Fluid pressure drops during stimulation of segmented faults in deep geothermal reservoirs

Abstract Hydraulic stimulation treatments required to produce deep geothermal reservoirs present the risk of generating induced seismicity. Understanding the processes that operate during the stimulation phase is critical for minimising and preventing the uncertainties associated with the exploitati...

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Main Authors: Guillem Piris, Albert Griera, Enrique Gomez-Rivas, Ignasi Herms, Mark W. McClure, Jack H. Norbeck
Format: Article
Language:English
Published: SpringerOpen 2018-11-01
Series:Geothermal Energy
Subjects:
Online Access:http://link.springer.com/article/10.1186/s40517-018-0110-7
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author Guillem Piris
Albert Griera
Enrique Gomez-Rivas
Ignasi Herms
Mark W. McClure
Jack H. Norbeck
author_facet Guillem Piris
Albert Griera
Enrique Gomez-Rivas
Ignasi Herms
Mark W. McClure
Jack H. Norbeck
author_sort Guillem Piris
collection DOAJ
description Abstract Hydraulic stimulation treatments required to produce deep geothermal reservoirs present the risk of generating induced seismicity. Understanding the processes that operate during the stimulation phase is critical for minimising and preventing the uncertainties associated with the exploitation of these reservoirs. It is especially important to understand how the phenomenon of induced seismicity is related to the pressurisation of networks of discrete fractures. In this study, we use the numerical simulator CFRAC to analyse pressure drops commonly observed during stimulation of deep geothermal wells. We develop a conceptual model of a fractured geothermal reservoir to analyse the conditions required to produce pressure drops and their consequences on the evolution of seismicity, fluid pressure, and fracture permeability throughout the system. For this, we combine two fracture sets, one able to be stimulated by shear-mode fracturing and another one able to be stimulated by opening-mode fracturing. With this combination, the pressure drop can be triggered by a seismic event in the shear-stimulated fracture that is hydraulically connected with an opening-mode fracture. Our results indicate that pressure drops are not produced by the new volume created by shear dilatancy, but by the opening of the conjugated tensile fractures. Finally, our results reveal that natural fracture/splay fracture interaction can potentially explain the observed pressure drops at the Rittershoffen geothermal site.
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spelling doaj.art-a438d2718e9b45cb9725cc3f795c269e2022-12-22T01:26:45ZengSpringerOpenGeothermal Energy2195-97062018-11-016112110.1186/s40517-018-0110-7Fluid pressure drops during stimulation of segmented faults in deep geothermal reservoirsGuillem Piris0Albert Griera1Enrique Gomez-Rivas2Ignasi Herms3Mark W. McClure4Jack H. Norbeck5Departament de Geologia, Universitat Autònoma de BarcelonaDepartament de Geologia, Universitat Autònoma de BarcelonaDepartament de Mineralogía, Petrología i Geología Aplicada, Universitat de BarcelonaInstitut Cartogràfic i Geològic de Catalunya (ICGC)ResFrac CorporationDepartment of Energy Resources Engineering, Stanford UniversityAbstract Hydraulic stimulation treatments required to produce deep geothermal reservoirs present the risk of generating induced seismicity. Understanding the processes that operate during the stimulation phase is critical for minimising and preventing the uncertainties associated with the exploitation of these reservoirs. It is especially important to understand how the phenomenon of induced seismicity is related to the pressurisation of networks of discrete fractures. In this study, we use the numerical simulator CFRAC to analyse pressure drops commonly observed during stimulation of deep geothermal wells. We develop a conceptual model of a fractured geothermal reservoir to analyse the conditions required to produce pressure drops and their consequences on the evolution of seismicity, fluid pressure, and fracture permeability throughout the system. For this, we combine two fracture sets, one able to be stimulated by shear-mode fracturing and another one able to be stimulated by opening-mode fracturing. With this combination, the pressure drop can be triggered by a seismic event in the shear-stimulated fracture that is hydraulically connected with an opening-mode fracture. Our results indicate that pressure drops are not produced by the new volume created by shear dilatancy, but by the opening of the conjugated tensile fractures. Finally, our results reveal that natural fracture/splay fracture interaction can potentially explain the observed pressure drops at the Rittershoffen geothermal site.http://link.springer.com/article/10.1186/s40517-018-0110-7Enhanced geothermal reservoirsPressure dropsReservoir simulationInduced seismicityFracture networks
spellingShingle Guillem Piris
Albert Griera
Enrique Gomez-Rivas
Ignasi Herms
Mark W. McClure
Jack H. Norbeck
Fluid pressure drops during stimulation of segmented faults in deep geothermal reservoirs
Geothermal Energy
Enhanced geothermal reservoirs
Pressure drops
Reservoir simulation
Induced seismicity
Fracture networks
title Fluid pressure drops during stimulation of segmented faults in deep geothermal reservoirs
title_full Fluid pressure drops during stimulation of segmented faults in deep geothermal reservoirs
title_fullStr Fluid pressure drops during stimulation of segmented faults in deep geothermal reservoirs
title_full_unstemmed Fluid pressure drops during stimulation of segmented faults in deep geothermal reservoirs
title_short Fluid pressure drops during stimulation of segmented faults in deep geothermal reservoirs
title_sort fluid pressure drops during stimulation of segmented faults in deep geothermal reservoirs
topic Enhanced geothermal reservoirs
Pressure drops
Reservoir simulation
Induced seismicity
Fracture networks
url http://link.springer.com/article/10.1186/s40517-018-0110-7
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