Geoscience Reference
In-Depth Information
Table 6.8 Field evaluation of rock weathering.
Properties
Weathering
XW
DW
SW
FR
Field description
Total
Discolouration &
Strength
No
discolouration.
strength loss, but
seems
evidence of
Readily
not enough to
similar to
chemical
disintegrates
allow small dry
fresh rock,
weathering
when gently
pieces to be
but more
shaken in
broken across
discoloured
water
the fabric - MW
Broken and
crumbled by
hand - HW
Struck by hammer
Dull thud
Rings
Rings
Allowable bearing
1 MPa
HW: 1-2 MPa
5-6 MPa
8 MPa
capacity Q all , other
MW: 2-4 MPa
than rocks below
Allowable bearing
0.75 MPa
HW: 0.75-1.0 MPa
2-3 MPa
4 MPa
capacity Q all of
MW: 1.0-1.5 MPa
argillaceous, organic
and chemically formed
sedimentary and
foliated metamorphic
rocks
Use of presumed bearing pressure from weathering only is simple - but not very
accurate - use only for preliminary estimate of foundation size.
Weathered shales, sandstones and siltstones can deteriorate rapidly upon exposure
or slake and soften when in contact with water. Final excavation in such materials
should be deferred until just before construction of the retaining wall/foundation
is ready to commence.
Alternatively the exposed surface should be protected with a blinding layer
immediately after excavation, provided water build up behind a wall is not a
concern.
A weathered rock can have a higher intact rock strength than the less weathered
grade of the same rock type, as a result of secondary cementation.
6.9 Rock classification
The likely bearing capacity can be made based on the rock classification.
There is approximately a ten fold increase in allowable bearing capacity from an
extremely weathered to a fresh rock.
The table is for shallow footings.
 
 
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