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This example illustrates the use of the program for lateral migration of a radioactive contaminant in a fractured porous rock with a single set of parallel fractures. It considers advective-dispersive transport along the fractures and diffusion into the rock matrix. The deposit is assumed to extend a considerable distance from the source (effectively an infinite distance) but we are only interested here in what happens over the first 50 m after 30 years..
It is assumed that the source concentration, co, is 1 unit and that the half life of the radioactive species is 100 years. The source is considered to have a sufficiently large supply that there is no significant change in source concentration due to mass movement into the rock. However the source does experience radioactive decay.
This example is also being used to illustrate the Maximum Sublayer Thickness Special Feature, for specifying sublayer thicknesses that are greater than 5 units.
The following parameters are defined for this example:
Property |
Symbol |
Value |
Units |
Darcy Velocity |
va |
0.08 |
m/a |
Fractured Rock Thickness |
HT |
50 |
m |
Number of Sub-layers |
|
5 |
- |
Fracture spacing |
2H1 |
0.05 |
m |
Fracture opening |
2h1 |
10 |
µm |
Dispersion along fractures |
Df |
6 |
m2/a |
Fracture Distribution Coefficient |
Kf |
0 |
cm3/g |
Matrix Diffusion Coefficient |
Dm |
0.0018 |
m2/a |
Matrix Distribution Coefficient |
Km |
0 |
cm3/g |
Matrix Porosity |
nm |
0.05 |
- |
Dry Density of Matrix |
|
2 |
g/cm3 |
Source Concentration |
co |
1 |
|
Half life of contaminant |
|
100 |
a |
Time period of interest |
|
30 |
a |