Figure 5 | Scientific Reports

Figure 5

From: A quantitative analysis of hydraulic interaction processes in stream-aquifer systems

Figure 5

The time-variation of the vertical hydraulic gradient at the free water surface of regional water table on the symmetrical line from the critical disconnection to entire disconnection (a), the relationship between the maximum thickness of inverted water table zone below streambed and the water depth in stream at steady state for entire disconnection observed by the laboratory sandbox experiment (b) and by the finite analytic numerical method (c).

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