Characterization of drained and undrained response of thermally loaded repository rocks
- 1 April 1982
- journal article
- research article
- Published by American Geophysical Union (AGU) in Water Resources Research
- Vol. 18 (2) , 281-290
- https://doi.org/10.1029/wr018i002p00281
Abstract
No abstract availableThis publication has 14 references indexed in Scilit:
- Thermal Expansion of Fluids and Fracture Initiation in Compacting SedimentsGSA Bulletin, 1979
- Deformation of spherical cavities and inclusions in fluid-infiltrated elastic materialsInternational Journal of Solids and Structures, 1978
- Permeability changes during the flow of water through westerly granite at temperatures of 100°–400°CJournal of Geophysical Research, 1978
- The influence of pore pressure on the mechanical properties of Kayenta sandstoneJournal of Geophysical Research, 1978
- Transport phenomena in hydrothermal systems; the nature of porosityAmerican Journal of Science, 1977
- Theoretical bounds for thermal expansion, specific heat, and strain energy due to internal stressJournal of Geophysical Research, 1973
- The influence of an undrained change in stress on the pore pressure in porous media of low compressibilityGéotechnique, 1973
- An exact effective stress law for elastic deformation of rock with fluidsJournal of Geophysical Research, 1971
- The Pore-Pressure Coefficients A and BGéotechnique, 1954
- On the flow of water in an elastic artesian aquiferEOS, Transactions American Geophysical Union, 1940