Pure and Applied Geophysics

, Volume 166, Issue 5, pp 1107–1123

Impact of Poroelastic Response of Sandstones on Geothermal Power Production

  • Guido Blöcher
  • Günter Zimmermann
  • Harald Milsch
Article

DOI: 10.1007/s00024-009-0475-4

Cite this article as:
Blöcher, G., Zimmermann, G. & Milsch, H. Pure appl. geophys. (2009) 166: 1107. doi:10.1007/s00024-009-0475-4

Abstract

During geothermal power production using a borehole doublet consisting of a production and injection well, the reservoir conditions such as permeability k, porosity φ and Skempton coefficient B at the geothermal research site Gross Schoenebeck/Germany will change. Besides a temperature decrease at the injection well and a change of the chemical equilibrium, also the pore pressure pp will vary in a range of approximately 44 MPa ± 10 MPa in our reservoir at −3850 to −4258 m depth. This leads to a poroelastic response of the reservoir rocks depending on effective pressure peff (difference between mean stress and pore pressure), resulting in a change in permeability k, porosity φ and the poroelastic parameter Skempton coefficient B. Hence, we investigated the effective pressure dependency of Flechtinger sandstone, an outcropping equivalent of the reservoir rock via laboratory experiments. The permeability decreased by 21% at an effective pressure range from 3 to 30 MPa, the porosity decreased by 11% (peff = 6 to 65 MPa) and the Skempton coefficient decreased by 24% (peff = 4 to 25 MPa). We will show which mechanisms lead to the change of the mentioned hydraulic and poroelastic parameters and the influence of these changes on the productivity of the reservoir. The most significant changes occur at low effective pressures until 15 to 20 MPa. For our in situ reservoir conditions peff = 43 MPa a change of 10 MPa effective pressure will result in a change in matrix permeability of less than 4% and in matrix porosity of less than 2%. Besides natural fracture systems, fault zones and induced hydraulic fractures, the rock matrix its only one part of geothermal systems. All components can be influenced by pressure, temperature and chemical reactions. Therefore, the determined small poroelastic response of rock matrix does not significantly influence the sustainability of the geothermal reservoir.

Keywords

Porosity permeability Skempton coefficient poroelasticity sandstone 

Copyright information

© Birkhäuser Verlag, Basel 2009

Authors and Affiliations

  • Guido Blöcher
    • 1
  • Günter Zimmermann
    • 1
  • Harald Milsch
    • 1
  1. 1.Helmholtz Centre PotsdamGFZ German Research Centre for GeosciencesPotsdamGermany

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