Directory UMM :Data Elmu:jurnal:A:Advances In Water Resources:Vol23.Issue3.1999:
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In isolation from the data collected during the detailed soil analysis, the initial `end member' data suggested that groundwater and soil water had a different isotopic composition..
In particular, we have examined the relationship between common line length, capillary pressure, and saturation; we have examined the relationship between ¯uid±¯uid interfacial
In this work, we seek to compare the current model predictions for three-phase relative permeabilities in weakly wetted mixed-wet and fractionally wet systems on: (i) the possible
If the log hydraulic conductivity ®eld is a normally distributed random variable and we have measurements of log conductivity and other vari- ables such as hydraulic head, we can
The fact that dependent variables of groundwater models are generally nonlinear functions of model parameters is shown to be a potentially signi®cant factor in calculating
In the following, two dierent cell-centered FVM schemes for two-dimensional modeling of transport will be presented, the ®rst of which is used for calculations on rectangular
solution derived in this work for a point source geometry with constant solute mass release rate is equivalent to the one-dimensional analytical solution for virus transport
The steps of the method are: (1) defining the transmissivity variogram from experimental data and geostatistically simulating a large number of trans- missivity fields; (2)