Effects of asperity distribution on fluid flow and induced seismicity during deep geothermal exploitation


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Date

2016-11

Publication Type

Conference Paper

ETH Bibliography

yes

Citations

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Data

Abstract

This work investigates the injection-induced seismic response of a heterogeneous fault plane, featuring low-permeability asperities embedded into a high-permeability damage zone. We simulate the pressure evolution with a hydrogeological simulator, accounting for the heterogeneous fault plane. Seismicity occurs then on the asperities, represented as unstable patches reactivating by means of the Mohr-Coulomb criterion. The hydrological and seismic modules are implicitly coupled to account for effects of asperity reactivation on the permeability. Results show that permeability changes may cause at a later time a change in seismicity propagation. We also investigated such effects by varying the density of asperities.

Publication status

published

Book title

European Geosciences Union General Assembly 2016, EGU Division Energy, Resources & the Environment (ERE)

Volume

97

Pages / Article No.

470 - 477

Publisher

Elsevier

Event

EGU General Assembly 2016

Edition / version

Methods

Software

Geographic location

Date collected

Date created

Subject

Induced seismicity; Permeability changes; Asperities; Deep geothermal system

Organisational unit

02818 - Schweiz. Erdbebendienst (SED) / Swiss Seismological Service (SED) check_circle

Notes

Funding

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