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- W1994011333 abstract "Tracer experiment was carried out using a packed bed of fine sand, where groundwater flowed as a single phase under unsaturated conditions. A new apparatus with the new evaporation technique proposed by Mohamed et al. was used to create an upward movement (i. e. upward soil water potential gradient) to estimate the hydrodynamic dispersion coefficient (D) The concentration distribution of the sodium chloride (NaCl) over the depth of the sand column at the end of the experiment could be measured using the electrical potential method. D could be determined by fitting an appropriate numerical solution of onedimensional Convection Dispersion Equation (CDE) to the measured vertical solute concentration through the depth of the unsaturated sand at the end of the experiment using Galerkin Finite Element Method (GFEM). A good agreement was found between the two series. The value of the estimated dispersivity is quite accurate and lies in the range 0.001-0.02m which is suggested by many authors." @default.
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- W1994011333 date "2000-01-01" @default.
- W1994011333 modified "2023-10-06" @default.
- W1994011333 title "DISPERSION COEFFICIENT IN UNSATURATED SOIL EXPOSED TO EVAPORATION" @default.
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- W1994011333 doi "https://doi.org/10.2208/prohe.44.211" @default.
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