Geoscience Reference
In-Depth Information
Flow
Joint flow
Approx. water
J w value
pressure (kPa)
Dry excavations or
ie
<
5 L/min locally
<
100
1.0
minor inflow
Medium inflow or
Occasional outwash of joint fillings
100-250
0.66
pressure
Large inflow or
With unfilled joints
0.5
250-1000
high pressure in
competent rock
Large inflow or
Considerable outwash of joint fillings
0.33
high pressure
Or water pressure at blasting, decaying with time
0.2-0.1
Exceptionally
Or water pressure continuing without noticeable
>
1000
0.1-0.05
high inflow
delay
Table 18.14 Stress reduction factor (Barton et al., 1974 with updates).
Zone characteristics
SRF
value
Rock type
Weakness zones
Material in zone
Depth
Multiple occurrences,
very loose surrounding rock
Single
Single
Any
50m
50m
10
5
2.5
Weakness zones
intersecting excavations
which may cause
loosening of rock mass
when tunnel is excavated
Chemically
disintegrated
rock
Clay
Multiple shear zones, loose
surrounding rock
Single Shear zones
Single Shear zones
Loose, open joints,
heavily jointed
Any
50m
50m
Any
7.5
5.0
2.5
5.0
No
clay
Stress
σ / σ c
UCS/ σ 1
Near surface, open joints
favourable stress condition
very tight structure. Usually
favourable to stability, may be
unfavourable for wall stability
moderate slabbing after 1
hour in massive rock Slabbing
and rock bursts after a few
minutes in massive rock
heavy rock burst
(Strain burst) and immediate
dynamic deformations in
massive rock
Competent rock,
rock stress problems
Low
Medium
High
0.01
0.01- 0.3
0.3-0.4
2.5
1
0.5-2
200
200-10
10-5
5-3
0.5-0.65
5-50
50-
200
200-
400
3-2
0.65-1
2
1
Squeezing rock, plastic
flow of incompetent rock
under the influence of
high rock pressure
Mild squeezing rock pressure
Heavy squeezing rock pressure
1-5
5
5-10
10-20
Swelling rock, chemical
swelling activity depending
on pressure of water
Mild swelling rock pressure
Heavy swelling rock pressure
5-10
10-15
 
Search WWH ::




Custom Search