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Fig. 10 | Geothermal Energy

Fig. 10

From: Hydraulic behavior of fault zones in pump tests of geothermal wells: a parametric analysis using numerical simulations for the Upper Jurassic aquifer of the North Alpine Foreland Basin

Fig. 10

Regression results for characteristic parameter combinations for the three observed flow regime transitions (1: radial to bilinear, 2: bilinear to linear, 3: linear to negative boundary); left: 50 m fault zone thickness; right: 150 m fault zone thickness; subplots have fixed specific matrix storage values; specific fault zone storage color-coded; line styles represent the flow regime transitions; parameter combinations that fall on the transition line should be seen as combinations for which the flow regime above has still been observed

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