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Elastic solutions of displacements for a transversely isotropic full space with inclined planes of symmetry subjected to a point load

✍ Scribed by Ting-Bin Hu; Cheng-Der Wang; Jyh-Jong Liao


Publisher
John Wiley and Sons
Year
2007
Tongue
English
Weight
522 KB
Volume
31
Category
Article
ISSN
0363-9061

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✦ Synopsis


Abstract

This work presents analytical solutions for displacements caused by three‐dimensional point loads in a transversely isotropic full space, in which transversely isotropic planes are inclined with respect to the horizontal loading surface. In the derivation, the triple Fourier transforms are employed toyield integral expressions of Green's displacement; then, the triple inverse Fourier transforms and residue calculus are performed to integrate the contours. The solutions herein indicate that the displacements are governed by (1) the rotation of the transversely isotropic planes (ϕ), (2) the type and degree of material anisotropy (E/E′, ν/ν′, G/G′), (3) the geometric position (r, φ, ξ) and (4) the types of loading (P~x~, P~y~, P~z~). The solutions are identical to those of Liao and Wang (Int. J. Numer. Anal. Methods Geomechanics 1998; 22(6):425–447) if the full space is homogeneous and linearly elastic and the transversely isotropic planes are parallel to the horizontal surface. Additionally, a series of parametric study is conducted to demonstrate the presented solutions, and to elucidate the effect of the aforementioned factors on the displacements. The results demonstrate that the displacements in the infinite isotropic/transversely isotropic rocks, subjected to three‐dimensional point loads could be easily determined using the proposed solutions. Also, these solutions could realistically imitate the actual stratum of loading situations in numerous areas of engineering. Copyright © 2007 John Wiley & Sons, Ltd.


📜 SIMILAR VOLUMES


Elastic solutions for a transversely iso
✍ Liao, J. J.; Wang, C. D. 📂 Article 📅 1998 🏛 John Wiley and Sons 🌐 English ⚖ 201 KB

We rederive and present the complete closed-form solutions of the displacements and stresses subjected to a point load in a transversely isotropic elastic half-space. The half-space is bounded by a horizontal surface, and the plane of transverse isotropy of the medium is parallel to the horizontal s