Abstract
We study fluid-induced deformation of granular media, and the fundamental role of capillarity and wettability on the emergence of fracture patterns. We develop a hydromechanical computational model, coupling a "moving capacitor"dynamic network model of two-phase flow at the pore scale with a discrete element model of grain mechanics. We simulate the slow injection of a less viscous fluid into a frictional granular pack initially saturated with a more viscous, immiscible fluid. We study the impact of wettability and initial packing density, and find four different regimes of the fluid invasion: cavity expansion and fracturing, frictional fingers, capillary invasion, and capillary compaction. We explain fracture initiation as emerging from a jamming transition, and synthesize the system's behavior in the form of a phase diagram of jamming for wet granular media. © 2020 authors. Published by the American Physical Society.
| Original language | English |
|---|---|
| Article number | 022012 |
| Number of pages | 7 |
| Journal | Physical Review Research |
| Volume | 2 |
| Issue number | 2 |
| Online published | 13 Apr 2020 |
| DOIs | |
| Publication status | Published - Apr 2020 |
| Externally published | Yes |
Funding
This work was supported by the US Department of Energy (Grant No. DE-SC0018357).
Publisher's Copyright Statement
- This full text is made available under CC-BY 4.0. https://creativecommons.org/licenses/by/4.0/
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