Report on Modelling Hillslope Scale Preferential Flow and Solute Transport

Kód výsledku v IS VaVaI

RIV/68407700:21110/09:00159917 - isvavai.cz

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Report on Modelling Hillslope Scale Preferential Flow and Solute Transport

Popis výsledku v původním jazyce

Soil water dynamics at the experimental hillslope site is studied by means of one-dimensional dual-continuum model based on Richards' equation for vertical soil water flow and advection-dispersion equation for vertical solute transport. Stable oxygen isotope 18O, monitored at the recharge as well as discharge face of the hillslope site, is used as natural tracer. The dual-continuum approach makes it possible to analyze in detail preferential flow effects in the soil of interest during vegetation season.

Název v anglickém jazyce

Report on Modelling Hillslope Scale Preferential Flow and Solute Transport

Popis výsledku anglicky

Soil water dynamics at the experimental hillslope site is studied by means of one-dimensional dual-continuum model based on Richards' equation for vertical soil water flow and advection-dispersion equation for vertical solute transport. Stable oxygen isotope 18O, monitored at the recharge as well as discharge face of the hillslope site, is used as natural tracer. The dual-continuum approach makes it possible to analyze in detail preferential flow effects in the soil of interest during vegetation season.

Druh

O - Ostatní výsledky

CEP obor

DA - Hydrologie a limnologie

OECD FORD obor

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Projekt

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Návaznosti

R - Projekt Ramcoveho programu EK

Rok uplatnění

2009

Kód důvěrnosti údajů

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