Directory UMM :Data Elmu:jurnal:A:Advances In Water Resources:Vol23.Issue6.2000:
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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
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 developing the method for representing wells in ®nite dierence models for variably saturated air and water ¯ow, it is assumed that any water entering the well accumulates at
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
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
In this paper, we present the methods we used to create DTMs and topographic maps of small, headwater stream channels using a total station.. We also recom- mend ways to use the
