In-situ flow visualization with Geo-Positron-Emission-Tomography in a granite fracture from Soultz-sous-Forêts, France

GND
1323550518
Affiliation
Institute for Geosciences, Friedrich-Schiller-University Jena
Pingel, Janis Leon;
ORCID
0000-0001-6566-5829
Affiliation
Reactive Transport Department, Institute of Resource Ecology, Helmholtz-Zentrum Dresden-Rossendorf, 04318 Leipzig
Kulenkampff, Johannes;
GND
1323555196
Affiliation
Institute for Geosciences, Friedrich-Schiller-University Jena
Jara-Heredia, Daniel;
GND
1163630063
Affiliation
Institute for Geosciences, Friedrich-Schiller-University Jena
Stoll, Madeleine;
ORCID
0000-0001-5242-2983
Affiliation
Reactive Transport Department, Institute of Resource Ecology, Helmholtz-Zentrum Dresden-Rossendorf, 04318 Leipzig
Zhou, Wenyu;
Affiliation
Reactive Transport Department, Institute of Resource Ecology, Helmholtz-Zentrum Dresden-Rossendorf, 04318 Leipzig
Fischer, Cornelius;
GND
173246893
ORCID
0000-0002-7133-8717
Affiliation
Institute for Geosciences, Friedrich-Schiller-University Jena
Schäfer, Thorsten

We investigate the fluid flow field in a fractured granite core sample. Sequential imaging with Positron-Emission-Tomography (PET) allows direct reconstruction of flow streamlines, thus providing a unique insight into the fluid dynamics of complex fractured crystalline materials. Pulse migration experiments using the positron-emitting radionuclide 18F− as tracer were conducted on a fractured granitic drill core, originating from a depth of 1958 m of the Enhanced Geothermal System (EGS) reference site at Soultz-sous-Forˆets, France. The flow field was analyzed as a function of in- and outlet positions across the fracture, as well as applied flow rates. Different flow path characteristics were identified. Both the fracture aperture variation and the topography of the fracture surface affect the flow field with consequences on flow channeling and preferential flow paths. Furthermore, pulse migration experiments were also numerically simulated with a 2.5D model using COMSOL Multiphysics®.
While the higher flow rate experiments show wider and higher dispersion of the flow path, lower velocity results in more localized flow and channeling behavior. This type of study thus yields enhanced experimental insights into the hydrodynamics of fracture flow and its relation to the rough structure of a single fracture, compared to input-output experiments. It can help to validate model simulations and experimentally determine hydrodynamic parameters needed for reactive transport modeling that are otherwise estimated with a high degree of uncertainty.

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