Implications of Self-Potential Distribution for Groundwater Flow System in a Nonvolcanic Mountain Slope
Figure 6
Calculated SP from various depths of a point source (1–100 m). The SP values are normalized by the respective value at 0 m in the horizontal distance where the source is located. The observed SP anomalies “A” and “B” in Figure 5(b) are shown by circles and rectangles, respectively.