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For modelling the water fluxes through the vadose zone, it is necessary to know the soil hydraulic properties. Because many of the soil parameters cannot be measured directly in the field, inverse modeling methods are used to find the most appropriate solution. For a limited number of parameters, the minimization approach provided by Marquardt-Levenberg (ML) has become a usual technique in nonlinear least-squares fitting in soil and hydrological studies. Classical gradient-based methods find the solution in the ne...

An accurate simulation of snowmelt infiltration rates for an area of Bucegi Mountains, during spring thaw, has been made using the snow routine of HYDRUS- 1D. The model is based on coupled flow and heat transport in the vadose zone. The snowmelt routine is based on degree day concept. As boundary conditions are used, surface water and heat fluxes can be calculated from the energy balance equation. The variables of the surface energy balance equation and melt rates can be calculated using meteorological data: air t...