Directory UMM :Data Elmu:jurnal:A:Advances In Water Resources:Vol23.Issue4.2000:
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It was found that using measured values to initialize the aerosol optical depth in the retrieval of surface global irradiance, the sur- face albedo increased by about 0.02 on
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
Selection of a weighting scheme becomes more critical when dealing with the coupled processes of multiphase ¯ow, tracer transport, and heat transfer in a fractured medium, because
First the con- vection of a square wave in a uniform ¯ow was studied, then the advective±diusion of an initial square column concentration distribution was investigated to show
The physics of the problem dictate that the eect of the boundary is felt by its adjacent grid node in the ®rst few time steps, after which the ¯ow conditions remains un- altered
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..
Using simple kinematic relations nonmonotonic saturation–depth profiles travelling both in 1D case and in 2D finger-type flows are interpreted as a consequence of hysteresis
