1972
DOI: 10.1007/bf02497798
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Approximate relation between the elastic constants of anisotropic rocks and the anisotropy parameters

Abstract: Many sedimentary rocks are transversely isotropic bodies, the deformation properties of which are characterized by independent constants: E z and E z) the Young's modulus for extension -compression in the plane of isotropy and normal to it; g z3) the Poisson ratio which characterizes contraction in the plane of iso=opy during compression in it; g12) the Poisson ratio characterizing contraction in the direction of the y axis, perpendicular to the plane of isotropy, during compression in the direction of the x o… Show more

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Cited by 46 publications
(18 citation statements)
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“…It can be shown that condition (2) actually occurs for fractured rock foundations. A sufficient experimental confirmation of this is given in [7].…”
supporting
confidence: 54%
“…It can be shown that condition (2) actually occurs for fractured rock foundations. A sufficient experimental confirmation of this is given in [7].…”
supporting
confidence: 54%
“…However, despite the simplicity of the constitutive relations, the determination of these elastic properties is not simple due to the lack of standardization for the measurement methods (Gonzaga et al 2008). The cross-shear modulus G 0 is the most difficult parameter to assess (Batugin and Nirenburg 1972;Homand et al 1993). Amadei et al (1987) discuss the ranges of properties for transversely isotropic rocks which can be found in nature.…”
Section: Ranges Of Properties Of Transversely Isotropic Rocksmentioning
confidence: 98%
“…While it is difficult to measure the shear modulus in the direction normal to the plane of isotropy of the TI material, several approximations in literature were made 17 : (15) will not be used in the examples presented in this work. It should only be used when laboratory measurements are not available.…”
Section: Materials Anisotropymentioning
confidence: 99%