3D mechanical analysis of geothermal reservoir operations in faulted sedimentary aquifers using MACRIS

Abstract Accurate and efficient predictions of three-dimensional subsurface stress changes are required for the assessment of geothermal operations with respect to fault stability and the potential risk for induced seismicity. This work extends the model capabilities of Mechanical Analysis of Comple...

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Main Authors: Arjan Marelis, Fred Beekman, Jan-Diederik van Wees
Format: Article
Language:English
Published: SpringerOpen 2024-02-01
Series:Geothermal Energy
Subjects:
Online Access:https://doi.org/10.1186/s40517-024-00284-8
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author Arjan Marelis
Fred Beekman
Jan-Diederik van Wees
author_facet Arjan Marelis
Fred Beekman
Jan-Diederik van Wees
author_sort Arjan Marelis
collection DOAJ
description Abstract Accurate and efficient predictions of three-dimensional subsurface stress changes are required for the assessment of geothermal operations with respect to fault stability and the potential risk for induced seismicity. This work extends the model capabilities of Mechanical Analysis of Complex Reservoirs for Induced Seismicity (MACRIS) to account for high-resolution thermo-elastic stress evaluations in structurally complex (i.e. faulted) and matrix permeability dominated geothermal systems. By adopting a mesh-free approach suitable to industry standard flow simulation models, MACRIS is capable of preserving the complex 3D hydraulic development of the injected cold-water volume and the 3D geometrical complexities of the reservoir model. The workflow has been applied to three-dimensional models with clastic reservoir characteristics representative for low enthalpy geothermal exploitation in the Netherlands. The models are marked by a single fault, subject to no and normal offset. Comparison of simulated stress evolutions in MACRIS with alternative analytical solutions highlight the effects of stress arching involved in the poro- and thermo-elastic stress developments on complex faults intersected by or in direct contact with the cold-water volume. Results are in agreement with previous studies and show the effect of thermal stressing to be dominant, arching of stresses to occur at the rim of the cold-water volume, and in cooling reservoirs, the intersection area of the cold-water volume in direct contact with the fault plane to be the main driver for fault reactivation and subsequent seismic potential. Moreover, results show the effects of stress arching (i) to be enhanced in the case of reservoir throw and flow compartmentalization, and (ii) to be reduced by a relative increase in conductive heat transfer between the reservoir and surrounding formations.
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spelling doaj.art-e5381a736eed4e46b34591ac83781bcf2024-03-05T18:38:32ZengSpringerOpenGeothermal Energy2195-97062024-02-0112112610.1186/s40517-024-00284-83D mechanical analysis of geothermal reservoir operations in faulted sedimentary aquifers using MACRISArjan Marelis0Fred Beekman1Jan-Diederik van Wees2Department of Earth Sciences, Utrecht UniversityDepartment of Earth Sciences, Utrecht UniversityDepartment of Earth Sciences, Utrecht UniversityAbstract Accurate and efficient predictions of three-dimensional subsurface stress changes are required for the assessment of geothermal operations with respect to fault stability and the potential risk for induced seismicity. This work extends the model capabilities of Mechanical Analysis of Complex Reservoirs for Induced Seismicity (MACRIS) to account for high-resolution thermo-elastic stress evaluations in structurally complex (i.e. faulted) and matrix permeability dominated geothermal systems. By adopting a mesh-free approach suitable to industry standard flow simulation models, MACRIS is capable of preserving the complex 3D hydraulic development of the injected cold-water volume and the 3D geometrical complexities of the reservoir model. The workflow has been applied to three-dimensional models with clastic reservoir characteristics representative for low enthalpy geothermal exploitation in the Netherlands. The models are marked by a single fault, subject to no and normal offset. Comparison of simulated stress evolutions in MACRIS with alternative analytical solutions highlight the effects of stress arching involved in the poro- and thermo-elastic stress developments on complex faults intersected by or in direct contact with the cold-water volume. Results are in agreement with previous studies and show the effect of thermal stressing to be dominant, arching of stresses to occur at the rim of the cold-water volume, and in cooling reservoirs, the intersection area of the cold-water volume in direct contact with the fault plane to be the main driver for fault reactivation and subsequent seismic potential. Moreover, results show the effects of stress arching (i) to be enhanced in the case of reservoir throw and flow compartmentalization, and (ii) to be reduced by a relative increase in conductive heat transfer between the reservoir and surrounding formations.https://doi.org/10.1186/s40517-024-00284-8Geothermal energyThermo-elasticityStress archingFault reactivationInduced seismicity
spellingShingle Arjan Marelis
Fred Beekman
Jan-Diederik van Wees
3D mechanical analysis of geothermal reservoir operations in faulted sedimentary aquifers using MACRIS
Geothermal Energy
Geothermal energy
Thermo-elasticity
Stress arching
Fault reactivation
Induced seismicity
title 3D mechanical analysis of geothermal reservoir operations in faulted sedimentary aquifers using MACRIS
title_full 3D mechanical analysis of geothermal reservoir operations in faulted sedimentary aquifers using MACRIS
title_fullStr 3D mechanical analysis of geothermal reservoir operations in faulted sedimentary aquifers using MACRIS
title_full_unstemmed 3D mechanical analysis of geothermal reservoir operations in faulted sedimentary aquifers using MACRIS
title_short 3D mechanical analysis of geothermal reservoir operations in faulted sedimentary aquifers using MACRIS
title_sort 3d mechanical analysis of geothermal reservoir operations in faulted sedimentary aquifers using macris
topic Geothermal energy
Thermo-elasticity
Stress arching
Fault reactivation
Induced seismicity
url https://doi.org/10.1186/s40517-024-00284-8
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AT fredbeekman 3dmechanicalanalysisofgeothermalreservoiroperationsinfaultedsedimentaryaquifersusingmacris
AT jandiederikvanwees 3dmechanicalanalysisofgeothermalreservoiroperationsinfaultedsedimentaryaquifersusingmacris