E \cdot \alpha_T^2 = k_{\alpha E} = {\rm const} |
where
| Young modulus | |
| thermal expansion coefficient | |
| universal constant |
Typical value for rocks is
Physics / Mechanics / Continuum mechanics / Young modulus (E)
R.E. Barker. J. Appl. Phys.34,1, 107(1963).
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