Directory UMM :Data Elmu:jurnal:A:Advances In Water Resources:Vol21.Issue6.1998:
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Numerical simulations of water ¯ow and solute transport were used to investigate the eect of the recharge (rain/irrigation) at the soil surface on solute spreading and breakthrough
The SIA1FULL code uses the SIA-1 method to solve the reactive transport equations and the direct solution method to solve the reaction parameter sensitivity equations.. The
More speci®cally, the present paper describes how the GITT can be used to derive analytical solutions for solute transport problems in porous media with spatially and
An iterative solution technique for reactive transport problems is developed, which we call the selective coupling method, that represents a versatile alternative to
Large eddy simulations of turbulent ¯ow and transport in the atmospheric boundary layer were conducted over heterogeneous sources of heat and water vapor to identify the
terms are given in order of sequence: the first term represents the mass exchange across the mantle segments forming the boundaries with neighbouring REWs, the second term is the
In this case of high water saturation, where Knudsen diffusion is assumed to be insignificant, the dusty gas model predicts greater flux rates than the Fickian model, as indicated
Numerical diffusion, though, can be partially attributed to the selected ELM: 2 the second moment of solutions with inexact tracking is of the same order of magnitude of the
