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Fig. 4 | Geothermal Energy

Fig. 4

From: Modelling of flow through naturally fractured geothermal reservoirs, Taupō Volcanic Zone, New Zealand

Fig. 4

Examples of backbone fracture networks. A Model A, P10 = 0.6 m−1 BD: networks close to the percolation threshold (Model I, P10 = 0.2 m−1). B Network not connected across the model domain in either X or Y direction (approximately 65% models). C Strongly channelled network supporting flow only in the Y direction (approximately 35% of models). Each of the four channels is displayed in a different colour. D Network connected across the model in both directions (0.1% of models)

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