摘要: The distribution of the chemical potential in a non-hydro statically stressed solid has been investigated. It is shown that strained elastic bodies must have same value at all points solid; and simple expression relating to components stress derived. effect pure shear on equilibrium appears be small. For non-elastic which not reached stable configuration under there an additional term continuous function position body. numerical this cannot computed without making assumptions concerning mechanism deformation or flow; but it small, least for nearly bodies. Elastic anisotropy probably important factor development oriented fabric rocks. Such recrystallization as may caused by non-hydrostatic (shear) believed result mostly from initially uneven stresses grains rock, rates certain reactions.
harvard.edu
agu.org参考文章(6)
Roy Waldemar Goranson, Thermodynamic relations in multi-component systems ,(1930)
Handbook of Physical Constants Geological Society of America. ,(1942) , 10.1130/SPE36
P. W. Bridgman, On The Effect of General Mechanical Stress on the Temperature of Transition of Two Phases, with a Discussion of Plasticity Physical Review. ,vol. 7, pp. 215- 223 ,(1916) , 10.1103/PHYSREV.7.215
R. W. GORANSON, “Flow” in stressed solids: an interpretation Geological Society of America Bulletin. ,vol. 51, pp. 1023- 1033 ,(1940) , 10.1130/GSAB-51-1023
E. D. Williamson, The Effect of Strain on Heterogeneous Equilibrium Physical Review. ,vol. 10, pp. 275- 283 ,(1917) , 10.1103/PHYSREV.10.275
George A. Russell, Crystal growth and solution under local stress American Mineralogist. ,vol. 20, pp. 733- 737 ,(1935)