Geoscience Reference
In-Depth Information
Table 18.12
(
Continued
)
Parameter/
symbol
Description
Value
Rock wall contact
Particles
Filling
Fillings type
φ
r
Slightly altered joint
walls, non softening
mineral coatings
Non softening
Silty or sandy - clay
coatings, small clay
fraction
Low friction clay
mineral coatings
ie Kaolinite, mica
No mineral
fillings, only
coatings
20-25
°
3.0
Softening
8-16
°
4.0
Sandy particles, clay -
free disintegrated rock
clay mineral
(continuous, but
5 mm thickness)
clay mineral fillings
(continuous, but
5 mm thickness)
Swelling - clay fillings
ie montmorillonite
(continuous, but
5 mm thickness)
25-30
°
4.0
Strongly over-
consolidated non
softening fillings
Joint
alteration
number
J
a
16-24
°
6.0
Thin mineral
fillings.
Rock wall
contact before
10 cm shear
Medium or low
over-consolidation,
softening
Depends on access
to water and % of
swelling clay size
particles
12-16
°
8.0
6-12
°
8-12
Zones or bands
Disintegrated or
crushed rock and clay
Silty or sandy clays
6-24
°
6, 8 or
8-12
5.0
No rock wall
contact when
sheared (thick
mineral fillings)
Zones or bands,
small clay fraction
(non softening)
6-24
°
Thick continuous
zones or bands of clay
10,13
or
13-20
18.13 Active stress - relative effects of water, faulting,
strength/stress ratio
•
The active stress is the ratio of the joint water reduction factor and the stress
reduction factor.
•
The joint water reduction factor accounts for the degree of water seepage (Table
18.13).
18.14 Stress reduction factor
•
The stress reduction factor is a measure of (Table 18.14):
-
The loosening load where excavations occur in shear zones and clay bearing
rock,
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