Temporary stability of slopes cut in London Clay Dr Nesha...
Transcript of Temporary stability of slopes cut in London Clay Dr Nesha...
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Temporary stability of slopescut in London Clay
Dr Nesha Kovacevic
Geotechnical Consulting Group, London
Deep excavations at Terminal 5
• Bottom-up construction
• Open cut excavations for economy
• Maximum depth 22m
• Cut slopes to be as steep as possible
• Stand-up time up to 1/2 years
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End shunt
CTB
Launch
chamber
Launch chamber
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Temporary stability of deep cuts in London Clay
• To predict stand-up time of deep cuts using numerical analyses and so optimise slope geometry – maximum steepness and minimum excavation and backfill?
• Only after calibration against case histories of temporary slope failures
(Bradwell, Prospect Park, Wraysbury)
Constitutive model forLondon Clay
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(εεεεdp)p (εεεεd
p)r εεεεd
p
ϕ ϕ ϕ ϕ ', c
'
ϕϕϕϕ'r , c'r
ϕϕϕϕ'p , c'p
Soil model used
G = G (p’, εεεεd)
K’ = K’ (p’, εεεεv)
0.0001 0.001 0.01 0.1 1
Axial strain or volumetric strain (%)
0
500
1,000
1,500
2,000
2,500
3,000
Se
ca
nt
(3
.G)/
p' o
r K
'/p
'
recommended shear
modelled shear
modelled bulk
Small strain stiffness curves in extension
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0 5 10 15 20
Shear strain, γ γ γ γ (%)
0
50
100
150
Sh
ea
r s
tre
ss
, τ τ τ τ
(kP
a)
0 0.025 0.05 0.075 0.1
Displacement across a 0.5m thick layer, ∆ ∆ ∆ ∆ (m)
σσσσ'=166.7kPa
γγγγ=∆/TT
∆∆∆∆ ττττ
Predicted behaviour in drained simple shear
-50
0
50PW
P c
ha
ng
e
0 2 4 6 8 10
Axial strain (%)
-150
-100
-50
0
Sh
ea
r s
tre
ss
(kP
a)
measured
predicted
Behaviour in undrained triaxial extension
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0 50 100 150 200 250
Vertical effective stress (kPa)
0
1
2
3
4
5
Vo
lum
etr
ic s
tra
in (
%)
Test (depth: 13.55m)
Predicted
Swelling in oedometer test
Non-linear permeability
model:k=k0.e
-b.p’
1E-012 1E-011 1E-010 1E-009 1E-008
Horizontal permeability (m/s)
50
40
30
20
10
0
Dep
th b
elo
w g
rou
nd
leve
l (m
)
A3
A3
A3
A3
A3
A2
A2
A2
A2
A2
A3
A2
A2A2
A2
A2
A2
A2
A2
A2
A2A2
A2A2
A2 A2A3
A3
A3
A3
A3
A2
Biii
Biii
Biii
Biii
BiiBii
Bi
East of basin
Near surface
A3
cen
tra
l and w
est
A2 central and west
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Short - term slope failure at Bradwell
3.5
m
Original ground levelClay Fill1:
1
Excavated slope at Bradwell
Marsh Clay
Weathered
London Clay
UnweatheredLondon Clay
GWL0.9m
11.3
m
2.7
m7.2
m
0.5
:1
1:1
200 40 60 80 100
Su (kPa)
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Tension zone
Predicted rupture surface at Bradwell by FE analysis
11.3
m London Clay
Marsh Clay
Clay Fill
MoS=1.02
εεεεpD=1%
Softening starts
at εεεεpD=5%
εεεεdp
Str
en
gth
residual
peak
5% 20%
Rupture
surface
Back-analysis by LEM(Skempton, 1965)
11.3
m
0.5
:1
1:1
1:1
Predicted rupture surfaces by LE and FE method of analysis
Clay Fill
Marsh Clay
London Clay
Predicted by FEM
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Short-term (undrained) failuresat Bradwell
• Can be analysed in terms of effective stresses using
the same constitutive model and soil parameters
as for the delayed failures of cuttings in London Clay
• Role of progressive failure is small, and concentrated
in the area around the toe of the slope
• Soil stiffness is of importance in estimating
the short-term stability
Slough
Windsor
Scale
0 1 2 3 4km
M25
Staines
StainesReservoir
HeathrowAirport
M4
Prospect Park
NM25
M4 Motorway
DatchetReservoir
WraysburyReservoir
King George VIReservoir
Site location
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Prospect Park failure 9 weeksafter excavation
Tectonic shear surface in London Clay
at Prospect Park
11
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Terrace Gravels
London Clay
London Clay
11
. 6m
Cut-off wall
Tectonic shear zone
Typical cross section at Prospect Park
Slip surface
0.5m
0 10mScale
With shear No shear
Movement vectors during excavation
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0
100 kPa
50
150
-50
0 10mScale
With shear No shear
Pore pressures at the end of excavation
0
100 kPa
50
150
-50
0 2 4 6 8
Depth of excavation below top ofLondon Clay (m)
0
0.1
0.2
Ho
rizo
nta
l m
ove
me
nts
(m
)
with shear
with shear, no prior gravel removalno shear, no prior gravel removal
shearzone
no shear
Horizontal movements at the top of London Clayduring excavation
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15% εεεεpD=2%
2%
15% εεεεpD=2%
2%
Rupture
surfaceRupture
surface
0 10mScale
With shear No shear
Plastic shear strains just prior to collapse
Ho
rizo
nta
l m
ove
me
nts
(m
)
0 0.2 0.4 0.6 0.8 1
Time since excavation (yrs)
0
0.1
0.2
with shear
with shear, no prior gravel removal
no shear, no prior gravel removal
no shear
Horizontal movements at top of London Clayafter excavation – Zero suction
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0 0.2 0.4 0.6 0.8 1
Time since excavation (yrs)
0
0.1
0.2
0.3
0.4
0.5
Ho
rizo
nta
l m
ove
me
nts
(m
)
025
Horizontal movements at top of London Clayafter excavation – With shear zone
Surface suction in kPa
50
Key factors determining time to failure
• Presence of tectonic shear
• Previous site history
• Surface suction; 25kPa gave the best match to observed time to failure
• Permeability profile and non-linearity
• Ko – if tectonic shear zone is absent
• Progressive failure – rate of drop from peak to residual strength
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Predicted failure mode for
5m bermed 1:1 slopes at T5
Surface suction 25kPa
Predicted failure mode
for 5m bermed 1:1 slope at T5
Surface suction ‘zero’
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Launch
chamber
Launch
chamber
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Lessons for the future
• Monitor movements to identify presence of tectonic shears or development of basal shear
• Take measures to maintain suctions at slope surface
• Monitor suctions• Differentiate between drying beds and
lagoons• Check sensitivity to Ko, k and surface
suction