Cesty proudění vody v horském povodí sledované izotopem kyslíku-18

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68407700%3A21110%2F07%3A01139127" target="_blank" >RIV/68407700:21110/07:01139127 - 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 Flowpaths in the Mountainous Watershed Traced by 18-oxygen Isotope

Popis výsledku v původním jazyce

Uhlirska, Jizera Mountains, Czech Republic, is a typical watershed with the crystalline bedrock forming Cambisols. It is situated in a humid mountainous region where soils are shallow and highly permeable with preferential pathways. As a result of thesefacts, outflow caused by storms can be of a quick response and high magnitude. Based on the observations performed since 1998, it becomes evident that soil profile plays dominant role in the rainfall-runoff transformation. Data collection of the water regime in the soil profile and the subsurface flow accompanied with the standard climatic and hydrological monitoring is performed. Due to the fact that the behavior of flow of water in the heterogeneous soil profile and hydrogeological structure is not fully understood, quantitative measurements are supplemented by the additional techniques of the tracing of stable oxygen isotope 18O and silica since 2006 in rainfall, outflow and soil and groundwater.

Název v anglickém jazyce

Water Flowpaths in the Mountainous Watershed Traced by 18-oxygen Isotope

Popis výsledku anglicky

Uhlirska, Jizera Mountains, Czech Republic, is a typical watershed with the crystalline bedrock forming Cambisols. It is situated in a humid mountainous region where soils are shallow and highly permeable with preferential pathways. As a result of thesefacts, outflow caused by storms can be of a quick response and high magnitude. Based on the observations performed since 1998, it becomes evident that soil profile plays dominant role in the rainfall-runoff transformation. Data collection of the water regime in the soil profile and the subsurface flow accompanied with the standard climatic and hydrological monitoring is performed. Due to the fact that the behavior of flow of water in the heterogeneous soil profile and hydrogeological structure is not fully understood, quantitative measurements are supplemented by the additional techniques of the tracing of stable oxygen isotope 18O and silica since 2006 in rainfall, outflow and soil and groundwater.

Druh

D - Stať ve sborníku

CEP obor

DA - Hydrologie a limnologie

OECD FORD obor

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Projekt

<a href="/cs/project/GA205%2F06%2F0375" target="_blank" >GA205/06/0375: Sledování cest proudění vody v půdním profilu horského povodí pomocí přirozených stopovačů</a><br>

Návaznosti

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Rok uplatnění

2007

Kód důvěrnosti údajů

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

Název statě ve sborníku

Advances in Isotope Hydrology and its Role in Sustainable Water Resources Management (IHS-2007)

ISBN

978-92-0-110207-2

ISSN

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e-ISSN

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Počet stran výsledku

7

Strana od-do

419-425

Název nakladatele

IAEA

Místo vydání

Wien

Místo konání akce

Vienna

Datum konání akce

21. 5. 2007

Typ akce podle státní příslušnosti

WRD - Celosvětová akce

Kód UT WoS článku

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