored in precipitation, subsurface hillslope discharge, and soil water, was used as a natural tracer to study the role of preferential flow in the formation of shallow subsurface runoff. The dual-continuum model of soil water flow was successfully applied to explain the observed variations of oxygen-18 in the hillslope discharge.
Czech name
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Czech description
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Classification
Type
J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)
CEP classification
DA - Hydrology and limnology
OECD FORD branch
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Result continuities
Project
Result was created during the realization of more than one project. More information in the Projects tab.
Continuities
R - Projekt Ramcoveho programu EK
Others
Publication year
2010
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Vadose Zone Journal
ISSN
1539-1663
e-ISSN
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Volume of the periodical
9
Issue of the periodical within the volume
2
Country of publishing house
US - UNITED STATES
Number of pages
8
Pages from-to
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UT code for WoS article
000277718000005
EID of the result in the Scopus database
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