Geometrical evolution of stressed and curved solid‐fluid phase boundaries: 2. Stability of cylindrical pores
- 10 January 1994
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 99 (B1) , 517-530
- https://doi.org/10.1029/93jb02572
Abstract
No abstract availableKeywords
This publication has 16 references indexed in Scilit:
- Strain-induced preferential dissolution of halitePublished by Elsevier ,2003
- Geometrical evolution of stressed and curved solid-fluid phase boundaries: 1. Transformation kineticsJournal of Geophysical Research, 1994
- Chapter 10 Growth of Grain Contacts in Halite by Solution-transfer: Implications for Diagenesis, Lithification, and Strength RecoveryPublished by Elsevier ,1992
- Stability of a two-phase process involving a planar phase boundary in a thermoelastic solidContinuum Mechanics and Thermodynamics, 1992
- A thermodynamic analysis of the conditions of equilibrium at nonhydrostatically stressed and curved solid‐fluid interfacesJournal of Geophysical Research, 1991
- Thermodynamics of rock deformation by pressure solutionPublished by Springer Nature ,1990
- Influence of geometry upon crack healing rate in calcitePhysics and Chemistry of Minerals, 1987
- Star-shaped unstable growth of grain-boundary cavitiesPhilosophical Magazine A, 1978
- Finger-like crack growth in solids and liquidsPhilosophical Magazine, 1976
- Morphological Stability of a Particle Growing by Diffusion or Heat FlowJournal of Applied Physics, 1963