Report on Modelling Hillslope Scale Preferential Flow and Solute Transport

Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68407700%3A21110%2F09%3A00159917" target="_blank" >RIV/68407700:21110/09:00159917 - 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
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.

Rok uplatnění
2009
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

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