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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