launch meeting CLIFFS
Transcript of launch meeting CLIFFS
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CLIFFS launch meeting26 October 2005, Holywell Park, Loughborough University
Response of Slope Stability to Vegetation changes due to Climate Change
John Greenwood
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Vegetation
• Recent research and demonstration projects
• Stability analysis to take account of vegetation and hydrological effects
• Influences of Climate change
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Signs of assistance from the vegetation ? - Water Lane, Kent
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Grasses on dunes (The Wash)
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Dune Grasses – Deep roots
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Shallow Slips - M69 - Vegetation probably plays a part
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Slips on M11 _ Can vegetation help prevent them?
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CIRIA Bioengineering Demonstration site set up on M20
View to West (1994)
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M20 - View to West (1998)
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M20 Vegetation Trials,
Conclusions over the 5 year trial period
• Significant root growth to 1.2m or more
• Roots often follow fissures and discontinuities
• Moisture changes due to roots masked by seasonal changes
• Window sampling too destructive to vegetation
• Standpipe levels dominated by seasonal changes
• Tensiometers appropriate for monitoring seasonal changes and storm events (detail in Ciria RP81)
• Vegetation maintenance regime important
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EU ECOSLOPES PROJECT
Testing with the NTU shear box / pull out apparatus
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EU project - Ecoslopes
• Characterising contribution of vegetation
• Characterising plant/root architecture
• Characterising loading on vegetation
• Resistance to tree overturning
• Effect of fires on vegetation, erosion, and slope stability
• Forest stand stability
• Root architecture and tree stability modelling
• Slope stability modelling (Limit equilibrium, energy approach, numerical modelling, etc)
• Project database
• Slope Decision Support System
• www.ecoslopes.com
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Root Clamping for pull-out
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Root pull-out notation/terminology
Diameter at failure point
Bark
Core
F
Clamp
lf
lf1
dc
d
dfc
df
Diameter at clamp
Ground Surface
Reference Surface
e
Failure Points
dfc1, df1
Root
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Pull out test in progress
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Actual pull-out result on Hawthorne root, 21.9 mm Dia
0.00
0.50
1.00
1.50
2.00
2.50
3.00
3.50
0 50 100 150 200
Displacement (mm)
Fo
rce (
KN
)
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Deeper Slip
Less influence
c´v
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Slope stability analysis
• Traditional methods of limit equilibrium stability analysis –Bishop, Janbu, Fellenius(Swedish) etc.
• Methods are prone to error particularly for submerged slopes and deep slip surfaces with high ‘∝’ values.
• Problems because water forces not taken fully into account.
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The stability equation solution based on effective
interslice forces
Many of the problems associated with the conventional stability
analysis equations are overcome if the equilibrium of the soil slice
is considered in terms of effective interslice forces to derive the
stability equations (Greenwood 1987, 1989, 1989b)
The basic stability equation for the factor of safety, equation (1), is
accepted as correct.
F = ...... (1)( )
∝∑
+∑
sin
'tan''
W
Nc φl
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Forces associated with each slice
soil 1
γ1 c′1φ′1
soil 2
γ2 c′2 φ′2
α
U1 S
W
τ
U2
ul
X2′
E2′
X1′
E1′
N′
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Figure. Forces acting on a slice of the stability analysis
a –conventional approach using total interslice forces(Barnes 1995)
b – Revised approach using effective interslice forces and interslice water forces (Greenwood 1987,1989)
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The Greenwood General slope stability equation is
derived by taking account of all the water forces
acting on the slice and assuming the resultant of
interslice forces is parallel to the slip surface :-
( )( )[ ]∝∑
∝−−−∝+∑=sin
'tansincos' 12
W
UUuWcF
φll
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By appropriate assumptions, the General equation may be adapted to
include an estimation of the horizontal interslice force based on the
coefficient of horizontal earth pressure, ‘K’ :-
F = ( ) ( )[ ]( )∝∑
∝−+∝−−−∝+∑
sin
'tansintansincos' 12
W
ubWαKUUuWc φll
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Additional Forces due to Vegetation, Reinforcement and
Hydrological changes
soil 1
γ1 c′1φ′1
soil 2
γ2 c′2 φ′2
+ c′v
α
U1 +∆U2 S
W
τ
U2 +∆U2
ul +∆uvl
X2′
E2′
X1′
E1′
N′
Dw
Wv
β
X2′
Tθ
∆hw
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The General equation is adapted for inclusion of vegetation effects,
reinforcement and hydrological changes as follows:-
F =
( )( )[ ]]cos)cos(sin)[(
'tansin)sin(sin)()()(cos)()'( 1122
θβαφθβα
TDWW
TDUUUUuuWWcc
wv
wvvvvv
−−+∝+∑
+−−∝∆+−∆+−∆+−∝++′+∑ ll
( )( )[ ]∝∑
∝−−−∝+∑=sin
'tansincos' 12
W
UUuWcF
φll
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SLIP4EX - SLOPE STABILITY ANALYSIS (NTU Oct 2002) Sheet 1 - Comparison of Methods
(See sheet 2, for effects of reinforcement, vegetation and hydrological changes)
PROJECT : NTU DESCRIPTION OF ANALYSIS: reinforced example
Date: Oct-02
Enter slice Data
Height 1 Unit wt 1 Height 2 Unit wt 2 Height 3 Unit wt 3 Breadth Alpha Cohesion* Phi' hw1 hw2 hw K
Slice Nr m kN/m^3 m kN/m^3 m kN/m^3 m degrees kN/m^2 degrees m m m
1 1.2 20 4.2 -20 8 25 0 1.44 0.72 0.2
2 5.4 20 4.8 -3 8 25 1.44 5.9 3.67 0.2
3 8.1 20 4.8 16 8 25 5.9 4 4.95 0.2
4 9 20 4.8 36 8 25 4 5.9 4.95 0.5
5 4.8 20 4 57 8 25 5.9 0 2.95 0.5
6 0 0 0 0 0 0 0 0 0 0
7 0 0 0 0 0 0 0 0 0 0 0
8 0 0 0 0 0 0 0 0 0 0 0
9 0 0 0 0 0 0 0 0 0 0 0
10 0 0 0 0 0 0 0 0 0 0 0
11 0 0 0 0 0 0 0 0 0 0 0
12 0 0 0 0 0 0 0 0 0 0 0
13 0 0 0 0 0 0 0 0 0 0 0
14 0 0 0 0 0 0 0 0 0 0 0
15 0 0 0 0 0 0 0 0 0 0 0
Calculated forces on slices Total Resistance - Moment equilibrium Total Resistance - Horizontal force equilibrium
General General Simple Simple Swedish Bishop General General Simple Simple Swedish
W U1 U2 u Dist force cohesive res K' K' K ' K'
slice kN kN kN kN/m2 kN kN kN kN kN kN kN kN kN kN kN kN kN
1 100.80 0.00 10.37 7.20 -34.48 35.76 66.57 67.39 66.67 67.49 64.92 84.26 70.85 71.72 70.95 71.83 69.09
2 518.40 10.37 174.05 36.70 -27.13 38.45 201.59 201.68 197.82 197.91 197.60 202.94 201.87 201.96 198.09 198.18 197.87
3 777.60 174.05 80.00 49.50 214.34 39.95 285.33 289.31 282.00 285.98 273.24 268.08 296.83 300.97 293.36 297.50 284.25
4 864.00 80.00 174.05 49.50 507.85 47.47 210.68 273.05 283.77 346.14 236.46 309.57 260.42 337.51 350.77 427.86 292.28
5 384.00 174.05 0.00 29.50 322.05 58.75 123.32 203.41 126.31 206.40 55.25 170.80 226.42 373.48 231.92 378.97 101.44
6 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00
7 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00
8 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00
9 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00
10 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00
11 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00
12 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00
13 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00
14 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00
15 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00
total 982.62 220.38 887.49 1034.85 956.58 1103.93 827.47 1035.66 1056.38 1285.63 1145.09 1374.34 944.93
Factors of Safety (no reinforcement or vegetation)
Moment equilibrium Force equilibrium
Fm Ff
Greenwood General 0.90 0.77
Greenwood General (K as input) 1.05 0.93
Greenwood Simple 0.97 0.83
Greenwood Simple (K as input) 1.12 1.00
Swedish 0.84 0.69
Bishop 1.05
Janbu (fo =1.05) 0.95
Bishop iteration Janbu Iteration
F initial F input F calc F input F calc
1 1.06 1.05 0.95 0.95
Stability Spreadsheet
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Factors of Safety (no reinforcement or vegetation)
Moment equilibrium Force equilibrium
Fm Ff
Greenwood General 0.90 0.77
Greenwood General (K as input) 1.05 0.93
Greenwood Simple 0.97 0.83
Greenwood Simple (K as input) 1.12 1.00
Swedish 0.84 0.69
Bishop 1.05
Janbu (fo =1.05) 0.95
Bishop iteration Janbu Iteration
F initial F input F calc F input F calc
1 1.06 1.05 0.95 0.95
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Reinforcement, vegetation and hydrological effects may be
added (Sheet 2)
Root Force
Root direction
Additional cohesion Change in water table
Mass of Vegetation
Wind force
Wind direction
T Theta c'v delta hw1
delta hw2 delta hw Wv D Beta
slice kN (/m) deg kN/m2 m m m kN (/m) kN (/m) deg.
1 0.95 45 0 -0.1 -0.05 0 0 0
2 5 45 -0.1 -0.1 -0.1
3 0.6 45 -0.1 -0.05
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Factors of Safety with Reinforcement ,Vegetation and hydraulic changes included
Fm
Greenwood General No reinforcement/Veg 0.90
with reinf /veg /water as input 1.05
Greenwood General (K as input) No reinforcement/Veg 1.05
With reinf /veg /water as input 1.22
Greenwood Simple No reinforcement/veg 0.97
With reinf/veg/water as input 1.13
Swedish No reinforcement/veg 0.84
With reinf/veg/water as input 0.98
Spreadsheet calculations of change in Factor of Safety due to
Vegetation, Reinforcement and Hydraulic changes
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Which vegetation effects have most influence on stability?
• Mass of vegetation ?- insignificant compared with soil mass
• Fine roots? – Important for erosion, unlikely to influence cohesion at
depth
• Wind forces? - Only relates to shallow depth
• Moisture change/cu change? - possibly some indirect influence at
depth but unlikely below 2 –3m depth (seasonal changes likely to
override)
• Pore Pressures ? (relate to moisture change) – unlikely to influence in
the longer term, again seasonal and geological effects likely to override
• Coarse roots? - most likely to influence at shallow depth but few will
penetrate below 1.5 –2m
• Vegetation effects likely to be most significant at toe
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Stability analysis 2 important points demonstrated by the ‘General’ solution
• Shape of the critical slip surface governed
by overconsolidation / anisotropy of soils
(K values)
• Calculation of restoring forces at toe
(Where vegetation can have an effect) is
very sensitive to hydrological conditions.
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Example deep slip – comparison of circular and wedge type
analysis
Factor of Safety
Deep circle Wedge
Bishop 1.05 1.17
Swedish 0.72 0.86
General 0.83 0.94
General (with K=1.5) 0.96 0.94
slice
1
slice
2
slice
3
slice
4
slice
5
slice
6
c′ = 1.5 kN/m2
φ′ = 22 deg
γ = 20 kN/m3
K = 0
K = 1.5
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Example deep slip – importance of correct water forces at toe
of deep circle
For Slice 1 of DEEP CIRCLE
Method Restoring force (kN) Disturbing force (kN)
Bishop (?water surface) 54.10 -61.09
Swedish (water parallel to slip) 28.88 -61.09
Simple (water horizontal) 33.77 -61.09
General (actual water surface) 37.70 -61.09
General (actual water surface,K=1.5) (50.89) -61.09
Water conditions at toe critical tostability – Vegetation and drainage will help
slice
1
slice
2
slice
3
slice
4
slice
5
slice
6
c′ = 1.5 kN/m2
φ′ = 22 deg
γ = 20 kN/m3
K = 0
K = 1.5
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Example deep slip – importance of correct water forces at toe
of Wedge?
For Slice 1 of Wedge
Method Restoring force (kN) Disturbing force (kN)
Bishop (?water surface) 14.6 1.68
Swedish (water parallel to slip) 14.8 1.68
Simple (water horizontal) 14.8 1.68
General (actual water surface) 14.6 1.68
General (actual water surface,K=1.5) 14.6 1.68
Slice 1 is not sensitive to water conditions because α is very small
slice
1
slice
2
slice
3
slice
4
slice
5
slice
6
c′ = 1.5 kN/m2
φ′ = 22 deg
γ = 20 kN/m3
K = 0
K = 1.5
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Example deep slip – importance of correct water forces at toe
of Wedge?
For Slice 1 of Wedge
Method Restoring force (kN) Disturbing force (kN)
Bishop (?water surface) 14.6 1.68
Swedish (water parallel to slip) 14.8 1.68
Simple (water horizontal) 14.8 1.68
General (actual water surface) 14.6 1.68
General (actual water surface,K=1.5) 14.6 1.68
Slice 1 is not sensitive to water conditions because α is very small
slice
1
slice
2
slice
3
slice
4
slice
5
slice
6
c′ = 1.5 kN/m2
φ′ = 22 deg
γ = 20 kN/m3
K = 0
K = 1.5
But - Interesting to note that slice 1 could become unstable in its own right due to
the water force U2 on the right hand side,
ie, U2 = γγγγwhw22 / 2 If hw =1.6m, U2 =12.8 kN Total disturbing force = 14.5 kN
(--very close to local failure of slice 1! – could lead to progressive failure)
slice
1
U2
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Benefits/Uncertainties
• Reducing run-off quantities
• Roots to bind surface soils and resist erosion
• Roots to reinforce deeper soils
• ? Help to control moisture content and pore water
pressures. (Dehydration – fissures – vulnerable to
intense rain events) ?
• ? Will vegetation survive changing climate ?
Concerns re climate change
More severe events – greater risk of instability – vegetation has
important role to help moderate the extremes.
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Information/research needs
• Soil Bioengineering – important link between Engineering and the Environment
• Gaining of data on effects of the vegetation gives engineering confidence in the benefits and drawbacks (Ecoslopes)
• Theoretical Analysis (Correct consideration of water forces!) of the effects of the vegetation needs to be supported with field observation and measurement (Hydrology at toe most critical!)
• SI procedures for vegetated slopes being developed.
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Conclusions
• Slopes more likely to fail under extremes of
climate
• Vegetation can potentially help to mitigate
the effects of climate extremes
• Vegetation itself is susceptible to effects of
climate change – less easy to sustain?
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Trained roots in Bali
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Response of Slope Stability to Vegetation changes due to
Climate Change
Thanks to all colleagues involved in supporting this
work.
John Greenwood
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References
Greenwood, J.R. (1987). Effective Stress Stability Analysis. Discussion in 9th European Conference on
Soil mechanics and Foundations, Dublin Sept 1987. Vol 3, post conference proceedings, Balkema 1989,
pp.1082-1083.
Morrison, I.M. and Greenwood, J.R. (1989). Assumptions in simplified slope stability analysis by the
method of slices. Geotechnique 39, No 3, pp.503-509.
Greenwood, J.R., Vickers, A.W., Morgan, R.P.C., Coppin, N.J. and Norris, J.E. (2001). Bioengineering
The Longham Wood Cutting field trial. CIRIA Project Report 81, London
Greenwood, J.R., Norris, J.E., Wint, J. and Barker, D.H. (2003). Bioengineering and the transportation
infrastructure. Proceedings of the Symposium on Transportation Geotechnics, EMGG, Nottingham,
September 2003. Thomas Telford, pp.205-220.
Greenwood, J.R., Norris, J.E. and Wint, J. (2004). Assessing the contribution of vegetation to slope
stability. Journal of Geotechnical Engineering, Vol. 157, Issue 4 pp 199-208.
Greenwood, J.R. (2004a). SLIP4EX – program for routine slope stability analysis to include the effects of
vegetation, reinforcement and hydrological changes. Int. Conf. on Eco-Engineering: “The use of
vegetation to improve slope stability”. Thessaloniki, Sept 2004. (Accepted by Geological and
Geotechnical Engineering)