Directory UMM :Data Elmu:jurnal:A:Advances In Water Resources:Vol23.Issue4.2000:
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We focused on two kinds of variables given as output by the CERES-Maize model; (a) final simulations of biomass, grain yield, yield components, maximum LAI and
Time series of the shore-parallel velocity component at the four near-shore midpoints, counterclockwise around the basin (western (a), southern (b), eastern (c) and northern shore
Application of the method to the characterization of the structure of an outcrop Grey- Vosgues sandstone (sample GV-1) indicated that the simultaneous prediction of capillary
However, in unsteady ¯ow, with signi®cant temporal variations in the velocity ®eld in both magni- tude and direction, the element-based algorithm pro- duces large tracking errors with
This example was used to test the accuracy and ro- bustness of the HLTFEM for simulating transport in a two-dimensional aquifer under one-dimensional con- stant groundwater
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
Again, since each conditional realization of f and h fields, derived from Approach II, satisfies the governing flow equation, these realizations yield mass-conservative velocity
Firstly, to derive closed solutions of the flow equation at very large length scale, i.e., to derive the velocity field, the flow pattern and the residence time of a fluid particle,
