Uploaded by Levi Manasseh

Rock Mass Classification Systems: RQD, RMR, GSI, Q-System

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ROCK MASS CLASSIFICATION
ROCK MASS CLASSIFICATION
Components of rock mass classification system
1
# of joint sets
2
3
Engineering definition of a joint
• A joint is an obvious feature that is continuous if its
length is greater than the width of the excavation or if
it abuts against another joint (after Laubscher, 1990)
• Joints create blocks
Joint descriptions
• Trace length
• persistence / continuity
• Sets
• Roughness
• rough
• smooth
• undulating
• planar
• Frequency
• Orientation
• Dip and strike / dip direction
• Aperture
• Infilling
• Weathering
Joint sets and scanlines
Pole plot of discontinuities in a rock mass
Defining joint sets
Describing joint roughness
Classification of discontinuity roughness
Class
Description
I
Rough or irregular, stepped
II
Smooth stepped
III
Slickensided, stepped
IV
Rough or irregular, undulating
V
Smooth, undulating
VI
Slickensided, undulating
VII
Rough or irregular, planar
VIII
Smooth, planar
IX
Slickensided, planar
Joint and excavation orientations
Discontinuity
aperture
description
Joint persistence
Joint trace
length (m)
<1
1-3
3-10
ISRM
description of
persistence
Very low
Low
Medium
10-20
>20
High
Very high
Rock mass
classification
systems
Why classifications systems
• Classify overall rock mass using parameters relevant for the
purpose of the classification
• Predict performance of rock mass under load and select
appropriate support
• Common language for communication
• Compares conditions with past experience for strategic planning
• Groups sections of rock mass into areas of similar characteristics
• Enables tracking of changes in rock mass with time
• Preliminary basis for design
• Estimation of rock mass mechanical properties, e.g Young’s
modulus (E), and m and s in Hoek-Brown criterion
Problems with classification systems (1/2)
• Databases may be limited and bias towards a
particular task
• Most based on civil engineering experience
• Focused on global conditions
• Input parameters are very subjective
• Tendency to mislead and obscure necessity for
detail design
Problems with classification systems (2/2)
• Joint persistence inadequately accounted for: assume
all joints are continuous
• Block size assessment problematic
• Geology and mineralogy underplayed
• Mix external and intrinsic factors
Two systems of classification
•Single parameter classification systems
•Multi-parameter classification systems
Single parameter classification system: RQD
RQD is a measure
of block size
• Significance
• Component of most multiparameter systems
• Problems
• depends on direction but
currently implies direction
independent
• does not account for joint:
• weathering
• infillings
• orientation
• high RQD does not always imply
competent rock (clay gouge)
Other methods for estimating RQD
• RQD can be estimated directly in the field from excavation
surfaces
• Easy to do in scanline surveys
• RQD can be estimated from joint frequency
measurements in the field
• RQD can be obtained from three-dimensional area
mapping using the equation:
• RQD=115-3.3Jv
Where Jv is the number of joints present in cubic
meter of rock (i.e. the volumetric joint count)
RQD and joint frequency
Practical problem!
RQD and rock mass rating
Example application of RQD as a rock mass quality index
Terzaghi’s rock load classification system
Overburden weight
Movement occurs
within this area B1
Terminology
Resisting forces transfer
most of W1 to abutments
Loosened rock
Resisting
frictional
forces
Application to tunnel support design
Problems with Terzaghi Rock Load Classification System
• Too general to
• permit objective evaluation of rock quality
• Provides no quantitative information on the rock
mass properties
• Too conservative and only for steel arch support
design
Lauffer’s Stand-up time classification system
Definitions
• Stand-up time
• length of time which an
underground opening will stand
unsupported after excavation
and scaling.
• Active span
• largest unsupported span in the
tunnel section between the face
and the supports.
Relationship between active
span and stand-up time for
different rock mass classes
Method is semi-quantitative
Rock Structure Rating (RSR)
• Wickham et al (1972) described a quantitative
method for describing the quality of a rock mass
and for selecting appropriate support on the basis
of their Rock Structure Rating (RSR) classification.
• Most of the case histories, used in the
development of this system, were for relatively
small tunnels supported by means of steel sets,
• Historically this system was the first to make
reference to shotcrete support.
• It introduced the concept of rating each of the
components listed below to arrive at a numerical value
of RSR = A + B + C.
1. Parameter A, Geology: General appraisal of geological
structure on the basis of:
a. Rock type origin (igneous, metamorphic, sedimentary)
b. Rock hardness (hard, medium, soft, decomposed)
c. Geologic structure (massive, slightly faulted/folded,
moderately faulted/folded, intensely faulted/folded).
2. Parameter B, Geometry: Effect of discontinuity
pattern with respect to the direction of tunnel drive on
the basis of:
• Joint spacing.
• Joint orientation (strike and dip).
• Direction of tunnel drive.
3. Parameter C: Effect of groundwater inflow and joint
condition on the basis of:
a) Overall rock mass quality on the basis of A and B
combined.
b) Joint condition (good, fair, poor).
c) Amount of water inflow (in gallons per minute per
1000 feet of tunnel).
• Note that the RSR classification used Imperial units
and these units have been retained in this discussion.
• Three tables from Wickham et al (1972 ) are reproduced in
Tables 1, 2 and 3.
• These tables can be used to evaluate the rating of each of these
parameters to arrive at the RSR value (maximum RSR = 100).
NOTES:
• Dip: flat: 0-20o; dipping: 20-50o; and vertical: 50-90o
• Joint condition: good = tight or cemented; fair = slightly
weathered or altered; poor = severely weathered, altered or
open
Rock structure rating system - RSR:
Wickham
Introduced the system of
rating used in most
classification systems today
Application of RSR to tunnel design and limitations
t=1”+Wr/1.25
Rib
section
• The limitations of the
RSR system are:
• steel arch supports
• data based on small
tunnels
datum
8WF=8”-deep wide flange I section
weighing 31 pounds per foot
RMR or Geomechanics Classification system: Sometimes called
CSIR system
• Parameters
• UCS of rock material
• RQD
• joint spacing
• Joint condition
• roughness
• aperture
• persistence
• weathering
• Groundwater
• Relative orientation of joints
RMR structure
RMR joint persistence rating based on ISRM persistence
classification
Joint trace
length (m)
<1
1-3
RMR rating
3-10
10-20
2
1
>20
0
6
4
RMR parameter rating (1/2)
(2/2)
Evolution of RMR parameter ratings
Application of RMR to excavation design
RMR support selection
Limitations of RMR
• UCS rating is insensitive
• Double counting by including both joint spacing and
RQD
• Does not account for
• faults
• blasting
• Whole excavation is assessed en mass
• individual excavation surfaces important in mining
• Support recommendations by RMR are highly
conservative, in particular for mining purposes
Geological Strength
Index (GSI)
•Advantage for estimation of engineering
properties of rock masses
Geological
Strength Index GSI
Geological strength Index GSI
• GSI can be deduced from RMR from the following
equations:
For better quality rock masses (GSI>25)
GSI  RMR1976 OR GSI  RMR1989  5
Where groundwater rating and joint orientation
adjustments are set to zero for the RMR 1976 OR
for RMR 1989, groundwater rating set to 15 and
joint orientation adjustment set to zero
For poor quality rockmasses (GSI<25 or RMR<25), GSI charts must
used as RMR is no longer valid
Hoek & Brown parameters and GSI
mi values for intact rocks, by rock group
Hoek and Brown parameters for the rockmass from GSI
(recall: �1 = �3 + ��� �3 + ��� 2 )
 GSI  100 
m b  m i exp 

28


For GSI>25:
 GSI  100 
s  exp 

9


a  0 .5
For GSI<25:
s0
and
GSI
a  0 . 65 
200
Mohr-Coulomb parameters from GSI
Mohr-Coulomb in effective principal stress space
 1   cm  k 3
where k is the slope of the line relating 1 and 3
Hence:
k 1
sin  
k 1
and
 cm 1 sin  
c
2 cos 
1

Hence k=tan
3
Estimation of rock mass properties 1/2
Estimation of rock mass properties 2/2
GSI deficiencies
• Inherits deficiencies of RMR
• Very qualitative and therefore subjective
• block size description
• Joint surface qualitative
• Joint roughness - inter-block shear strength
not included
The Mining Rock Mass Rating System
• Summary of adjustments
• weathering 30-100
• orientation 63-100
• Induced stresses 60-120
• Blasting 80-100
Application of MRMR to stope design
Limitation of the system
• Major criticism of MRMR is that it is too
complicated to use and requires a lot of
experience to get it right!
Q-System - (TQI or NGI-system)
•Q-system (Barton et al. 1974)
•Q’-system
•Stability graph
Q-System
• Principal parameters
• Rock quality designation (RQD)
• Joint set number (Jn)
• Joint roughness (Jr)
• Joint alteration (Ja)
• Joint water reduction factor (Jw)
• Stress reduction factor (SRF)
(Note: Jr, Ja, Jw are the properties of the
critical joint)
Combination of factors for rockmass rating
• The rock mass is rated according to the following empirical
equation:
Q=(RQD/Jn)x(Jr/Ja)x(Jw/SRF)
• RQD/Jn=average block size
• Jr/Ja =joint surface integrity and interblock shear strength
• Jw/SRF=active stress state
Description of
considerations
and their
ratings in
tunnelling
quality index
(Q system)
Classification of the rock mass quality in Q-system
Q range
Rockmass description
0.001 – 0.01
Exceptionally poor
0.01 – 0.1
Extremely poor
0.1 - 1
Very poor
1-4
Poor
4 – 10
Fair
10 – 40
Good
40 – 100
Very good
100 – 400
Extremely good
400 - 1000
Exceptionally good
Limitations of the Q-system
• SRF is ambiguous
• difficult to determine
• Jn is always difficult to determine and often leads to
underestimation of rock mass quality
• RQD is directional but often used independent of
direction
• Wrong to include stress and water effects (stress and
water to intrinsic rock mass properties - external
factors)
• Does not account for joint persistence
• Assumes all joints are continuous
Relationship between Q and RMR
Application of Q-system to
excavation design
Definitions: ESR and De
• Excavation Support Ratio (ESR)
• accounts for excavation life span
• acceptable risk
• Equivalent dimension of
excavation (De)
De=Excavation span, diameter or
wall height (m)/ESR
Relationship between De and Q
Q-system for support design
Q-system for support selection
Concerns in the use of Q for support design in mining
• Too conservative
• Insensitive to changes in rock mass quality in
hard rock mining where rock mass qualities
generally fall within a narrow range
• Does not account for new support technologies
• spray-on liners e.g. Tekflex
• Does not account for relative orientation of
excavation with structure
• Does not account for blast damage
Application of Q-system to
stope design
•Modified Q (Q’)
•Stability graph - Mathews method
Modified Q - Q’
• Hard rock mines where open stoping can be used
generally dry and Jw=1
• SRF difficult to assess (set to 1) and is replaced
with a more realistic factor - Stress factor A
• Also wrong to include Jw and SRF in rock mass
rating as these are external factors
• Hence modified Q defined as:
Q’=(RQD/Jn)x(Jr/Ja)
Some empirical correlations between classification systems and rock mass mechanical properties
Correlation of RMR and Q with E
Best fitted
Equation
For ci<100
 GSI 10 

40 
 ci 
Em 
10
100
Stability graph for open stope design
1000
Modified stability number N'
• Definitions
• stability number N
N=Q’xAxBxC
• A=stress factor
• B=joint orientation factor
• C=gravity factor
• Hydraulic radius
HR=surface area/perimeter
• Stability graph is a plot of
stability number N against
shape factor HR (or S)
100
Stable zone
10
Caving
1
0.1
0
5
10
15
Hydraulic radius HR (m)
20
25
Charts for determining factors A, B and C
Problems with stability graph
• Did not account for
• faults
• blast damage
• time
• tension
• complex stope surface geometries
• C is not applicable to footwalls
• Originally subjective
• transition zones
• bias towards relaxation
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