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

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CHAPTER 5. JOINTLY MAPPING HYDRAULIC . . . 127<br />

250<br />

North<br />

S1: variance <strong>of</strong> concentration<br />

.0<br />

.0 East<br />

250<br />

S3: variance <strong>of</strong> concentration<br />

250<br />

North<br />

.0<br />

.0 East<br />

250<br />

S5: variance <strong>of</strong> concentration<br />

250<br />

North<br />

.0<br />

.0 East<br />

250<br />

3.0<br />

2.0<br />

1.0<br />

.0<br />

3.0<br />

2.0<br />

1.0<br />

0.0<br />

3.0<br />

2.0<br />

1.0<br />

0.0<br />

250<br />

North<br />

S2: variance <strong>of</strong> concentration<br />

.0<br />

.0 East<br />

250<br />

S4: variance <strong>of</strong> concentration<br />

250<br />

North<br />

.0<br />

.0 East<br />

250<br />

S6: variance <strong>of</strong> concentration<br />

250<br />

.0<br />

.0 East<br />

250<br />

Figure 5.10: Ensemble variance <strong>of</strong> concentration fields at t = 300 day for the<br />

different scenarios.<br />

North<br />

3.0<br />

2.0<br />

1.0<br />

0.0<br />

3.0<br />

2.0<br />

1.0<br />

0.0<br />

3.0<br />

2.0<br />

1.0<br />

0.0

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