Quantitative assessment of liquefaction potential in selected areas in Christchurch, New Zealand
Investigating Liquefaction Effects in Christchurch, New ... · Investigating Liquefaction Effects...
Transcript of Investigating Liquefaction Effects in Christchurch, New ... · Investigating Liquefaction Effects...
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Investigating Liquefaction Effects
in Christchurch, New Zealand
Jonathan Bray, Ph.D., P.E., NAEFaculty Chair in Earthquake Engineering Excellence
with M. Cubrinovski, J. Zupan, C. Markham, C. Beyzaei, R. Luque, M. Riemer, M. Stringer & M. TaylorUniversity of California - Berkeley & Univ. of Canterbury
Sponsors: National Science Foundation & Earthquake Commission New Zealand
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AcknowledgementsGraduate Students & Post-Docs: Josh Zupan, Merrick Taylor, Chris Markham, Christine Beyzaei, Kelly Robinson, Anna Winkley,
Duncan Henderson, Yasuyo Hosono, Matthew Hughes, Kun Ma, Simona Giorgini, Masoud Moghaddasi, Catherine Tatarniuk, Yusa Muhamed, Jawad Arefi, Patrick Kailey, Kelvin Loh, ...
Financial support: U.S. National Science Foundation EQC (NZ Earthquake Commission) MBIE (NZ government) Natural Hazards Research Platform & UC ECan (Environment Canterbury)
Collaboration with: Tom ORourke of Cornell Univ., R. Green of Virginia Tech, B. Bradley of Univ. of Canterbury, K. Stokoe & B. Cox of Univ. of Texas at Austin, L. Wotherspoon of U. of Auckland, S. van Ballegooy, M. Jacka, R. Wentz & others of Tonkin & Taylor, US-GEER team, Univ. of California, Berkeley, Univ. of Arkansas, JGS team, Kiso-Jiban Cons., McMillan Drilling Ser., Fugro, CERA, NHRP, CCC
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George F. Sowers
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OUTLINE Christchurch Geologic Setting 2010-2011 Canterbury Earthquakes Widespread Liquefaction Effects Site Investigations Evaluation of Liquefaction Effects Conclusions
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New Zealand
Pacific plate
Australianplate
Alpine FaultMCE Mw = 8
Christchurch
Wellington
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Canterbury Plains
Christchurch
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East-West Cross Section through Christchurch
CBDGroundsurface
Watertable
Top of RiccartonGravel
40m
20m
from M. Cubrinovski
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Streams in Central Christchurch (from 1850s Black Maps)
from M. Cubrinovski
Hereford St.
Armaph St.
Mad
ras
St.
Cathedral
Kilmore St.Zone 1
Zone 4
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Subsurface Profile: Madras & Armagh, Zone 4
SAND
GRAVEL
SAND
GRAVEL
SM
SAND
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Subsurface Profile at Kilmore St. in Zone 1
50 2.05 15%
Taylor et al. 2012RICCARTON GRAVEL
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R = 0.6246
0
0.5
1
1.5
2
2.5
3
3.5
4
0 20 40 60 80 100
Ic
Fines Content (%)
Ic Fines Content CorrelationsRobinson, Cubrinovski, & Bradley 2013
CBD Data from Taylor 2014 & Zupan 2014
Apparent FC
Idriss & Boulanger 2008
Chart1
2.368541.261.121.73
1.914661.271.131.74
2.004941.281.141.75
2.51781.291.151.76
1.93131.31.161.77
2.055321.311.171.78
2.120061.321.181.79
1.97411.331.191.8
2.083221.341.21.81
2.204821.351.211.82
2.348721.361.221.83
2.211941.371.231.84
2.169761.381.241.85
2.170241.391.251.86
2.440161.41.261.87
2.034121.411.271.88
1.951021.421.281.89
2.005221.431.291.9
2.003781.441.31.91
1.74931.451.311.92
1.70761.461.321.93
1.745281.471.331.94
1.85881.481.341.95
1.958721.491.351.96
1.942981.51.361.97
2.097541.511.371.98
1.879721.521.381.99
1.894961.531.392
2.605781.541.42.01
2.54691.551.412.02
2.56841.561.422.03
2.138141.571.432.04
2.568781.581.442.05
2.098761.591.452.06
2.198561.61.462.07
1.943221.611.472.08
1.899481.621.482.09
1.857461.631.492.1
1.917741.641.52.11
2.122441.651.512.12
1.977681.661.522.13
1.984861.671.532.14
2.137021.681.542.15
1.879461.691.552.16
1.779581.71.562.17
2.061941.711.572.18
1.721.582.19
1.731.592.2
1.741.62.21
1.751.612.22
1.761.622.23
1.771.632.24
1.781.642.25
1.791.652.26
1.81.662.27
1.811.672.28
1.821.682.29
1.831.692.3
1.841.72.31
1.851.712.32
1.861.722.33
1.871.73
1.881.74
1.891.75
1.91.76
1.911.77
1.921.78
1.931.79
1.941.8
1.951.81
1.961.82
1.971.83
1.981.84
1.991.85
21.86
2.011.87
2.021.88
2.031.89
2.041.9
2.051.91
2.061.92
2.071.93
2.081.94
2.091.95
2.11.96
2.111.97
2.121.98
2.131.99
2.142
2.152.01
2.162.02
2.172.03
2.182.04
2.192.05
2.22.06
2.212.07
2.222.08
2.232.09
2.242.1
2.252.11
2.262.12
2.272.13
2.282.14
2.292.15
2.32.16
2.312.17
2.322.18
2.332.19
2.342.2
2.352.21
2.362.22
2.372.23
2.382.24
2.392.25
2.42.26
2.412.27
2.422.28
2.432.29
2.442.3
2.452.31
2.462.32
2.472.33
2.482.34
2.492.35
2.52.36
2.512.37
2.522.38
2.532.39
2.542.4
2.552.41
2.562.42
2.572.43
2.582.44
2.592.45
2.62.46
2.612.47
2.622.48
2.632.49
2.642.5
2.652.51
2.662.52
2.672.53
2.682.54
2.692.55
2.72.56
2.712.57
2.722.58
2.732.59
2.742.6
2.752.61
2.762.62
2.772.63
2.782.64
2.792.65
2.82.66
2.812.67
2.822.68
2.832.69
2.842.7
2.852.71
2.862.72
2.872.73
2.882.74
2.892.75
2.92.76
2.912.77
2.922.78
2.932.79
2.942.8
2.952.81
2.96
2.97
2.98
2.99
3
3.01
3.02
3.03
3.04
3.05
3.06
3.07
3.08
3.09
3.1
3.11
3.12
3.13
3.14
3.15
3.16
3.17
3.18
3.19
3.2
3.21
3.22
3.23
3.24
3.25
3.26
3.27
3.28
3.29
3.3
3.31
3.32
3.33
3.34
3.35
3.36
3.37
3.38
3.39
3.4
3.41
3.42
3.43
3.44
3.45
3.46
3.47
3.48
3.49
3.5
Data
R&W(98)-General Correlation
R&W(98)-PI>>
13.931.9211
13.941.9212
13.951.9206
13.961.9148
13.971.9082
13.981.9083
13.991.9128
141.907
14.011.8996
14.021.8906
14.031.8869
14.041.8825
14.051.8798
14.061.8659
14.071.8722
14.081.8731
14.091.8754
14.11.8869
14.111.8763
14.121.87
14.131.8695
14.141.8688
14.151.8716
14.161.8792
14.171.8856
14.181.9023
14.191.9118
14.21.9199
14.211.9251
14.221.9342
14.231.9458
14.241.9498
14.251.9546
14.261.9505
14.271.9504
14.281.9502
14.291.9528
14.31.9554
14.311.9519
14.321.9537
14.331.9493
14.341.9478
14.351.9515
14.361.9587
14.371.9769
14.382.0227
14.392.0698
14.42.0623
14.412.0611
14.422.0827
14.432.0685
14.442.0651
14.452.0745
14.462.0762
14.472.0591
14.482.0515
14.491.9712
14.51.9058
14.511.8652
14.521.7723
14.531.6823
14.541.6402
14.551.6154
14.561.6048
14.571.617
14.581.6321
14.591.6448
14.61.6456
14.611.6429
14.621.6403
14.631.6393
14.641.6414
14.651.6421
14.661.6431
14.671.6437
14.681.6399
14.691.6371
14.71.6341
14.711.6325
14.721.628
14.731.626
14.741.6262
14.751.6248
14.761.6233
14.771.6184
14.781.6142
14.791.6125
14.81.607
14.811.6055
14.821.6009
14.831.5976
14.841.5948
14.851.5881
14.861.5811
14.871.5662
14.881.5585
14.891.557
14.91.5507
14.911.5468
14.921.5372
14.931.5301
14.941.5204
14.951.5055
14.961.4994
14.971.4878
14.981.482
14.991.4746
151.4574
15.011.4521
15.021.4437
15.031.4433
15.041.4426
15.051.4473
15.061.4505
15.071.4552
15.081.458
15.091.4595
15.11.4629
15.111.4611
15.121.4599
15.131.4623
15.141.4689
15.151.4672
15.161.4696
15.171.4698
15.181.479
15.191.4787
15.21.4832
15.211.4897
15.221.4964
15.231.4991
15.241.5024
15.251.5066
15.261.5121
15.271.5175
15.281.5158
15.291.5168
15.31.5191
15.311.5207
15.321.5246
15.331.5303
15.341.5321
15.351.5325
15.361.5316
15.371.5277
15.381.5281
15.391.5251
15.41.5234
15.411.5183
15.421.5208
15.431.5169
15.441.5139
15.451.5107
15.461.511
15.471.511
15.481.5111
15.491.5126
15.51.5184
15.511.5219
15.521.52
15.531.5283
15.541.5401
15.551.5527
15.561.5641
15.571.5727
15.581.5834
15.591.5943
15.61.6028
15.611.6141
15.621.6267
15.631.6336
15.641.6383
15.651.649
15.661.6587
15.671.6652
15.681.6744
15.691.6815
15.71.692
15.711.7053
15.721.726
15.731.7397
15.741.7546
15.751.7724
15.761.7874
15.771.8066
15.781.8204
15.791.837
15.81.8483
15.811.857
15.821.8702
15.831.8768
15.841.8833
15.851.8878
15.861.8987
15.871.9187
15.881.9244
15.891.9281
15.91.9355
15.911.9482
15.921.9596
15.931.9688
15.941.9745
15.951.9736
15.961.9692
15.971.9622
15.981.9578
15.991.9452
161.9325
16.011.9181
16.021.9064
16.031.8969
16.041.8841
16.051.8679
16.061.8466
16.071.806
16.081.7807
16.091.7917
16.11.7503
16.111.7343
16.121.7208
16.131.7094
16.141.7011
16.151.6873
16.161.6784
16.171.6697
16.181.6577
16.191.6553
16.21.6494
16.211.6445
16.221.6391
16.231.6344
16.241.6246
16.251.616
16.261.6092
16.271.6038
16.281.597
16.291.5908
16.31.5869
16.311.5833
16.321.5819
16.331.5793
16.341.5752
16.351.5645
16.361.5546
16.371.5479
16.381.5399
16.391.533
16.41.5263
16.411.5196
16.421.5171
16.431.5137
16.441.5123
16.451.5149
16.461.5192
16.471.518
16.481.5195
16.491.5227
16.51.5298
16.511.537
16.521.5459
16.531.557
16.541.5638
16.551.5676
16.561.5647
16.571.5601
16.581.5565
16.591.5546
16.61.5517
16.611.5492
16.621.5443
16.631.5382
16.641.5376
16.651.5365
16.661.5401
16.671.5483
16.681.5547
16.691.5654
16.71.5754
16.711.5821
16.721.5875
16.731.5904
16.741.5887
16.751.5832
16.761.5778
16.771.5782
16.781.5807
16.791.5825
16.81.5909
16.811.5963
16.821.5989
16.831.6051
16.841.6044
16.851.5976
16.861.5921
16.871.5846
16.881.5825
16.891.576
16.91.5721
16.911.5665
16.921.5641
16.931.5592
16.941.5574
16.951.5497
16.961.5504
16.971.5506
16.981.5469
16.991.5815
171.5659
17.011.5577
17.021.5578
17.031.5599
17.041.5581
17.051.5643
17.061.573
17.071.585
17.081.5922
17.091.6
17.11.6047
17.111.6078
17.121.608
17.131.6104
17.141.6094
17.151.6121
17.161.6137
17.171.615
17.181.6114
17.191.6078
17.21.6042
17.211.6029
>>
>>
FC-Ic Correlation
Data
R&W(98)-General Correlation
R&W(98)-PI
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Grain-Size Composition of SoilsSand ejecta samples from areas in Christchurch
(Courtesy of M. Pender, Univ. of Auckland)
Clean fine sands and non-plastic silty sands Does soil know that the #200 sieve exists?
#200
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Particle Shape of Soils
EQC funded work by Tonkin & Taylor & Others
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2010-2011 Canterbury Earthquakes
185 fatalities in the 22 FEB 2011 Christchurch M 6.2 Earthquake
Central Business District (CBD) destroyed
20,000 residential properties severely affected & 8,000 abandoned
700 km of waste water pipes with loss/limited service
Total economic loss: ~ NZ$30B (25% of its GDP)
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MW = 7.14 Sept 10
MW = 6.013 June 11
MW = 6.222 Feb 11
MW = 5.923 Dec 11
2010-2011 Canterbury Earthquake Sequence
GNS Science
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Seismic Demand in CBD
0 10 20 30 40
0.5
0
0.5
0
0.5
0
0.5
0
0.5
Time(s)
Acce
lerati
on (g
)
0 10 20 30 400
1
2
3
4
Time (s)
Ari
as In
ten
sity (
m/s
)
4 SEP 10: SIR = .09 m/s2
26 DEC 10: SIR = .20 m/s2
22 FEB 11: SIR = .59 m/s2
13 JUN 11: SIR = .14 m/s2
REHS 092 Recordings (GeoNet)
4 SEP 10D5-95 = 25 s
26 DEC 10D5-95 = 4 s
22 FEB 11D5-95 = 10 s
13 JUN 11D5-95 = 11 s
SIR = Ia 5-75 / D5-75
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Canterbury EQs: Widespread Liquefaction
Cubrinovski et al. 2011
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Liquefaction from 3+ EQs (Cubrinovski 2011)
Base Map 22 Feb 2011 Mw = 6.2White Areas 4 Sep 2010 Mw = 7.1Black Areas 13 Jun 2011 Mw = 6.0
CBD
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4 Sept 2010
(Mark Quigley: Avonside)
22 Feb 2011
16 April 2011
13 June 2011: Part 1
13 June 2011: Part 2
Repeated Liquefaction Events
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Age of Christchurch Soils
from M. Cubrinovski
After Liquefaction
0
-
Liquefaction Effects in Christchurch
From M. Cubrinovski
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Effects of Lateral Spreading
from M. Cubrinovski
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Performance of House Foundations
Crack
Settlement
from M. Cubrinovski
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from M. Cubrinovski
Seismic Performance of Buried Utilities
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Effects of Liquefaction on Water Mains
from M. Cubrinovski
No failure of HDPE pipes installed after 2010 Darfield EQ
from T. ORourke
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Liquefaction in Christchurch
(van Ballegooy et al. 2014)
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CPT Investigations in Christchurch
(van Ballegooy et al. 2014)
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0 1 2 3 4
0
2
4
6
8
10
12
14
16
18
20
Ic
Dep
th (m
)
0 200 400 600 800
0
2
4
6
8
10
12
14
16
18
20
qc1n
Z2-16Z2-8
CPT Z2-8 in July 2011: refusal at only 3.4 m
CPT Z2-16 in March 2013: advanced to 9 m with pre-collaring
CPT Investigations at Shallow Gravel Sites
DENSE GP
McMillan Drilling Services
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CPT Investigations at Shallow Gravel Sites
Pre-Collaring System (developed by I. Haycock, McMillan Drilling Services)
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CPT Z2-30 in April 2013: advanced through gravel with 20 ton truck
0 1 2 3 4
0
2
4
6
8
10
12
14
16
18
20
Ic
Dept
h (m
)
0 200 400 600 800
0
2
4
6
8
10
12
14
16
18
20
qc1n
Z2-30
CPT Investigations at Shallow Gravel Sites
DENSE GP
Fugro
qc = 60+ MPa
-
Capturing Liquefaction Effects
-
Post-Liquefaction Volumetric Strain (v)
Ishihara & Yoshimine 1992
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Post-Liquefaction Volumetric Strain (v)
Ishihara & Yoshimine 1992
Decreasing FS
Incr
easi
ng v
Dec
reas
ing
Dr
-
Capturing Liquefaction Effects
van Ballegooy et al. 2014
LSN considers when FS > 1
LSN limited by max v
LSN affected by Dr
LSN heavily weights shallow layers
-
Capturing Liquefaction Effects
van Ballegooy et al. 2014
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Liquefaction in Christchurch
(van Ballegooy et al. 2014)
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Liquefaction of Silty Sands
(from R. Wentz, Wentz-Pacific)
CPT at Christchurch site where no liquefaction effects were observed
-
Liquefaction of Silty Sands
Evaluation of 4 CPTs at site where no liquefaction effects were observed
(from R. Wentz, Wentz-Pacific)
LSN > 20
-
Observations of Liquefaction Ejecta
2010 Darfield EQ
Ejecta Observed
No Ejecta
van Ballegooy et al.Tonkin & Taylor
for the EQC
Ic = 1.8
-
Central Business District of ChristchurchStrong Motion Station
UCB/UC Study Zones
Liquefaction22 FEB 2011
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Seismic Demand in CBDEvent
MedianCSRM7.5(16% - 84%)
Level of Liquefaction
in CBD
4 SEP 10Mw = 7.1
0.12(0.10 0.17)
Low
26 DEC 10Mw = 4.8
0.07 None
22 FEB 11Mw = 6.2
0.20(0.16 0.28)
Severe
13 JUN 11Mw = 6.0
0.09(0.08 0.15)
Low
23 DEC 11Mw = 5.9 0.10 Low
CSRM7.5 = 0.65 (PGA/g) / MSF MSF = 6.9 exp(-Mw/4) 0.058 1.8Median PGA from recordings; 16% - 84% PGA from Bradley and Hughes (2012)
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Liquefaction Effects on Structures
15 cm
1.8o
Tilting and Sliding of Buildings Settlement of Ground next to Piled Bldg.
30 cm
= 1/70
Cracking due to Differential Settlement Tilt of Tall Buildings
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Central Business District of ChristchurchCBD STUDY ZONES:
107 UCB-UC CPTs13 UCB-UC BHs 34 CGD CPTs 8 CGD BHs
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Variability in Shallow SoilsCar Park on Corner of Armagh and Madras Streets
CTUC Building
UC Berkeley / Univ. of Canterbury CPTs by McMillan Drilling Services
Severe Liquefaction
-
Variability in Shallow SoilsCar Park on Corner of Armagh and Madras Streets
No-to-Minor Liquefaction || Severe Liquefaction
SM / ML
SP / GP
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CTUC BuildingLiquefaction-Induced Differential Settlement Induces Distress
GEER: Bray, Cubrinovski et al.
Building Settlement (cm)Maximum Angular Distortion 1 / 50
490
7811206
31
Ejecta
0
-
CTUC Building
Severe Liquefaction Zone
B
-
CTUC Building: Christchurch EQ
2011 Christchurch EQ: Robertson & Wride (1998)
N
-
CTUC Building Settlement
~40 cm ~15 cm
Actual Settlement
~15 cm ~10 cm ~5 cm
Robertson & Wride (1998) & Zhang, Robertson et al. (2002)
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0 0.5 1 1.5 2
0
1
2
3
4
5
6
7
8
9
10
FS
Dep
th (m
)
0 5 10 15 20
0
1
2
3
4
5
6
7
8
9
10
Settlement (cm)
4 SEP 1026 DEC 1022 FEB 1113 JUN 11
CTUC Building: Sensitivity of Results
Robertson & Wride (1998) & Zhang, Robertson et al. (2002)
CPT Z4-5
-
SA BuildingLiquefaction-Induced Differential Settlement
GEER: Bray, Cubrinovski et al.
-
SA BuildingLiquefaction-Induced Differential Settlement
2011 Christchurch EQ
-
2011 Christchurch EQ: Robertson & Wride (1998)
SA Building: Christchurch EQ
-
0 0.5 1 1.5 2
0
1
2
3
4
5
6
7
FS
Dep
th (m
)
0 5 10 15 20
0
1
2
3
4
5
6
7
Settlement (cm)
4 SEP 1026 DEC 1022 FEB 1113 JUN 11
SA Building: Sensitivity of Results
Robertson & Wride (1998) & Zhang, Robertson et al. (2002)
CPT Z8-7
Observed Settlement10 cm - 25 cm
FSBC 1
-
PWC BuildingLiquefaction-Induced Differential Settlement and Tilt
GEER: Bray, Cubrinovski et l
21 stories on basement mat
-
PWC Building
2011 Christchurch EQ: Robertson & Wride (1998)
-
Cyclic Triaxial Test Results
0
0.05
0.1
0.15
0.2
0.25
1 10 100
CSR
= d
/(2'
c)
No. Cycles
Upper Soil--Field
Lower Soil--Field
Cycles to ax-S.A.=3%
FC = 4 to 8%
FC = 22 to 26%
CTUC Building Shallow Soils
Ph.D. Students: C. Markham & C. Beyzaei
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D&M Thin- Walled Piston Sampler
Undisturbed Soil Sampling & Testing
Careful Handling
Cut Extrude Test
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Ph.D. Students: C. Markham & R. Luque
Calibration of Constitutive Model for Numerical Analyses
FTG-7 Building
PM4SAND
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LIQUEFACTION
1964 Niigata, Japan EQ (from H.B. Seed)1906 San Francisco EQ (Lawson et al. 1908)
1989 Loma Prieta EQ
EFFECTS
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LIQUEFACTION EFFECTS
Flow Liquefaction Cyclic Mobility(strain-softening large strain) (strain-hardening limited strain)
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LIQUEFACTION Factor of Safety (FS)
Idriss & Boulanger 2008
CRR
LiquefactionEffects Observed at Ground Surface
No LiquefactionEffects Observed at Ground Surface
FS = CRR / CSRCSR
FS =1.2
FS =1.2
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LIQUEFACTION EFFECTS
Idriss & Boulanger 2008
Flow Liquefaction
Cyclic Mobility
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Liquefaction Flow Slides when qc1Ncs-Sr < 85
Idriss & Boulanger 2008
85
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CONCLUSIONS Liquefaction severely damaged ground,
buildings, and buried utilities in Christchurch Loose shallow silty sand layer led to much of the
damage in CBD, especially in areas with ejecta Shear-induced deformation is critical mechanism Current analytical procedures do not capture
effects of liquefaction well in Christchurch Each EQ was well recorded, so there is an
opportunity to refine analytical procedures
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RECOMMENDATIONSFor level ground conditions with no free-face:
Pile foundation with its neutral plane in firm ground below the liquefiable layer will not settle significantly
Shallow foundation with deep liquefiable layer will largely undergo volumetric reconsolidation that can be estimated using 1D procedures
Shallow foundation with shallow liquefiable layer can undergo largely shear-induced movements that cannotbe estimated using available 1D procedures
Effective stress analyses based on good earthquake & soil characterization can provide useful insights
Investigating Liquefaction Effects in Christchurch, New ZealandSlide Number 2George F. SowersOUTLINENew ZealandSlide Number 6Slide Number 7Slide Number 8Slide Number 9Slide Number 10Slide Number 11Slide Number 12Slide Number 132010-2011 Canterbury EarthquakesSlide Number 15Slide Number 16 Canterbury EQs: Widespread LiquefactionSlide Number 18Repeated Liquefaction EventsSlide Number 20Liquefaction Effects in Christchurch Slide Number 22 Performance of House FoundationsSlide Number 24Slide Number 25Liquefaction in Christchurch CPT Investigations in Christchurch Slide Number 28CPT Investigations at Shallow Gravel Sites Slide Number 30Capturing Liquefaction Effects Slide Number 32Slide Number 33Slide Number 34Capturing Liquefaction Effects Liquefaction in Christchurch Liquefaction of Silty Sands Liquefaction of Silty Sands Observations of Liquefaction EjectaSlide Number 40Slide Number 41Slide Number 42Slide Number 43Slide Number 44Slide Number 45CTUC BuildingLiquefaction-Induced Differential Settlement Induces DistressCTUC BuildingCTUC Building: Christchurch EQCTUC Building SettlementCTUC Building: Sensitivity of ResultsSA BuildingLiquefaction-Induced Differential SettlementSlide Number 52Slide Number 53SA Building: Sensitivity of ResultsPWC BuildingLiquefaction-Induced Differential Settlement and TiltPWC BuildingSlide Number 57Slide Number 58Slide Number 59LIQUEFACTIONSlide Number 61LIQUEFACTION Factor of Safety (FS)LIQUEFACTION EFFECTSLiquefaction Flow Slides when qc1Ncs-Sr < 85Slide Number 65Slide Number 66