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Reactivation of variably sealed joints and permeability enhancement in geothermal reservoir rocks
Hydraulic stimulation of enhanced deep geothermal reservoirs commonly targets pre-existing joint networks with the goal of increasing reservoir permeability. Here, we study the permeability and strength of joint-free and jointed Buntsandstein sandstones from the EPS-1 exploratory borehole at the Sou...
Autores principales: | , , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Springer Berlin Heidelberg
2023
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10658799/ https://www.ncbi.nlm.nih.gov/pubmed/38026831 http://dx.doi.org/10.1186/s40517-023-00271-5 |
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author | Kushnir, Alexandra R. L. Heap, Michael J. Baud, Patrick Reuschlé, Thierry Schmittbuhl, Jean |
author_facet | Kushnir, Alexandra R. L. Heap, Michael J. Baud, Patrick Reuschlé, Thierry Schmittbuhl, Jean |
author_sort | Kushnir, Alexandra R. L. |
collection | PubMed |
description | Hydraulic stimulation of enhanced deep geothermal reservoirs commonly targets pre-existing joint networks with the goal of increasing reservoir permeability. Here, we study the permeability and strength of joint-free and jointed Buntsandstein sandstones from the EPS-1 exploratory borehole at the Soultz-sous-Forêts geothermal site (France). The studied jointed samples contain naturally formed fractures that are variably filled with secondary mineralisation. We find that the permeability of these rocks is more sensitive to the presence and orientation of bedding than to the presence of joints at the scale of the samples: permeability is lowest in samples where bedding is oriented perpendicular to the direction of fluid flow. While well-sealed joints can act as barriers to fluid flow, partially filled joints neither inhibit nor promote fluid flow with respect to their joint-free counterparts. These samples were then deformed under triaxial conditions to assess (1) whether deformation reactivates pre-existing joints, and (2) how permeability changes as a result of deformation. We find that the mechanical response of the rocks depends on the extent to which joints are sealed. Well-sealed joints locally increase rock strength and experimentally induced fractures do not exploit pre-existing joint surfaces; partially sealed joints, by contrast, act as planes of weakness that localise strain. Although the permeability of all samples increased during deformation, permeability increase was largest in samples with poorly filled joints. We conclude that hydraulic stimulation operations must carefully consider the extent to which targeted joint networks are filled. Partially sealed joints are ideal targets for stimulation: these features act as planes of weakness within the rock mass and their reactivation can result in significant increases in permeability. By contrast, well-sealed joints may increase rock strength locally and may never reactivate during stimulation, making them poor targets for permeability enhancement. SUPPLEMENTARY INFORMATION: The online version contains supplementary material available at 10.1186/s40517-023-00271-5. |
format | Online Article Text |
id | pubmed-10658799 |
institution | National Center for Biotechnology Information |
language | English |
publishDate | 2023 |
publisher | Springer Berlin Heidelberg |
record_format | MEDLINE/PubMed |
spelling | pubmed-106587992023-11-13 Reactivation of variably sealed joints and permeability enhancement in geothermal reservoir rocks Kushnir, Alexandra R. L. Heap, Michael J. Baud, Patrick Reuschlé, Thierry Schmittbuhl, Jean Geotherm Energy (Heidelb) Research Hydraulic stimulation of enhanced deep geothermal reservoirs commonly targets pre-existing joint networks with the goal of increasing reservoir permeability. Here, we study the permeability and strength of joint-free and jointed Buntsandstein sandstones from the EPS-1 exploratory borehole at the Soultz-sous-Forêts geothermal site (France). The studied jointed samples contain naturally formed fractures that are variably filled with secondary mineralisation. We find that the permeability of these rocks is more sensitive to the presence and orientation of bedding than to the presence of joints at the scale of the samples: permeability is lowest in samples where bedding is oriented perpendicular to the direction of fluid flow. While well-sealed joints can act as barriers to fluid flow, partially filled joints neither inhibit nor promote fluid flow with respect to their joint-free counterparts. These samples were then deformed under triaxial conditions to assess (1) whether deformation reactivates pre-existing joints, and (2) how permeability changes as a result of deformation. We find that the mechanical response of the rocks depends on the extent to which joints are sealed. Well-sealed joints locally increase rock strength and experimentally induced fractures do not exploit pre-existing joint surfaces; partially sealed joints, by contrast, act as planes of weakness that localise strain. Although the permeability of all samples increased during deformation, permeability increase was largest in samples with poorly filled joints. We conclude that hydraulic stimulation operations must carefully consider the extent to which targeted joint networks are filled. Partially sealed joints are ideal targets for stimulation: these features act as planes of weakness within the rock mass and their reactivation can result in significant increases in permeability. By contrast, well-sealed joints may increase rock strength locally and may never reactivate during stimulation, making them poor targets for permeability enhancement. SUPPLEMENTARY INFORMATION: The online version contains supplementary material available at 10.1186/s40517-023-00271-5. Springer Berlin Heidelberg 2023-11-13 2023 /pmc/articles/PMC10658799/ /pubmed/38026831 http://dx.doi.org/10.1186/s40517-023-00271-5 Text en © The Author(s) 2023 https://creativecommons.org/licenses/by/4.0/Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/ (https://creativecommons.org/licenses/by/4.0/) . |
spellingShingle | Research Kushnir, Alexandra R. L. Heap, Michael J. Baud, Patrick Reuschlé, Thierry Schmittbuhl, Jean Reactivation of variably sealed joints and permeability enhancement in geothermal reservoir rocks |
title | Reactivation of variably sealed joints and permeability enhancement in geothermal reservoir rocks |
title_full | Reactivation of variably sealed joints and permeability enhancement in geothermal reservoir rocks |
title_fullStr | Reactivation of variably sealed joints and permeability enhancement in geothermal reservoir rocks |
title_full_unstemmed | Reactivation of variably sealed joints and permeability enhancement in geothermal reservoir rocks |
title_short | Reactivation of variably sealed joints and permeability enhancement in geothermal reservoir rocks |
title_sort | reactivation of variably sealed joints and permeability enhancement in geothermal reservoir rocks |
topic | Research |
url | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10658799/ https://www.ncbi.nlm.nih.gov/pubmed/38026831 http://dx.doi.org/10.1186/s40517-023-00271-5 |
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