4D microvelocimetry reveals multiphase flow field perturbations in porous media
- Author
- Tom Bultreys (UGent) , Sharon Ellman (UGent) , Christian M. Schlepütz, Matthieu Boone (UGent) , Gülce Kalyoncu Pakkaner (UGent) , Shan Wang (UGent) , Mostafa Borji (UGent) , Stefanie Van Offenwert (UGent) , Niloofar Moazami Goudarzi (UGent) , Wannes Goethals (UGent) , Chandra Winardhi (UGent) and Veerle Cnudde (UGent)
- Organization
- Project
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- 3D X-ray velocimetry to explain fluid flow dynamics inside porous materials
- Unravelling unsteady fluid flows in porous media with 3D X-ray micro-velocimetry
- From pore to core: understanding multiphase flow in rocks from the µm- to the cm-scale using multi-scale X-ray imaging
- Energy storage in the geological subsurface: impact of salt precipitation in porous media
- Joint deformation estimation and Computerized Tomographic reconstruction for studying dynamic processes
- Development of methodologies for X-ray transmission CT imaging to provide both chemical and morphological information
- Hyperspectral speckle-based X-ray imaging
- Abstract
- Many environmental and industrial processes depend on how fluids displace each other in porous materials. However, the flow dynamics that govern this process are still poorly understood, hampered by the lack of methods to measure flows in optically opaque, microscopic geometries. We introduce a 4D microvelocimetry method based on high- resolution X-ray computed tomography with fast imaging rates (up to 4 Hz). We use this to measure flow fields during unsteady-state drainage, injecting a viscous fluid into rock and filter samples. This provides experimental insight into the nonequilibrium energy dynamics of this process. We show that fluid displacements convert surface energy into kinetic energy. The latter corresponds to velocity perturbations in the pore-scale flow field behind the invading fluid front, reaching local velocities more than 40 times faster than the constant pump rate. The characteristic length scale of these perturbations exceeds the characteristic pore size by more than an order of magnitude. These flow field observations suggest that nonlocal dynamic effects may be long-ranged even at low capillary numbers, impacting the local viscous- capillary force balance and the representative elementary volume. Furthermore, the velocity perturbations can enhance unsaturated dispersive mixing and colloid transport and yet, are not accounted for in current models. Overall, this work shows that 4D X- ray velocimetry opens the way to solve long- standing fundamental questions regarding flow and transport in porous materials, underlying models of, e.g., groundwater pollution remediation and subsurface storage of CO2 and hydrogen.
- Keywords
- Multidisciplinary, hydrogeology, 3D velocimetry, porous media, multiphase flow
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Citation
Please use this url to cite or link to this publication: http://hdl.handle.net/1854/LU-01HRYEQRQWNA3AGDYW4T83QYR0
- MLA
- Bultreys, Tom, et al. “4D Microvelocimetry Reveals Multiphase Flow Field Perturbations in Porous Media.” PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA, vol. 121, no. 12, 2024, doi:10.1073/pnas.2316723121.
- APA
- Bultreys, T., Ellman, S., Schlepütz, C. M., Boone, M., Kalyoncu Pakkaner, G., Wang, S., … Cnudde, V. (2024). 4D microvelocimetry reveals multiphase flow field perturbations in porous media. PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA, 121(12). https://doi.org/10.1073/pnas.2316723121
- Chicago author-date
- Bultreys, Tom, Sharon Ellman, Christian M. Schlepütz, Matthieu Boone, Gülce Kalyoncu Pakkaner, Shan Wang, Mostafa Borji, et al. 2024. “4D Microvelocimetry Reveals Multiphase Flow Field Perturbations in Porous Media.” PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA 121 (12). https://doi.org/10.1073/pnas.2316723121.
- Chicago author-date (all authors)
- Bultreys, Tom, Sharon Ellman, Christian M. Schlepütz, Matthieu Boone, Gülce Kalyoncu Pakkaner, Shan Wang, Mostafa Borji, Stefanie Van Offenwert, Niloofar Moazami Goudarzi, Wannes Goethals, Chandra Winardhi, and Veerle Cnudde. 2024. “4D Microvelocimetry Reveals Multiphase Flow Field Perturbations in Porous Media.” PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA 121 (12). doi:10.1073/pnas.2316723121.
- Vancouver
- 1.Bultreys T, Ellman S, Schlepütz CM, Boone M, Kalyoncu Pakkaner G, Wang S, et al. 4D microvelocimetry reveals multiphase flow field perturbations in porous media. PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA. 2024;121(12).
- IEEE
- [1]T. Bultreys et al., “4D microvelocimetry reveals multiphase flow field perturbations in porous media,” PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA, vol. 121, no. 12, 2024.
@article{01HRYEQRQWNA3AGDYW4T83QYR0, abstract = {{Many environmental and industrial processes depend on how fluids displace each other in porous materials. However, the flow dynamics that govern this process are still poorly understood, hampered by the lack of methods to measure flows in optically opaque, microscopic geometries. We introduce a 4D microvelocimetry method based on high- resolution X-ray computed tomography with fast imaging rates (up to 4 Hz). We use this to measure flow fields during unsteady-state drainage, injecting a viscous fluid into rock and filter samples. This provides experimental insight into the nonequilibrium energy dynamics of this process. We show that fluid displacements convert surface energy into kinetic energy. The latter corresponds to velocity perturbations in the pore-scale flow field behind the invading fluid front, reaching local velocities more than 40 times faster than the constant pump rate. The characteristic length scale of these perturbations exceeds the characteristic pore size by more than an order of magnitude. These flow field observations suggest that nonlocal dynamic effects may be long-ranged even at low capillary numbers, impacting the local viscous- capillary force balance and the representative elementary volume. Furthermore, the velocity perturbations can enhance unsaturated dispersive mixing and colloid transport and yet, are not accounted for in current models. Overall, this work shows that 4D X- ray velocimetry opens the way to solve long- standing fundamental questions regarding flow and transport in porous materials, underlying models of, e.g., groundwater pollution remediation and subsurface storage of CO2 and hydrogen.}}, articleno = {{e2316723121}}, author = {{Bultreys, Tom and Ellman, Sharon and Schlepütz, Christian M. and Boone, Matthieu and Kalyoncu Pakkaner, Gülce and Wang, Shan and Borji, Mostafa and Van Offenwert, Stefanie and Moazami Goudarzi, Niloofar and Goethals, Wannes and Winardhi, Chandra and Cnudde, Veerle}}, issn = {{0027-8424}}, journal = {{PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA}}, keywords = {{Multidisciplinary,hydrogeology,3D velocimetry,porous media,multiphase flow}}, language = {{eng}}, number = {{12}}, pages = {{8}}, title = {{4D microvelocimetry reveals multiphase flow field perturbations in porous media}}, url = {{http://doi.org/10.1073/pnas.2316723121}}, volume = {{121}}, year = {{2024}}, }
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