Geoscience Reference
In-Depth Information
Table 18.19 P - wave velocity estimate using Q value (adapted from Barton, 2006).
Rock mass quality, Q
value
<0.01
0.01-0.1
0.1-1.0
1 - 10
10 - 100
100 - 1000
Poor
Poor/Fair
Good
Description
Exception.
Extremely
Very
OK/very
Ext./Exc.
P - wave velocity V p (km/s)
1.5
1.5-2.5
2.5-3.5
3.5-4.5
4.5-5.5
RQD %
5%
5-10%
10-40%
40-80%
80-95%
95%
Fractures/metre
27
27-14
14-7
7-3
3
18.20 Prediction of lugeon using Q values
The Lugeon values provide an indication of the rock permeability.
Chapter 8 related the Lugeon value to the rock jointing characteristics-akey
parameters in the Q value assessment see Table 18.20.
Table 18.20 Average lugeon estimate using Q c value (adapted from Barton, 2006).
Qc Q UCS/100
0.001
0.01-0.1
0.1-1.0
1-10
10-100
100-1000
Poor
Poor/Fair
Good
Exception.
Extremely
Very
OK/very
Ext./Exc.
Description
Hard
porous
Hard
jointed
Hard
massive
Major fault
Minor fault
Typical lugeon value
1000-100
100-10
10-1
1-0.1
0.1-0.01
.01-0.001
Lugeon value at depth
1000 m
500 m
100 m
50 m
25 m
~0.01
0.01-0.1
0.1-1.0
1.0-10
10-100
0.01-0.001
0.1-0.01
0.1-0.01
1.0-0.1
~1.0
0.01-0.001
0.01-0.001
0.01-0.001
0.1-0.01
0.1-0.01
0.01-0.1
0.1-1.0
1.0-10
10-100
100-1000
0.01-0.001
18.21 Prediction of advancement of tunnel using Q values
The tunnel advancement is proportional to the rock quality.
The Q value has therefore been used by Barton to estimate the average tunnel
advancement.
The TBM rates decline more strongly with increasing tunnel length.
 
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