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In-situ hydraulic fracturing experiment

Applicant Valley Benoît Christian
Number 165677
Funding scheme Project funding
Research institution Centre d'hydrogéologie et de géothermie Université de Neuchâtel
Institution of higher education University of Neuchatel - NE
Main discipline Other disciplines of Earth Sciences
Start/End 01.09.2016 - 31.08.2020
Approved amount 299'706.00
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All Disciplines (2)

Discipline
Other disciplines of Earth Sciences
Geophysics

Keywords (6)

Hydromechanical rockmass response; hydraulic fracturing; Induced seismicity; Enhanced Geothermal Energy; In situ experiments; Grimsel test site

Lay Summary (French)

Lead
Être capable de créer de la perméabilité dans les massifs rocheux profonds de manière contrôlée permettrait d'extraire de l'énergie géothermale afin de chauffer les bâtiments et/ou produire de l'électricité. En Suisse, des températures entre 170 et 190°C sont présentes à des profondeurs de 4 à 6 km, mais la perméabilité des roches cristallines présentes à ces profondeurs est trop faible pour permettre la circulation des volumes de fluides nécessaire à l'extraction de la chaleur. La maitrise de processus d'ingénierie des réservoirs profonds par injection hydrauliques permettrait de pallier à cette situation.
Lay summary

Deux paradigmes sont typiquement invoqués lorsque l'on pour créer de la perméabilité en injectant des fluides: 1) La création de nouvelle fracture en tension, c'est-à-dire la fracturation hydraulique et 2) la réactivation de fracture existante en cisaillement associé avec de la dilation, généralement appelé la stimulation hydraulique. S'il est très probable que ces deux mécanismes peuvent être activés simultanément, les interactions entre ces processus sont peu connues et les paramètres du massif rocheux et de l'injection promouvant l'un ou l'autre des processus sont mal compris. Ceci est particulièrement vrai dans les roches cristallines pertinentes pour la géothermie profonde.

Afin d'adresser ces questions, nous allons effectuer des expériences d'injection en vue de générer des fractures hydrauliques dans les roches cristallines du laboratoire du Grimsel. L'avantage de travailler en laboratoire sous-terrain est que grâce à l'accès fourni par les différents tunnels du laboratoire il sera possible d'instrumenter le volume expérimental avec un détail sans précédents. Ceci permettra de capturer le développement des fractures hydraulique et leur impact sur les propriétés mécanique (champ de contraintes et de déformations) et hydraulique (variation du champ de pression et de la perméabilité).

Cette expérience générera des informations inédites sur les mécanismes de création de perméabilité dans les roches cristalline ce qui permettra de développer des stratégies d'injections permettant une meilleure ingénierie des réservoirs pour les projets géothermique profonds.

Direct link to Lay Summary Last update: 02.05.2016

Responsible applicant and co-applicants

Employees

Publications

Publication
Hydromechanical insight of fracture opening and closure during in-situ hydraulic fracturing in crystalline rock
Dutler Nathan, Valley Benoît, Gischig Valentin, Jalali Mohammadreza, Brixel Bernard, Krietsch Hannes, Roques Clément, AmannFlorian (2020), Hydromechanical insight of fracture opening and closure during in-situ hydraulic fracturing in crystalline rock, in International Journal of Rock Mechanics and Mining Sciences, 135, 104450-104450.
In situ observation of helium and argon release during fluid-pressure-triggered rock deformation
Roques Clément, Weber Ulrich W., Brixel Bernard, Krietsch Hannes, Dutler Nathan, Brennwald Matthias S., Villiger Linus, Doetsch Joseph, Jalali Mohammadreza, Gischig Valentin, Amann Florian, Valley Benoît, Klepikova Maria, Kipfer Rolf (2020), In situ observation of helium and argon release during fluid-pressure-triggered rock deformation, in Scientific Reports, 10(1), 1-9.
Influence of reservoir geology on seismic response during decameter-scale hydraulic stimulations in crystalline rock
Villiger Linus, Gischig Valentin Samuel, Doetsch Joseph, Krietsch Hannes, Dutler Nathan Oliver, Jalali Mohammadreza, Valley Benoît, Selvadurai Paul Antony, Mignan Arnaud, Plenkers Katrin, Giardini Domenico, Amann Florian, Wiemer Stefan (2020), Influence of reservoir geology on seismic response during decameter-scale hydraulic stimulations in crystalline rock, in Solid Earth, 11(2), 627-655.
On the Variability of Pressure Propagation During Hydraulic Stimulation Based on Seismic Velocity Observations
Schopper Florian, Doetsch Joseph, Villiger Linus, Krietsch Hannes, Gischig Valentin S., Jalali Mohammadreza, Amann Florian, Dutler Nathan, Maurer Hansruedi (2020), On the Variability of Pressure Propagation During Hydraulic Stimulation Based on Seismic Velocity Observations, in Journal of Geophysical Research: Solid Earth, 125(2), 2019-018801.
Hydraulic fracture propagation in a heterogeneous stress field in a crystalline rock mass
Dutler Nathan, Valley Benoît, Gischig Valentin, Villiger Linus, Krietsch Hannes, Doetsch Joseph, Brixel Bernard, Jalali Mohammadreza, Amann Florian (2019), Hydraulic fracture propagation in a heterogeneous stress field in a crystalline rock mass, in Solid Earth, 10(6), 1877-1904.
Hydraulic stimulation and fluid circulation experiments in underground laboratories: Stepping up the scale towards engineered geothermal systems
Gischig Valentin S., Giardini Domenico, Amann Florian, Hertrich Marian, Krietsch Hannes, Loew Simon, Maurer Hansruedi, Villiger Linus, Wiemer Stefan, Bethmann Falko, Brixel Bernard, Doetsch Joseph, Doonechaly Nima Gholizadeh, Driesner Thomas, Dutler Nathan, Evans Keith F., Jalali Mohammadreza, Jordan David, Kittilä Anniina, Ma Xiaodong, Meier Peter, Nejati Morteza, Obermann Anne, Plenkers Katrin, Saar Martin O., Shakas Alexis, Valley Benoît (2019), Hydraulic stimulation and fluid circulation experiments in underground laboratories: Stepping up the scale towards engineered geothermal systems, in Geomechanics for Energy and the Environment, 100175-100175.
Stress Measurements for an In Situ Stimulation Experiment in Crystalline Rock: Integration of Induced Seismicity, Stress Relief and Hydraulic Methods
Krietsch Hannes, Gischig Valentin, Evans Keith, Doetsch Joseph, Dutler Nathan Oliver, Valley Benoît, Amann Florian (2019), Stress Measurements for an In Situ Stimulation Experiment in Crystalline Rock: Integration of Induced Seismicity, Stress Relief and Hydraulic Methods, in Rock Mechanics and Rock Engineering, 52(2), 517-542.
A Multi-Scale Approach to Identify and Characterize the Preferential Flow Paths of a Fractured Crystalline Rock
Jalali Mohammadreza, Klepikova M., Doetsch Joseph, Krietsch Hannes, Brixel Bernard, Dutler Nathan, Gischig Valentin, Amann Florian (2018), A Multi-Scale Approach to Identify and Characterize the Preferential Flow Paths of a Fractured Crystalline Rock, American Rock Mechanics Association, Seattle.
Comprehensive geological dataset describing a crystalline rock mass for hydraulic stimulation experiments
Krietsch Hannes, Doetsch Joseph, Dutler Nathan, Jalali Mohammadreza, Gischig Valentin, Loew Simon, Amann Florian (2018), Comprehensive geological dataset describing a crystalline rock mass for hydraulic stimulation experiments, in Scientific Data, 5(1), 180269-180269.
Observations of Fracture Propagation During Decameter-Scale Hydraulic Fracturing Experiments
Dutler N. O., Valley B., Gischig V., Jalali M. R., Doetsch J., Krietsch H., Villiger L., Amann F. (2018), Observations of Fracture Propagation During Decameter-Scale Hydraulic Fracturing Experiments, American Rock Mechanics Association, Seattle.
The seismo-hydromechanical behavior during deep geothermal reservoir stimulations: open questions tackled in a decameter-scale in situ stimulation experiment
Amann Florian, Gischig Valentin, Evans Keith, Doetsch Joseph, Jalali Reza, Valley Benoît, Krietsch Hannes, Dutler Nathan, Villiger Linus, Brixel Bernard, Klepikova Maria, Kittilä Anniina, Madonna Claudio, Wiemer Stefan, Saar Martin O., Loew Simon, Driesner Thomas, Maurer Hansruedi, Giardini Domenico (2017), The seismo-hydromechanical behavior during deep geothermal reservoir stimulations: open questions tackled in a decameter-scale in situ stimulation experiment, in Solid Earth Discussions, 1-55.

Datasets

Data collection for the Grimsel In-Situ Stimulation and Circulation (ISC) experiment

Author Doetsch, Joseph; Gischig, Valentin; Amann, Florian; Jalali, Reza; Krietsch, Hannes
Publication date 12.10.2018
Persistent Identifier (PID) 10.3929/ethz-b-000276170
Repository ETH Research collection


Collaboration

Group / person Country
Types of collaboration
High Performance Computing for Geothermics, Univ. of Neuchâtel Switzerland (Europe)
- in-depth/constructive exchanges on approaches, methods or results
- Publication
- Research Infrastructure
Lawrence Livermore National Laboratory United States of America (North America)
- in-depth/constructive exchanges on approaches, methods or results
- Publication
SCCER-SoE plateform at ETH Zürich Switzerland (Europe)
- in-depth/constructive exchanges on approaches, methods or results
- Publication

Scientific events



Self-organised

Title Date Place
Workshop on in-situ hydraulic fracturing experiments 04.10.2018 Neuchâtel, Switzerland

Abstract

Successfully creating permeability in deep-seated rock masses to economically tap the heat to generate electricity remains a challenge for society. If solution can be found to unlock these resources a large amount of clean, local and renewable energy can be produced. Indeed, the Swiss Energy Strategy 2050 (ES2050) propose scenarios with 7% of national electricity supply from Deep Geothermal Energy (DGE), which corresponds to over 500 MWel installed capacity. In Switzerland, temperatures between 170-190°C are found at 4-6 km depths, but the natural permeability of deep crystalline basement rocks is too low to allow large volume fluid circulation for sufficient heat extraction. Therefore, permeability must be enhanced using high-pressure fluid injection to exploit DGE in an Enhanced Geothermal System (EGS).Two different paradigms are commonly referred to when discussing permeability creation processes through hydraulic injections: 1) hydraulic fracturing as the initiation and propagation of mode I fractures and 2) hydraulic stimulation, i.e. the mobilization of existing discontinuities in shear with associated dilation leading to a self-propping mechanism. The former is the common concept used in reservoir enhancement in the oil and gas industry, while the latter is typically the case in enhanced geothermal reservoirs. If it is currently accepted that both mechanisms can occur concomitantly, it is not well-understood how these processes interact and what rock mass characteristics and injection metrics controls which mechanisms dominate.To address these questions, relevant datasets from well-controlled hydraulic injection experiments are required. We propose to perform such experiments in an underground laboratory where rock mass conditions are representative of target formations for EGS in Switzerland, and with excellent access to the rock mass. Experimental work on small samples in loading frames suffers issues of scale because the samples tested are often homogenous and therefore unrealistic at larger scales. Well-controlled experiments at larger scales are often impeded by insufficient access to the rock mass. Funding to execute a well-controlled experiment at the Grimsel test site has secured under the umbrella of the Swiss Competence Center for Energy Research - Supply of Electricity (SCCER-SoE), and an experimental plan has been developed. This experiment is referred as the In-situ Stimulation and Circulation experiment (ISC-experiment). The ISC experimental plan focusses on the stimulation of existing shear zones, and includes an extensive pre- and post- stimulation rock mass characterization program and a comprehensive monitoring package. This unique setting will allow observations and measurements in a coupled manner of all parameters relevant to geomechanics (i.e. stress state, deformation, fracturing, pressure propagation during injection and following shut-in, etc.), hydrogeology (i.e. fluid flow, permeability, fracture connectivity, etc.) and seismology (i.e. a micro-seismic monitoring system at multiple scales).The objective of this proposal is to expand the ISC experimental plan by adding a research component dedicated to understanding and modeling the initiation and propagation of hydraulic fractures. This research will address unresolved questions regarding the initiation, propagation, and interaction of hydraulic fracturing in tough crystalline rocks. Multiple hydraulic fractures will be created using a variety of injection strategies to determine their behavior and compare their impact. The characterization and monitoring systems in place will allow precise mapping of hydraulic fracture evolution, and their impact on the pore pressure field and the rock mass. Essential parameters controlling hydraulics, such as fracture aperture changes during injection, will be measured. The seismic response to hydraulic fracturing will be measured and compared with shear zone stimulation. The research plan is composed of three main components: 1) execution of the hydraulic fracturing tests, 2) characterization of the fractured volume and the analyses of the collected data, and 3) benchmarking of hydraulic fracturing simulation tools against the field data set. Results of this research will significantly contribute to the understanding of injection strategies to truly engineer permeability creation in the rock mass at depth for deep geothermal systems.
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