Hillslope Hydrograph Analysis Using Synthetic and Natural Oxygen-18 Signatures
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68407700%3A21110%2F12%3A00200752" target="_blank" >RIV/68407700:21110/12:00200752 - isvavai.cz</a>
Result on the web
<a href="http://dx.doi.org/10.1016/j.jhydrol.2012.10.025" target="_blank" >http://dx.doi.org/10.1016/j.jhydrol.2012.10.025</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1016/j.jhydrol.2012.10.025" target="_blank" >10.1016/j.jhydrol.2012.10.025</a>
Alternative languages
Result language
angličtina
Original language name
Hillslope Hydrograph Analysis Using Synthetic and Natural Oxygen-18 Signatures
Original language description
Shallow subsurface runoff is one of the most important mechanisms determining hydrological responses of headwater catchments to rainstorms. In this study, a simplified approach combining one-dimensional dual-continuum vertical flow in a variably saturated soil profile and one-dimensional saturated flow along the soil-bedrock interface was used to study rainfall-runoff events at an experimental hillslope. A dual set of Richards' equations was used to predict vertical flow of water in the soil matrix andpreferential pathways. Subsurface flow along the soil-bedrock interface was described by diffusion wave equation. The observed subsurface runoff and its oxygen-18 composition were compared with the model predictions. Contributions of pre-event and eventwater to hillslope runoff during major rainfall-runoff episodes were evaluated by means of numerical experiments involving synthetic oxygen-18 rainfall signatures. Although preferential flow played an important role in the hillslope runof
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
<a href="/en/project/GA205%2F08%2F1174" target="_blank" >GA205/08/1174: Hydrological fluxes in soil-plant-atmosphere system</a><br>
Continuities
Z - Vyzkumny zamer (s odkazem do CEZ)
Others
Publication year
2012
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Journal of Hydrology
ISSN
0022-1694
e-ISSN
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Volume of the periodical
475
Issue of the periodical within the volume
December
Country of publishing house
NL - THE KINGDOM OF THE NETHERLANDS
Number of pages
13
Pages from-to
415-427
UT code for WoS article
000313864200034
EID of the result in the Scopus database
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