Directory UMM :Data Elmu:jurnal:A:Advances In Water Resources:Vol22.Issue8.1999:
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This was because the actual velocity was greater near the soil surface than in the deep soil Ð due to the better soil structure and low water content in the shallow soil Ð and
Afterwards a calibration of hydraulic parameters was performed using measured water and bromide contents in soil (Weiherbach, Vredepeel and Brimstone) or leachate (Tor Mancina)..
In this paper, a variational data assimilation procedure for initialization of a cloud model using radar re¯ectivity and radial velocity observations and its impact on short
The original dual formulation for construction of streamline-oriented grids was restricted to isotropic hydraulic conductivity ®elds in two-dimensional do- mains without
The algorithm involves (1) limited stretching or shrinking of elements along the water table if the change in the position of the water table is small with respect to the vertical
In this paper we analyze a model for brine transport in porous media, which includes a mass balance for the fluid, a mass balance for salt, Darcy’s law and an equation of state,
(From left to right:) Variance of head, unsaturated hydraulic conductivity, horizontal flux, and vertical flux as functions of (from top to bottom:) soil textural variability
Firstly, to derive closed solutions of the flow equation at very large length scale, i.e., to derive the velocity field, the flow pattern and the residence time of a fluid particle,