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dc.contributor.author
Liem, Michael
dc.contributor.supervisor
Jenny, Patrick
dc.contributor.supervisor
Matthai, Stephan K.
dc.contributor.supervisor
Meyer-Massetti, Daniel Werner
dc.date.accessioned
2024-08-05T08:51:43Z
dc.date.available
2024-07-24T12:14:44Z
dc.date.available
2024-07-30T13:52:41Z
dc.date.available
2024-08-05T08:51:43Z
dc.date.issued
2024
dc.identifier.uri
http://hdl.handle.net/20.500.11850/685017
dc.identifier.doi
10.3929/ethz-b-000685017
dc.description.abstract
Subsurface applications such as geothermal heat extraction or CO2 sequestration are vital for solving today's energy and climate challenges. Their reservoir rock typically consists of fractured porous media, whose fractures can greatly affect flow, transport, and mechanics. Accurate and efficient modelling of the relevant physical processes and characterising the related parameters are crucial for performance estimation and risk assessment. This simulation-based thesis aims to enhance these aspects. Time-dependent hyperbolic partial differential equations (PDEs) are commonly used for modelling transport phenomena and seismic activity. Adaptive time stepping methods, like the adaptive conservative time integration (ACTI) scheme, improve the efficiency of explicit time integration by allowing variable local time steps. We extend ACTI to tracer transport in fractured porous media, achieving accurate results while reducing computational costs by orders of magnitude compared to global time stepping. Limited observability of subsurface reservoirs and substantial uncertainties, particularly concerning fractures and their apertures, pose challenges to accurate modelling. Ensemble-based data assimilation (DA) methods, like the ensemble smoother with multiple data assimilation (ESMDA), are established tools for reducing uncertainty in model parameters and improving simulation results. We demonstrate the significant impact of measurement strategies and matrix permeability on DA results, highlighting the utility of intermediate measurements during reservoir stimulation and the influence of matrix permeability on fracture parameter estimation. Constructing a prior ensemble that accurately reflects available knowledge is crucial for ensemble-based DA methods. We introduce the far-field stress approximation (FFSA), a proxy model which projects the far-field stresses onto the fracture planes and approximates shear displacement with linear elastic theory. The FFSA efficiently generates reasonable prior realisations of fracture apertures in a realistic two-dimensional fracture network. The resulting posterior ensemble matches the flow and transport behaviour of the synthetic reference at measurement locations. It improves the estimation of the fracture apertures, markedly outperforming results from prior ensembles based on naïve stochastic approaches. In conclusion, this thesis contributes to a more efficient and accurate simulation of fractured porous media, paving the way for improved reservoir management and decision-making in various subsurface applications.
en_US
dc.format
application/pdf
en_US
dc.language.iso
en
en_US
dc.publisher
ETH Zurich
en_US
dc.rights.uri
http://creativecommons.org/licenses/by-nc-nd/4.0/
dc.subject
Fractured porous media
en_US
dc.subject
Fracture flow and transport
en_US
dc.subject
Scalar transport
en_US
dc.subject
Higher-order flux scheme
en_US
dc.subject
Adaptive time stepping
en_US
dc.subject
Sub-time steps
en_US
dc.subject
CFL
en_US
dc.subject
Data assimilation
en_US
dc.subject
History matching
en_US
dc.subject
Ensemble Kalman filter
en_US
dc.subject
Prior knowledge
en_US
dc.subject
Prior distributions
en_US
dc.subject
Tracer test
en_US
dc.subject
Fracture aperture
en_US
dc.subject
Discrete fracture model
en_US
dc.title
Efficient Simulation of Tracer Transport in Fractured Porous Media and Data-Driven Aperture Estimation
en_US
dc.type
Doctoral Thesis
dc.rights.license
Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International
dc.date.published
2024-08-05
ethz.size
150 p.
en_US
ethz.code.ddc
DDC - DDC::6 - Technology, medicine and applied sciences::620 - Engineering & allied operations
en_US
ethz.code.ddc
DDC - DDC::5 - Science::550 - Earth sciences
en_US
ethz.grant
Data Guided Modelling and Uncertainty Quantification of Permeability Changes in Geological Formations due to Flow Induced Fracture Propagation and Rock-Chemistry
en_US
ethz.identifier.diss
30234
en_US
ethz.publication.place
Zurich
en_US
ethz.publication.status
published
en_US
ethz.leitzahl
ETH Zürich::00002 - ETH Zürich::00012 - Lehre und Forschung::00007 - Departemente::02130 - Dep. Maschinenbau und Verfahrenstechnik / Dep. of Mechanical and Process Eng.::02628 - Institut für Fluiddynamik / Institute of Fluid Dynamics::03644 - Jenny, Patrick / Jenny, Patrick
en_US
ethz.grant.agreementno
178922
ethz.grant.fundername
SNF
ethz.grant.funderDoi
10.13039/501100001711
ethz.grant.program
Projekte MINT
ethz.relation.cites
10.3929/ethz-b-000552667
ethz.relation.cites
20.500.11850/446779
ethz.relation.cites
20.500.11850/572415
ethz.relation.isSupplementedBy
10.3929/ethz-b-000632502
ethz.date.deposited
2024-07-24T12:14:45Z
ethz.source
FORM
ethz.eth
yes
en_US
ethz.availability
Open access
en_US
ethz.rosetta.installDate
2024-08-05T08:54:01Z
ethz.rosetta.lastUpdated
2024-08-05T08:54:01Z
ethz.rosetta.versionExported
true
ethz.COinS
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