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Deformation and water-assisted diffusive mass transfer in rock salt

Research output: Chapter in Book/Report/Conference proceedingConference contributionAcademicpeer-review

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.
Original languageEnglish
Title of host publicationThe Mechanical Behavior of Salt XI
Subtitle of host publicationProceedings
EditorsSteven Sobolik, Mathew Ingraham, Edward Matteo, Melissa Mills, Tonya Ross, Donald Conley, John Stormont
PublisherCRC Press
Pages426-437
ISBN (Print)978-1-032-28220-6
Publication statusPublished - Jul 2025
Event11th Conference on the Mechanical Behavior of Salt - Drury Plaza Hotel, Sante Fe, United States
Duration: 8 Jul 202510 Jul 2025

Conference

Conference11th Conference on the Mechanical Behavior of Salt
Abbreviated titleSaltMech XI
Country/TerritoryUnited States
CitySante Fe
Period8/07/2510/07/25

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