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This example illustrates the use of the program for the case where one of the layers are fractured and there is and sorption of the contaminant species. The “barrier” consists of a 1 m thick compacted clay layer overlying a 3 m thick fractured till. A reactive species (i.e., one that will sorb on to the clay) is modelled in this case. The same finite mass source and leachate collection system is used as in the previous examples. A Darcy velocity (va) of 0.02 m/a through the deposit and an infiltration through the cover (qo) of 0.3 m/a are assumed. The Volume of Leachate Collected (Qc) is then given by:
Qc = qo - va = 0.3 - 0.02 = 0.28 m/a
As in the previous examples the inflow in the aquifer at the up gradient edge of the landfill is 4 m/a. The outflow (vb) at the down gradient edge of the landfill is then:
vb = 4 + 200*0.02 = 8 m/a
The following parameters are defined for this example:
Property |
Symbol |
Value |
Units |
Darcy Velocity |
va |
0.02 |
m/a |
Diffusion Coefficient |
D |
0.01 |
m2/a |
Distribution Coefficient |
Kd |
1.5 |
cm3/g |
Soil Porosity |
n |
0.4 |
- |
Dry Density |
|
2 |
g/cm3 |
Soil Liner Thickness |
HL |
1 |
m |
Number of Sub-layers |
|
1 |
- |
Fractured Till Thickness |
HT |
3 |
m |
Number of Sub-layers |
|
1 |
- |
Fracture spacing in x direction |
2H1 |
1 |
m |
Fracture opening in x |
2h1 |
10 |
µm |
Fracture spacing in y direction |
2H2 |
1 |
m |
Fracture opening in y |
2h2 |
10 |
µm |
Dispersion along fractures |
Df |
0.06 |
m2/a |
Fracture Distribution Coefficient |
Kf |
0 |
cm3/g |
Matrix Diffusion Coefficient |
Dm |
0.01 |
m2/a |
Matrix Distribution Coefficient |
Km |
1.5 |
cm3/g |
Matrix Porosity |
nm |
0.4 |
- |
Dry Density of Matrix |
|
2 |
g/cm3 |
Source Concentration |
co |
1000 |
mg/L |
Rate of Increase in co |
cr |
0 |
mg/L/a |
Ref. Height of Leachate |
Hr |
7.5 |
m |
Volume Collected |
Qc |
0.28 |
m/a |
Landfill Length |
L |
200 |
m |
Landfill Width |
W |
1 |
m |
Thickness of Aquifer |
h |
1 |
m |
Porosity of Aquifer |
nb |
0.35 |
|
Base Outflow Velocity |
vb |
8 |
m/a |
Lower and Upper Time Limits |
|
20, 300 |
a |