Prediction of Occurrence of Discrete Events - Geomathematics: Theoretical Foundations, Applications and Future Developments - page 157

600000 620000 640000 660000 680000 700000 720000 740000

4880000 4880000

4860000 4860000

Spring
High Slope (>8)
<8
>=8
Distances to High_Slope Zone

Spatial Correlation

0 574.058

574.058

−

8 1148.116

−

1148.116 − 1722.174

1722.174 − 2296.231

4 2296.231 − 2870.289

4840000 4840000

2870.289 − 3444.347

3444.347 − 4018.405

0

4018.405 4592.463

4592.463 − 5166.521
5166.521

−

− 5740.578

− 4

5740.578 − 6314.636

6314.636 − 6888.694

6888.694 − 7462.752

− 8

4820000 4820000

0 2000 4000 6000 8000

Distance

600000 620000 640000 660000 680000 700000 720000 740000

Fig. 5.16 Flowing wells versus distance from relatively steep slope zone in study area shown in Fig. 5.13 (Courtesy of Q. Cheng)