Directory UMM :Data Elmu:jurnal:A:Advances In Water Resources:Vol23.Issue8.2000:
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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
Referring to the governing equations for the porous ¯ow, (3)±(5), the major dierences between the present dynamic model and previous quasi-static model are the pore ¯uid and
We propose that the concept of physical geometry as a spatiotemporal continuum with properties that are empirically de®ned is im- portant in hydrologic analyses, and that the
Since explicit ®nite dierence formulations directly compute the ¯ow variables at the new time level from the known initial conditions, implementing a standard multigrid
The inverse problem to estimate the coecients in the convection diusion equation which is assumed to govern the air-mixed ¯ow in a hydraulic jump is for- mulated as the
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
For fBm media, this size dependence can be explained using an eective variance that increases with increasing size of the ¯ow system.. However, the magnitudes of the
The constant ¯ow rate experiments show a signi®- cant reduction of the dispersion coecient in case of an increasing density dierence between the resident and displacing ¯uids..
