Influence of degree of interlock on confined strength of jointed hard rock masses

The strength of jointed rock mass is strongly controlled by the degree of interlock between its constituent rock blocks. The degree of interlock constrains the kinematic freedom of individual rock blocks to rotate and slide along the block forming joints. The Hoek–Brown (HB) failure criterion and th...

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Main Authors: Navid Bahrani, Peter K. Kaiser
Format: Article
Language:English
Published: Elsevier 2020-12-01
Series:Journal of Rock Mechanics and Geotechnical Engineering
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S1674775520301098
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author Navid Bahrani
Peter K. Kaiser
author_facet Navid Bahrani
Peter K. Kaiser
author_sort Navid Bahrani
collection DOAJ
description The strength of jointed rock mass is strongly controlled by the degree of interlock between its constituent rock blocks. The degree of interlock constrains the kinematic freedom of individual rock blocks to rotate and slide along the block forming joints. The Hoek–Brown (HB) failure criterion and the geological strength index (GSI) were developed based on experiences from mine slopes and tunneling projects in moderately to poorly interlocked jointed rock masses. It has since then been demonstrated that the approach to estimate the HB strength parameters based on the GSI strength scaling equations (called the ‘GSI strength equations’) tends to underestimate the confined peak strength of highly interlocked jointed rock masses (i.e. GSI > 65), where the rock mass is often non-persistently jointed, and the intact rock blocks are strong and brittle. The estimation of the confined strength of such rock masses is relevant when designing mine pillars and abutments at great depths, where the confining pressure is high enough to prevent block rotation and free sliding on block boundaries. In this article, a grain-based distinct element modeling approach is used to simulate jointed rock masses of various degrees of interlock and to investigate the influences of block shape, joint persistence and joint surface condition on the confined peak strengths. The focus is on non-persistently jointed and blocky (persistently jointed) rock masses, consisting of hard and homogeneous rock blocks devoid of any strength degrading defects such as veins. The results from this investigation confirm that the GSI strength equations underestimate the confined strength of highly interlocked and non-persistently jointed rock masses. Moreover, the GSI strength equations are found to be valid to estimate the confined strength of persistently jointed rock masses with smooth and non-dilatant joint surfaces.
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spelling doaj.art-737721d95f4647c293363d9c87390cbe2022-12-21T17:26:18ZengElsevierJournal of Rock Mechanics and Geotechnical Engineering1674-77552020-12-0112611521170Influence of degree of interlock on confined strength of jointed hard rock massesNavid Bahrani0Peter K. Kaiser1Department of Civil and Resource Engineering, Dalhousie University, Halifax, Nova Scotia, Canada; Corresponding author.Bharti School of Engineering, Laurentian University, Sudbury, Ontario, CanadaThe strength of jointed rock mass is strongly controlled by the degree of interlock between its constituent rock blocks. The degree of interlock constrains the kinematic freedom of individual rock blocks to rotate and slide along the block forming joints. The Hoek–Brown (HB) failure criterion and the geological strength index (GSI) were developed based on experiences from mine slopes and tunneling projects in moderately to poorly interlocked jointed rock masses. It has since then been demonstrated that the approach to estimate the HB strength parameters based on the GSI strength scaling equations (called the ‘GSI strength equations’) tends to underestimate the confined peak strength of highly interlocked jointed rock masses (i.e. GSI > 65), where the rock mass is often non-persistently jointed, and the intact rock blocks are strong and brittle. The estimation of the confined strength of such rock masses is relevant when designing mine pillars and abutments at great depths, where the confining pressure is high enough to prevent block rotation and free sliding on block boundaries. In this article, a grain-based distinct element modeling approach is used to simulate jointed rock masses of various degrees of interlock and to investigate the influences of block shape, joint persistence and joint surface condition on the confined peak strengths. The focus is on non-persistently jointed and blocky (persistently jointed) rock masses, consisting of hard and homogeneous rock blocks devoid of any strength degrading defects such as veins. The results from this investigation confirm that the GSI strength equations underestimate the confined strength of highly interlocked and non-persistently jointed rock masses. Moreover, the GSI strength equations are found to be valid to estimate the confined strength of persistently jointed rock masses with smooth and non-dilatant joint surfaces.http://www.sciencedirect.com/science/article/pii/S1674775520301098Rock mass strengthDegree of interlockNon-persistently jointed rock massBlocky rock massGeological strength index (GSI)GSI strength equations
spellingShingle Navid Bahrani
Peter K. Kaiser
Influence of degree of interlock on confined strength of jointed hard rock masses
Journal of Rock Mechanics and Geotechnical Engineering
Rock mass strength
Degree of interlock
Non-persistently jointed rock mass
Blocky rock mass
Geological strength index (GSI)
GSI strength equations
title Influence of degree of interlock on confined strength of jointed hard rock masses
title_full Influence of degree of interlock on confined strength of jointed hard rock masses
title_fullStr Influence of degree of interlock on confined strength of jointed hard rock masses
title_full_unstemmed Influence of degree of interlock on confined strength of jointed hard rock masses
title_short Influence of degree of interlock on confined strength of jointed hard rock masses
title_sort influence of degree of interlock on confined strength of jointed hard rock masses
topic Rock mass strength
Degree of interlock
Non-persistently jointed rock mass
Blocky rock mass
Geological strength index (GSI)
GSI strength equations
url http://www.sciencedirect.com/science/article/pii/S1674775520301098
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