Report on Modelling Hillslope Scale Preferential Flow and Solute Transport
Result description
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.
Keywords
preferential flowhillslopedual-continuum modeloxygen isotopeRichards' equation
The result's identifiers
Result code in IS VaVaI
Result on the web
—
DOI - Digital Object Identifier
—
Alternative languages
Result language
angličtina
Original language name
Report on Modelling Hillslope Scale Preferential Flow and Solute Transport
Original language description
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.
Czech name
—
Czech description
—
Classification
Type
O - Miscellaneous
CEP classification
DA - Hydrology and limnology
OECD FORD branch
—
Result continuities
Project
—
Continuities
R - Projekt Ramcoveho programu EK
Others
Publication year
2009
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Basic information
Result type
O - Miscellaneous
CEP
DA - Hydrology and limnology
Year of implementation
2009