02-Loehr PPT Load transfer and failure modes for deep foundation
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Transcript of 02-Loehr PPT Load transfer and failure modes for deep foundation
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8/17/2019 02-Loehr PPT Load transfer and failure modes for deep foundation
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Load Transfer and Failure Modes
or eep oun a ons n ar
Slopes
J. Erik Loehr, Ph.D., P.E.
Associate Professor
University of Missouri
Passive slope reinforcement schemes
FillSoil Dowels
Shotcrete
Stiff Clay
Relic Shear Surface
Nails
Railway
2after Bruce and Jewell, 1986
ReticulatedMicropiles
Firm Stratum soil nails
sliding surface
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Mobilization of resistance
Most deep foundations are passive elements
that require relative pile-soil movement to
Relative mobilization of axial and lateral
components depends primarily on
• Orientation of reinforcement
• Stiffness of soil and reinforcement
• Structural and geotechnical limit states
3
Load transfer
S o i l M
o v e m
e n t
4
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Failure modes for piles in slopes
Soil failure
• passive (lateral) failureabove/below sliding
Sliding
SlopeSurface
ReinforcingMember
Sliding
Location after
Sliding
• pullout (axial) failureabove/below slidingsurface
Structural failure• flexural failure
• shear failure
Surface
FailedSoil
RelativeMovement
Initial LocationFailedSoil
RelativeMovement
Sliding
Initial Location
Slidin
Initial Location
• axial failure- compression
- tension Serviceability limits
5
Failure ofmemberin bending
RelativeMovement
li iSurface
Failure ofmemberin Shear
RelativeMovement
Large-scale model tests
6
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Reinforced slope (s/d≈3) w/ capping beam
7
Reinforced slope (s/d≈2) w/ capping beam
8
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Reinforced slope (s/d≈4) w/o capping beam
9
t-z analyses for axial load
axial
Input Profile of Axial Soil Movement
Cap Bearing
Pile AxialStiffness (EA)
Soil ShearResistance (t)
Sliding Surface
Axial Componentof moving soil
10
zSoil EndBearing (Q)
Stable Soil(no soil movement)
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Lateral load transfer – “long” pile
0-400 -200 0 200 400
Lateral Soil Reaction (kip/in)
0-1.2 -0.8 -0.4 0.0 0.4 0.8 1.2
Pile Deflection (in)
5
10
15
20
5
10
15
20
D e p t h ( f t )
sliding surface
limit soil
pressure
13
30
35
40
=0.01 in
=0.1 in =0.3 in
=1.0 in
ℓ
ℓ
ℓ
ℓ
30
35
40
Lateral load transfer – “long pile” mode
0
-400 -200 0 200 400
Lateral Soil Reaction (kip/in)
0
-1.2 -0.6 0.0 0.6 1.2
Pile Deflection (in)
0
-60 0 60 120 180
Bending Moment (kip-in)
0
-3.0 -1.5 0.0 1.5 3.0
Shear Force (kip)
5
10
15
20
25
5
10
15
20
25
D e p t h ( f t )
5
10
15
20
25
5
10
15
20
25
sliding surface
14
30
35
40
30
35
40
30
35
40
=0.01 in
=0.1 in
=0.3 in
=1.0 in
ℓ
ℓ
ℓ
ℓ
30
35
40
limit soil
pressure
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Lateral load transfer – “short pile” mode
0-12 -6 0 6 12
Pile Deflection (in)
0-400 -200 0 200 400
Lateral Soil Reaction (kip/in)
=5
10
15
20
D e p t h ( f t )
5
10
15
20
.
=0.5 in
=1.0 in
=10.6 in
ℓ
ℓ
ℓ
ℓ limit soil
pressure
15
30
35
40
30
35
40
sliding surface
Lateral load transfer – “short pile” mode
0
-12 -6 0 6 12
Pile Deflection (in)
0
-3000-2000-1000 0 1000
Bending Moment (kip-in)
0
-30 -15 0 15 30
Shear Force (kip)
0
-400 -200 0 200 400
Lateral Soil Reaction (kip/in)
5
10
15
20
D e p t h ( f t )
5
10
15
20
25
=0.1 in
=0.5 in
=1.0 in
=10.6 in
ℓ
ℓ
ℓ
ℓ
5
10
15
20
5
10
15
20
limit soilpressure
16
30
35
40
30
35
40
30
35
40
30
35
40
sliding
surface
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Lat. load transfer – “intermediate” mode
0-40 -20 0 20 40
Pile Deflection (in)
0-400 -200 0 200 400
Lateral Soil Reaction (kip/in)
=0.1 in 5
10
15
20
D e p t h ( f t )
5
10
15
20
.
=0.5 in
=10 in
=30 in
ℓ
ℓ
ℓ
sliding surface
limit soilpressure
17
30
35
40
30
35
40
Lat. load transfer – “intermediate” mode
0
-40 -20 0 20 40
Pile Deflection (in)
0
-1000 0 1000 2000 3000
Bending Moment (kip-in)
0
-30 -15 0 15 30
Shear Force (kip)
0
-400 -200 0 200 400
Lateral Soil Reaction (kip/in)
5
10
15
20
D e p t h ( f t )
5
10
15
20
=0.1 in
=0.5 in
=10 in
=30 in
ℓ
ℓ
ℓ
ℓ
5
10
15
20
5
10
15
20
slidingsurface
limit soilpressure
18
30
35
40
30
35
40
30
35
40
30
35
40
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Summary – load transfer and failure modes
Numerous failure modes
Controlling failure mode varies with
Load transfer for deep foundations in slopesis complex• Depends on
- Soil and pile stiffness
- Sliding depth
- Orientation of reinforcement
- Structural and geotechnical limit states
Generally dangerous to assume loaddistribution
19
Design Resistance for Deep
Foundations in Earth Slopes
J. Erik Loehr, Ph.D., P.E.
Associate Professor
University of Missouri
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Challenges for predicting resistance
Deformation required to mobilize resistance
Soil provides both load and resistance
Numerous limit states
Must consider compatibility and serviceability
of axial and lateral resistance
21
Limit states for soil reinforcement
Soil failure
• passive (lateral) failure above or below sliding surface
•
Structural failure
• flexural failure
• shear failure
• axial failure
- com ression- tension
Serviceability limits
22
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Prediction of reinforcement resistance
1. Estimate profile of soil movement
2. Resolve soil movement into axial and lateralcom onents
3. Independently predict mobilization of axial andlateral resistance
a. Using “p-y” analyses for lateral load transfer
b. Using “t-z” analyses for axial load transfer
4. Select appropriate axial and lateral resistancew cons era on g ven o compa y anserviceability
23
Soil movement components
Slope Surface
lat.
lat.
axial
24
SlidingSurface
axial
soil
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Lateral resistance from p-y analyses
Use “soil movement” option (L-Pile v4.0M or v5)
For an assumed depth of sliding:1. A l dis lacements in soil above slidin surface
2. Determine response from p-y analyses
3. Mobilized resistance is shear force in member atdepth of sliding
4. Repeat steps 1 through 3 with incrementallyincreasing displacement until a limit state is reached
Shear force at sliding depth when first limit stateis reached taken to be available resistance forthat sliding depth
25
Mobilization of lateral resistance
0
-80 -40 0 40 80
Mobilized Shear Force (kip)
=0.1 in
0
0.0 1.0 2.0 3.0 4.0 5.0
Pile Deformation (in)
0
-1500 -750 0 750 1500
Mobilized Bending Moment (kip-in)
10
20
30
=1.0 in
=3.0 in
clay
slide
10
20
30 D e p t h ( f t )
10
20
30
26
40
50
rock
40
50
40
50
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Mobilization of lateral resistance
40
45
50
15
20
25
30
35
M o b i l i z e d S h e a r F o r c e ( k i p )
27
0
5
10
0.0 1.0 2.0 3.0 4.0 5.0 6.0Total Slope Movement (in)
Axial resistance from t-z analyses
For an assumed depth of sliding:
1. Apply displacements in soil above sliding surface
-.
3. Mobilized resistance is axial force in member at depth
of sliding
4. Repeat steps 1 through 3 with incrementally
increasing displacement until a limit state is reached
Axial force at sliding depth when first limit state
is reached taken to be available resistance for
that sliding depth
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Mobilization of axial resistance
0
0 20 40 60 80 100 120 140 160
Mobilized Axial Load (kip)
=0.1 in
clay
slide
10
20
30 D e p t h ( f t )
=0.3 in
=0.42 in
=0.5 in
29
rock
40
50
Mobilization of axial resistance
120
140
160
40
60
80
100
M o b i l i z e d A x i a l F o r c e ( k i p )
30
0
20
0.00 0.25 0.50 0.75 1.00 1.25 1.50
Total Slope Movement (in)
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Repeat for other sliding depths…
Result is two resistance functions that describeresistance versus position along reinforcement
31
Resistance functions (per member)
0
0 50 100 150
Lateral Resisting Force (kip)
0
0 50 100 150 200 250
Axial Resisting Force (kip)
clay
10
20
30
S
l i d i n g D e p t h ( f t )
d
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Resistance functions (per lineal foot)
00 10 20 30 40 50
Axial Resisting Force (kip/ft)
00 5 10 15 20 25
Lateral Resisting Force (kip/ft)
10
20
30
S l i d i n g D e p t h ( f t )
clay
10
20
30
S l i d i n g D e p t h ( f t )
= -
33
40
50 rock
40
50
Member resistance divided by member spacing
Summary – design resistance
Predicting load transfer is the difficult part
Must consider all limit states, including
compa y an serv cea y
Resistance changes with location of sliding
surface
Process is presently tedious
34
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A Few Issues
35
Issues
Mode of soil movement
Drained vs. undrained loading
Factors of safety
p-y and t-z models
• influence of member size and spacing
• influence of member inclination
• drained models for cla s Cap/group/network effects
36
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Drained vs. undrained analyses
Check short- and long-term conditions
• Possible to have drained loading of slope, but
-
• Prudent to evaluate both & use least resistance
Question whether can use “sand” models to
evaluate drained loading for clays
37
Factors of Safety
Factor of safety against slope instability just like
other slope applications
reinforcement resistance is subject of debate
• Slope analyses already includes margin of safety
• Applying factor of safety to non-controlling limit states
has no benefit
• It is not appropriate to apply factor of safety toreinforcement resistance alone
• I personally believe should not apply factor of safety to
reinforcement resistance
38
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p-y and t-z models
Approach is at least semi-empirical
Not a lot of good data available
• - -
- Brown and Chancellor, 1997
- Liang, 2000
- Hasenkamp and Turner, 2000
• Large-scale laboratory model tests
- Boeckmann, 2006
- ex or,
- Bozok, 2009
39
p-y and t-z models – limit soil pressure
0.0
0 100 200 300 400 500 600 700 800 900 1000
Limit Soil Pressure (psf)
1.0
2.0
3.0
4.0
D e p t h ( f t )
DeBeer & Carpentier Ito & MatsuiReeseFlemingBromsPoulos
40
.
6.0
7.0
8.0
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Brown and Chancellor, 1997
41
Bending moments – Littleville
0
-40 -20 0 20 40
Bending Moment (in-kips)
redicted
0
-40 -20 0 20 40
Bending Moment (in-kips)
redicted
10
20
30 D e p t h ( f t )
measured (2+70U)
measured (1+70U)
downslope
p mod = 0.2
10
20
30 D e p t h ( f t )
measured (2+70U)
measured (1+70U)
upslope
p mod = 0.2
42
40
50 tot = 0.31-in
40
50 tot = 0.39-in
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Axial resistance – Littleville
0-60 -40 -20 0 20 40 6
Axial Load T, kip (+=tension)
0-60 -40 -20 0 20 40 60
Axial Load T, kip (+=tension)
10
20
30 D e p t h , z ( f t . )
downslope
10
20
30 D e p t h , z ( f t . ) upslope
= 0.3
z ult = 0.06-in
43
40
50predictedmeasured (2+70U)
measured (1+70U) tot = 0.24-in
.
z ult = 0.06-in40
50
predicted
measured (2+70U)
measured (1+70U)
tot = 0.34-in
Predicted mobilization – Littleville
80
100
120
Upslope Micropile
Sliding Depth = 33-ft
140
16.0
18.0
Upslope Micropile
Slide Depth = 33-ft
-
-40
-20
0
20
40
60
M o b i l i z e d A x i a l F o r c e ( k i p )
6.0
8.0
10.0
12.0
.
M o b i l i z e d S h e a r F o r c e ( k i p )
44
-120
-100
-80
0.0 1.0 2.0 3.0 4.0
Total Slope Movement (in)
pre c on
prediction A*
calibration points
0.0
2.0
4.0
0 5 10 15 20
Total Slope Movement (in)
s c ay mo e
API sand model
alternate
calibration points
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Model tests – no cap
25
30
o m )
44 (2.8) 25
30
o m )
10
15
20
n A l o n g P i l e ( i n .
f r o m b
o t LPile (2.8)
10
15
20
n A l o n g P i l e ( i n .
f r o m b
o t 44 (2.8)
t-z (2.8)
45
0
5
-300 -200 -100 0 100 200 300
Induced Bending Moment (lb-in)
P o s i t i
0
5
-1000 -500 0 500 1000
Induced Axial Load (lb)
P o s i t i
TC
Model tests – with cap
40
45
o m )
44 (1.9)40
45
o m )
44 (1.9)
15
20
25
30
35
n
A l o n g P i l e ( i n .
f r o m b
o t t t-z (1.9)
15
20
25
30
35
n A l o n g P i l e ( i n .
f r o m b
o t e .
46
0
5
10
-1000 -500 0 500 1000Induced Axial Load (lb)
P o s i t i
TC
0
5
-1500 -500 500 1500
Induced Bending Moment (lb-in)
P o s i t i
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Results
2.0
Kubo's tests
Awoshika's tests
0.5
1.0
.
p - m u l t i p l i e r
Recommended by
Reese's et al., 2006
0.0-35 -25 -15 -5 5 15 25 35
Batter angle (Degree)
Recommended by
Bozok, 2009
Summary – a few issues
Performance depends on soil movement
Check short- and long-term conditions
ac or o sa e y app e o s ope s a y
Uncoupled method suitable when no cap or
when cap influence is limited
Influence of cap difficult to model with current
tools
Work needed on p-y and t-z models
• Some evidence that current models appropriate
• Some evidence that modified models needed
48
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