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Fig. 3 | Geothermal Energy

Fig. 3

From: Influence of extreme fracture flow channels on the thermal performance of open-loop geothermal systems at commercial scale

Fig. 3

Upscaled permeability distribution from Altona for a synthetic circular region of 500 m of radius. The permeability distribution was rescaled using a renormalization technique for the x and y coordinates (\(dx\to k\cdot dx\), \(dy\to k\cdot dy)\) where k is 42.55. Permeability is expressed in m2 units. Orientation of the fracture was shifted so due North is aligned with the positive y-axis

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