Directory UMM :Data Elmu:jurnal:A:Advances In Water Resources:Vol23.Issue8.2000:
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The plants were garden weeds and collected in # ower near Aberystwyth (Tyn-y-Graig, Wales), and a voucher specimen (N9623) of this collection has been retained in the herbarium at
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 solution process is as follows: (i) move the masslets in a Lagrangian manner according to the ¯ow velocity components, (ii) create a re®ned hierarchical grid about the
In order to address this problem in the use of 30- arc-second DEM, we adopt the following procedure: (i) estimate topographic index using the single ¯ow algorithm from the
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..
