Technical Papers
Nov 24, 2011

Effects of Grain Scale Heterogeneity on Rock Strength and the Chipping Process

Publication: International Journal of Geomechanics
Volume 12, Issue 6

Abstract

Heterogeneity is an important factor controlling fracture initiation, accumulation, and propagation within polycrystalline rock. Internal spatial variability in terms of mineralogy, grain size, and anisotropy affect the yielding process. To investigate these factors, a texture-generating algorithm integrated within a numerical model was developed to create realistic rock analogs and provide user control over geological characteristics including mineral type, grain size, and anisotropic crystal shape. A mineral-specific constitutive model was created and calibrated using published values and real laboratory strength values. Brazilian tensile strength and unconfined compressive strength (UCS) model tests were developed using the finite-difference modeling software FLAC to perform parametric analysis of a series of geological characteristics. The results show that the methodology is capable of realistically reproducing damage propagation and failure behavior similar to that observed during laboratory testing. The strength results show trends similar to those found during laboratory testing. This methodology was applied to the simulation of tunnel-boring machine (TBM) cutter excavation to investigate the effect of geomechanical characteristics on the chipping process.

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Acknowledgments

Financial support was provided by Herrenknecht AG and a Postgraduate Scholarship from the Natural Science and Engineering Research Council (NSERC) of Canada.

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Information & Authors

Information

Published In

Go to International Journal of Geomechanics
International Journal of Geomechanics
Volume 12Issue 6December 2012
Pages: 632 - 647

History

Received: Mar 29, 2011
Accepted: Nov 22, 2011
Published online: Nov 24, 2011
Published in print: Dec 1, 2012

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Authors

Affiliations

Marlène C. Villeneuve [email protected]
Lecturer, Dept. of Geological Sciences, Univ. of Canterbury, Christchurch 8140, New Zealand (corresponding author). E-mail: [email protected]
Mark S. Diederichs
Professor, Dept. of Geological Sciences and Geological Engineering, Queen’s Univ., Kingston, ON, Canada K7L 3N6.
Peter K. Kaiser
Professor, President, and CEO, Centre for Excellence in Mining Innovation, Laurentian Univ., Sudbury, ON, Canada P2E 2C6.

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