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The effect of fluid compressibility and elastic rock properties on deformation of geothermal reservoirs

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Academic year: 2019

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Figure

Figure 1. Schematic figure showing subsidence due to the extraction of pore fluids. Deformation of the flat subsurface reservoir leads to measurable surfacedisplacements
Figure 2. Downsampled line-of-sight InSAR (a) and horizontal GNSS (d) data of Hengill 2012–2015 after correcting for plate motion (see Juncu et al
Table 1. Parameters of water, steam and rock on the vapour–liquid satura-tion curve at average temperatures for the Hellisheidi, Reykjanes and TheGeysers geothermal fields
Figure 5. Bivariate histograms for K and χ for a pure liquid phase pore fluid in the Reykjanes reservoir (Keiding et al
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