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

116 CHAPTER 5. JOINTLY MAPPING HYDRAULIC . . .
250
North
(A) Reference concentration field (t=300)
.0
.0 East
250
250
North
(C) Reference concentration field (t=400)
.0
.0 East
250
250
North
(E) Reference concentration field (t=500)
.0
.0 East
250
2.0
1.5
1.0
0.5
0.0
1.5
0.5
0.0
(B) Concentration Data (t=300) to be Conditioned
250.
200.
150.
100.
50.
0.
0. 50. 100. 150. 200. 250.
(D) Concentration data (t=400) to be Conditioned
250.
200.
1.0 150.
1.5
0.5
0.0
100.
50.
0.
0. 50. 100. 150. 200. 250.
(F) Concentration Data (t=500) to be Conditioned
250.
200.
1.0 150.
100.
0. 50. 100. 150. 200. 250.
Figure 5.3: Reference concentration fields at time 300(A), 400(C) and 500(E)
days. Conditioning concentration data at time 300 (B), 400 (D), and 500 (F)
days.
50.
0.
2.0
1.5
1.0
0.5
0.0
1.5
1.0
0.5
0.0
1.5
1.0
0.5
0.0