Journal ArticleDOI
A geometrical picture of anisotropic elastic tensors
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In this paper, a geometrical picture of fourth-order, three-dimensional elastic tensors in terms of Maxwell multipoles is developed and used to obtain the elastic tensor appropriate to various crystal symmetry groups.Abstract:
A geometrical picture of fourth-order, three-dimensional elastic tensors in terms of Maxwell multipoles is developed and used to obtain the elastic tensors appropriate to various crystal symmetry groups. Simply examining the picture shows whether an elastic tensor, described by its 21 independent components relative to an ill-chosen coordinate system, has an axis of symmetry of any order. The picture also facilitates obtaining the elastic tensor from the observed dependence of the three body-wave phase velocities on the direction of the propagation vector κ. In particular, for q = 2, 4, and 6, is a linear combination of the surface spherical harmonics of even orders up to and including q. Since determine uniquely, all the body-wave phase-velocity dependence on can be summarized by the 6 coefficients of spherical harmonics in P(2), the 15 coefficients in P(4), and the 28 coefficients in P(6). For nearly isotropic media, the anisotropy in the P velocity determines 15 of the 21 elastic coefficients, whereas determines the other 6 elastic coefficients. Our description of elastic tensors is generalized to all fourth-order tensors in three dimensions and certain fourth-order tensors in higher dimensions. The problem in higher dimensions produces simple examples of unitary representations of the rotation group ON+ with N ≥ 4 which contain no harmonic irreducible components.read more
Citations
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Journal ArticleDOI
A general anisotropic yield criterion using bounds and a transformation weighting tensor
A.P. Karafillis,Mary C. Boyce +1 more
TL;DR: In this paper, a gspeneral expression for the yield surface of polycrystalline materials is developed, which can describe both isotropic and anisotropic materials.
Journal ArticleDOI
The azimuthal dependence of Love and Rayleigh wave propagation in a slightly anisotropic medium
Martin L. Smith,F. A. Dahlen +1 more
TL;DR: In this article, the effect of a small anisotropy on the propagation of Love and Rayleigh surface waves in an arbitrarily stratified half-space was investigated, and it was shown that a slight elastic anisotropic effect gives rise to an azimuthal dependence of the phase velocities of both Love and rayleigh waves of the form c(ω, θ) = A1(ω) + A2(ω), cos 2θ + A3(ω).
Journal ArticleDOI
A simple method for inverting the azimuthal anisotropy of surface waves
TL;DR: In this article, the authors investigated the problem of retrieving anisotropy as a function of depth in the mantle, from the observed azimuthal variations of Love and Rayleigh wave velocities.
Journal ArticleDOI
Moment Tensors and other Phenomenological Descriptions of Seismic Sources—I. Continuous Displacements
TL;DR: In this article, the authors extended their earlier work to cover the possibility that 9 is a singular generalized function, so that s can be discontinuous or singular, even when s is smooth, generalized functions simplify the notation.
References
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Mechanics of Incremental Deformation
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TL;DR: In this paper, the authors present an approach to non-linear elasticity which is characterized by the use of cartesian concepts and of elementary mathematical methods that do not require a knowledge of the tensor calculus or other more specialized techniques.
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