Upscaling and Inverse Modeling of Groundwater Flow and Mass ...

160 CHAPTER 6. GROUNDWATER FLOW INVERSE MODELING . . .
Unconditional
Parallel flow
Non Localized
Parallel flow
Localized
Radial flow
Non Localized
Radial flow
Localized
Conncectivity Function
1
0.8
0.6
0.4
0.2
Scenario 1/7
Correct Prior Wrong Prior
0
0 50 100 150
Lag [m]
200 250 300
Conncectivity Function
1
0.8
0.6
0.4
0.2
Scenario 2/8
0
0 50 100 150
Lag [m]
200 250 300
Figure 6.8: Connectivity function of logconductivity fields at time step
nT = 60 for the different scenarios. Gray curves correspond to individual
realizations, their mean is given by the triangles and the circles correspond to
the reference.