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Orthotropic anisotropy: on contributions of elasticity parameters to a difference in quasi-P-wave-squared velocities resulted from propagation in two orthogonal symmetry planes
Authors:Filip P Adamus
Institution:Department of Earth Sciences, Memorial University of Newfoundland, St. John's, NL, A1C 5S7 Canada
Abstract:We investigate the dependence of quasi P-wave phase velocity propagating in orthotropic media on particular elasticity parameters. Specifically, due to mathematical facilitation, we consider the squared-velocity difference, urn:x-wiley:00168025:media:gpr12998:gpr12998-math-0001, resulted from propagation in two mutually perpendicular symmetry planes. In the context of the effective medium theory, urn:x-wiley:00168025:media:gpr12998:gpr12998-math-0002 may be viewed as a parameter evaluating the influence of cracks – embedded in the background medium – parallel to one or both aforementioned planes. Our investigation is both theoretical and numerical. Based on Christoffel's equations, we propose two accurate approximations of urn:x-wiley:00168025:media:gpr12998:gpr12998-math-0003. Due to them, we interpret the aforementioned squared-velocity difference as being twice more dependent on urn:x-wiley:00168025:media:gpr12998:gpr12998-math-0004, than on urn:x-wiley:00168025:media:gpr12998:gpr12998-math-0005. To describe the magnitude of the dependence, we consider the proportions between the partial derivatives of urn:x-wiley:00168025:media:gpr12998:gpr12998-math-0006. Further, it occurs that urn:x-wiley:00168025:media:gpr12998:gpr12998-math-0007 is influenced by the ratio of vertically propagating quasi P-wave to vertically propagating quasi S-wave. Anomalously high urn:x-wiley:00168025:media:gpr12998:gpr12998-math-0008 might be caused by the low P/S ratio, which in turn can be an indicator of the presence of gas in natural fractures or aligned porosity. Also, we carry out numerical sensitivity study, according to which urn:x-wiley:00168025:media:gpr12998:gpr12998-math-0009 is approximately twice more dependent on urn:x-wiley:00168025:media:gpr12998:gpr12998-math-0010 than on urn:x-wiley:00168025:media:gpr12998:gpr12998-math-0011, twice more sensitive to urn:x-wiley:00168025:media:gpr12998:gpr12998-math-0012 than to urn:x-wiley:00168025:media:gpr12998:gpr12998-math-0013, and equally dependent on urn:x-wiley:00168025:media:gpr12998:gpr12998-math-0014 as on urn:x-wiley:00168025:media:gpr12998:gpr12998-math-0015. The dependence on urn:x-wiley:00168025:media:gpr12998:gpr12998-math-0016 and urn:x-wiley:00168025:media:gpr12998:gpr12998-math-0017 can be neglected, especially for small phase angles. We verify the approximations and perform the sensitivity study, using eight examples of the elasticity tensors.
Keywords:Anisotropy  Elastics  Numerical study  Theory  Velocity analysis
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