Abstract
Rock salt exhibits fully ductile crystal plastic flow as well as brittle-ductile damage and water-assisted diffusive mass transfer (dissolution-precipitation transfer) at shallow crustal and even surface conditions. These processes lead to a wide range of coupled phenomena that influence compaction creep of salt backfill, deviatoric creep of intact rock salt, microcrack damage and healing, and the evolution of microstructure, porosity and permeability. While the purely
mechanical behaviour of salt is relatively well understood, the effects of water-assisted mass transfer, occurring in the presence of brine or adsorbed moisture, have received less attention.
This paper reviews the thermodynamic driving forces governing fluid-rock interactions in stressed rock salt and salt backfill, and the resulting effects on deformation and microstructural change.
mechanical behaviour of salt is relatively well understood, the effects of water-assisted mass transfer, occurring in the presence of brine or adsorbed moisture, have received less attention.
This paper reviews the thermodynamic driving forces governing fluid-rock interactions in stressed rock salt and salt backfill, and the resulting effects on deformation and microstructural change.
| Original language | English |
|---|---|
| Title of host publication | The Mechanical Behavior of Salt XI |
| Subtitle of host publication | Proceedings |
| Editors | Steven Sobolik, Mathew Ingraham, Edward Matteo, Melissa Mills, Tonya Ross, Donald Conley, John Stormont |
| Publisher | CRC Press |
| Pages | 426-437 |
| ISBN (Print) | 978-1-032-28220-6 |
| Publication status | Published - Jul 2025 |
| Event | 11th Conference on the Mechanical Behavior of Salt - Drury Plaza Hotel, Sante Fe, United States Duration: 8 Jul 2025 → 10 Jul 2025 |
Conference
| Conference | 11th Conference on the Mechanical Behavior of Salt |
|---|---|
| Abbreviated title | SaltMech XI |
| Country/Territory | United States |
| City | Sante Fe |
| Period | 8/07/25 → 10/07/25 |
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