Geoscience Reference
In-Depth Information
Table 14.19 Typical slopes under water (ICE, 1995).
Type of material
Description
Slopes in still water
Slopes in active water
Rock
Nearly vertical
Nearly vertical
Clay
Stiff
45
1V: 1H
45
1V: 1H
Firm
35
1V: 1.4H
30
1V: 1.7H
Sandy
25
1V: 2.1H
15
1V: 3.7 H
Sand
Coarse
20
1V: 2.7H
10
1V: 5.7H
Fine
15
1V: 3.7H
5
1V: 11.4H
Silt
Mud
10-1
1V: 5.7H to 57H
5
1V: 11.4 H or less
<
14.20 Side slopes for canals in different materials
The side slopes in canals depends on the type of natural materials, and the canal
depth.
A canal that is 1.0m in depth may have material that can have a 1V: 1.0H slopes,
while at 2.0m depth a slope of 1V: 2.0H may be required.
The flow velocity in the canal may require revetment protection, and that may
govern the slope.
Table 14.20 Typical slopes for earthen canals in different soil materials.
Group symbol
Material type
Minimum side slope
Comments
Rock
1V: 0.25 H
Extent of weathering and joints
may affect slope design
Boulders, cobbles
1V:1.5H
Good erosion resistance
Seepage loss
GW, GP
Gravels, well or poorly graded
1V: 2.5H
Good erosion resistance
SW, SP
Sands, well or poorly graded
Seepage loss
SC
Clayey sands
1V: 2.5H
Fine sands have poor erosion
SM
Silty sands
resistance
GM
Silty gravels
1V: 1.5H
Medium erosion resistance
GC
Clayey gravels
Medium seepage loss
ML
Inorganic low plasticity silts
1V: 1.5H
Poor erosion resistance for low
CL
Inorganic low plasticity clays
Plasticity index
OH
Organic low plasticity clays
Low seepage loss
MH
Inorganic high plasticity silts
1V: 3.0H
Low seepage loss
CH
Inorganic high plasticity clays
OH
Organic high plasticity clays
14.21 Seismic slope stability
Pseudo-static analysis is performed by applying an acceleration coefficient in the
analysis.
The long term parameters are considered appropriate, however both types of
analysis are presented in the table below. There seems to be a divided opinion in
the literature in using long term or short-term analysis.
Horizontal seismic coefficient (k h )
=
a max /g.
 
 
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