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Figure 15 | Geothermal Energy

Figure 15

From: Two-dimensional THM modelling of the large scale natural hydrothermal circulation at Soultz-sous-Forêts

Figure 15

Vertical profiles of total stress (MPa). σ h and σ v are the horizontal and vertical total stress in the plane of the model (i.e. σ xx and σ yy , respectively), σ hv is the associated shear stress (i.e. σ xy ), σ h is the horizontal total stress perpendicular to the plane of the model (σ zz ), and σ p is the hydraulic stress. The lithostatic stress σlitho is calculated via the formula σlitho=r0g z, r0 being the total homogenized initial density.

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