Dynamic Model of the Zonal Disintegration of Rock Surrounding a Deep Spherical Cavity
Publication: International Journal of Geomechanics
Volume 17, Issue 6
Abstract
It is assumed that a deep spherical cavity is subjected to in situ stress at infinity, and the excavation process of the deep spherical cavity is treated like the decrease of pressure applied on its internal boundary. Trigonometric functions and hyperbolic cosine and sine functions are used in the scalar curvature. A non-Euclidean dynamic kinematic equation based on the strain incompatibility condition is derived. Laplace transformation and residue theory are used to deduce the stress fields. The strength criterion of the deep rock masses is applied to determine the number and magnitude of fractured zones and nonfractured zones of the surrounding rock masses around a deep spherical cavity.
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Acknowledgments
The work is supported by the National Natural Science Foundation of China (Grants 51325903 and 51279218), Project 973 (Grant 2014CB046903) the Natural Science Foundation Project of CQ CSTC (Grant CSTC, cstc2013kjrc-ljrccj0001), the Research Fund by the Doctoral Program of Higher Education of China (Grant 20130191110037), and the Chongqing Graduate Student Research Innovation Project (Grant CYB14017).
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© 2016 American Society of Civil Engineers.
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Received: Nov 19, 2015
Accepted: Sep 6, 2016
Published online: Oct 24, 2016
Discussion open until: Mar 24, 2017
Published in print: Jun 1, 2017
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