modelinggp of seismic response of thick soil sites and depth … response/hashash-mid... · 2020....
TRANSCRIPT
1
Modeling of Seismic Response of thick soil sitesg pand Depth dependent site coefficients
TRB COMMITTEE AFF50 - SEISMIC DESIGN OF BRIDGESGeo Seismic Concerns Subcommittee Meeting
23 January 2007 10:15 am – 12:00 pm, Marriott Hotel, Balcony Room D
Youssef Hashash ([email protected])In collaboration with Graduate Research Assistants:In collaboration with Graduate Research Assistants:
Chi-Chin Tsai, Camilo Phillips, Duhee Park (now @ Hanyang University)
University of Illinois at Urbana-Champaign
Mid-America Earthquake Center
University of Illinois at Urbana Champaign
2
Outline
• Backgroundg• Site response analysis of deep soil deposits• PSHA-NL: Integrated probabilistic seismic• PSHA-NL: Integrated probabilistic seismic
hazard analysis with non-linear site effectsNEHRP t l d th d d t it ffi i t• NEHRP style depth dependent site coefficients
• Conclusions
Mid-America Earthquake Center
3
Background: Mid-America Regional Issues
St.LouisMissouriMi i i i
E-W Section through Memphis
Cairo
Illinois
Sea level200 mMemphis
MississippiFlood Plain
New Madrid
Kentucky
Paleocene
1000 m
Recent and Plio-pleistocene
50 km0
Memphis
Tennessee
Mi i i
PaleoceneCretaceousPaleozoic RockLower Eocene
p
Middle and upper Eocene
MississippiArkansas Note vertical
scale exaggeration
Mid-America Earthquake Center
4
Modeling of site response of thick soil deposit- DEEPSOIL
-Nonlinear analysis (time domain): >Pressure dependent soil model>New Viscous Damping formulationNew Viscous Damping formulation
-Equivalent linear (Frequency domain):> Three types of complex shear modulus
-Graphical User Interface, User Base ~ 400 users
Mid-America Earthquake Center
http://www.uiuc.edu/~DEEPSOIL
5
Mississippi Embayment properties
• Dynamic properties from laboratory tests
– Laird and Stokoe (1993) & Chang 0.6
0.8
1
Gm
ax
(a)
23
456
7
7
( ) get al. (1992)
0 2 0 0 4 0 0 6 0 0 8 0 0 1 0 0 0
Vs
( m / s e c )
0
0.2
0.4G/G 65432
1
12 7
0
1 0 0
2 0 0
3 0 0
( a )00.0001 0.001 0.01 0.1 1
1: Proposed 3m2: Proposed 10.5m3: Proposed 26m4: Proposed 56.5m5: Proposed 114m
1: EPRI 3m2: EPRI 10.5m3: EPRI 26m4: EPRI 56.5m5: EPRI 114m
Shear strain, γ (%)
3 0 0
4 0 0
5 0 0
6 0 0
Dep
th (m
)
12
15
%) 1
(b) 12 3 4 5
6
5: Proposed 114m6: Proposed 228.5m7: Proposed 1000m
5: EPRI 114m6: EPRI 228.5m7: EPRI 1000m
7 0 0
8 0 0
9 0 0L o w l a n d s P r o f i l eU p l a n d s P r o f i l e
3
6
9
Dam
ping
ratio
(%
65
43
26
7
7
Mid-America Earthquake Center
1 0 0 0 Hardrock Vs=3000 m/sec 00.0001 0.001 0.01 0.1 1
Shear strain, γ (%)
6
Significance of overburden pressure dependency
1000 m Soil Column 100 m Soil Column
0.05
0.1
n(g
) Soil Column: 1000 m0.05
0.1
n (g
) Soil Column: 100 m
Amplificationof
Long Period -0.05
0
Acc
eler
atio
n
-0.05
0
Acc
eler
atio
n
Input Motion (after deconvolution):Yerba Buena
1000 m ColumnSi P i d 5 0
Waves-0.1
0 10 20 30 40Time (sec)
-0.10 10 20 30 40
Time (sec)
Loma Prieta Earthquake
0.1
Acc
eler
atio
n (g
) Site Period: 5.0 sec
Propagation of
High Frequency
0.1
Acc
eler
atio
n (g
)0.01 Input Motion (after deconvolution)
Pressure Dependent Model
Pressure Independent Model
Spec
tral A
Frequency Waves
0.01Sp
ectra
l A100 m ColumnSite Period: 0.9 sec
Mid-America Earthquake Center
0.01 0.1 1 10Period (sec) 0.01 0.1 1 10Period (sec)
7Integrated Probabilistic Seismic Hazard Analysis with Non-linear Site Effects (PSHA-NL)
Site
1D Nonlinear sitePath
Fault Surficial layers
1D Nonlinear site response analysis using DEEPSOIL
Source
Probabilistic seismic hazard analysis with ground motion generation Park & Hashash (2003)
Develop an integrated PSHA-NL tool that combines source/path effects + site effects: applied to Mid-America
Output1. A computational framework that can define Seismic Hazard / Representative ground motions
at any location in Upper Mississippi Embayment
Mid-America Earthquake Center
at any location in Upper Mississippi Embayment.2. Develop NEHRP style site coefficients
8
PSHA w/ Nonlinear Site Effects: PSHA-NL
Step 1 Select Site coordinates, site profiles, and dynamic properties.
Step 2 Perform PSHA at hard rockStep 2 Perform PSHA at hard rock.Choose number of simulations (N)
Output: a) Suite of hard rock motions, b) UHRS Point Source model & finite fault model
Step 3Propagate the hard rock motions
through B/C BoundaryOutput: UHRS
Step 4Propagate the hard rock motions through
site profiles using DEPPSOIL
Is UHRS close to USGS B/C hazard maps?No
Output: a) suite of site specific motions
Yes
hazard maps? Output: a) suite of site specific motions, b) UHRS
S 5
Mid-America Earthquake Center
Step 5Develop depth dependent site coefficients
9
PSHA-NL: I-Site selection
Site No
Ss (g) Sl (g) PGA(g)
Fa Fv
1 0.656 0.20 0.307 1.28 2
37
Carbondale
62 0.75 0.22 0.34 1.2 1.96
3 1.00 0.30 0.568 1.1 1.8
4 1.25 0.34 0.66 1.0 1.72
36
23
45 7
85 1.50 0.40 0.796 1.0 1.6
6 1.84 0.50 1.01 1.0 1.5
35Memphis
1
23
34
1
Mid-America Earthquake Center
-93 -92 -91 -90 -89 -8834
10PSHA-NL: III-PSHA ground motion generation Comparison of Uniform Hazard Response Spectra with USGS (B/C boundary)
Number of motions generated 9,000 – 10,000
Site 1 (2% 50 years exceedence UHRS)
0.6
0.7
0.8
0.9FINSIM w/o capSMSIM with cap2002map
Site 3 (2% 50 years exceedence UHRS)
1
1.2
1.4
FINSIM w/o capSMSIM with cap2002map
Site 5 (2% 50 years exceedence UHRS)
1 5
2
2.5FINSIM w/o capSMSIM w/o capSMSIM with cap2002map
0
0.1
0.2
0.3
0.4
0.5
0 01 0 1 1 10
Sa(
g)
0
0.2
0.4
0.6
0.8
0.01 0.1 1 10
Sa(
g)
0
0.5
1
1.5
0.01 0.1 1 10
Sa(
g)
0.01 0.1 1 10Period(sec)
Site 2 (2% 50 years exceedence UHRS)
0 70.80.9
1FINSIM w/o capSMSIM with cap2002map
0.01 0.1 1 10Period(sec)
Site 4 (2% 50 years exceedence UHRS)
1.4
1.6
1.8
FINSIM w/o capSMSIM with cap
Period(sec)
Site 6 (2% 50 years exceedence UHRS)
2 5
3
3.5FINSIM w/o capSMSIM w/o capSMSIM with cap
00.10.20.30.40.50.60.7
Sa(
g)
2002map
0
0.2
0.4
0.6
0.8
1
1.2
Sa(
g)
2002map
0
0.5
1
1.5
2
2.5
Sa(
g)
SMSIM with cap2002map
Mid-America Earthquake Center
00.01 0.1 1 10
Period(sec)
00.01 0.1 1 10
Period(sec)
00.01 0.1 1 10
Period(sec)
11
PSHA-NL: IV-Site effects & response
• 9000 generated rock motions are propagated through randomized soil profiles
0 200 400 600 800 1000 1200
0
Vs (m/s)
(b)
– 30 profiles
Shear Wave Velocity Dynamic Soil Properties Weight 200
Profiles (No. of Simulation)
ME properties 0.75w (22) Uplands 400
(m)
EPRI properties 0.25w (8)
ME properties 0.75w (22) Lowlands
EPRI ti 0 25 (8)
600
Dep
th
EPRI properties 0.25w (8) 800
UplandsMean - 1standard deviationMean + 1standard deviationRandomized profile
Mid-America Earthquake Center
1000
Randomized profile
0 200 400 600 800 1000 1200
12
PSHA-NL: IV-Site effects & response -Depth dependent UHRS
2Site D (NEHRP)
30
2 30 m100 m200 m300 m
1.5
30 m
100 m200 m
300 m
500 m1.5
300 m500 m1000 m30m Amp100m Amp200m Amp300m Amp500 m Amp1000m Amp
1
PSA
(g)
1000 m
1
PS
A (g
)
1000m AmpNEHRP Site D
0.50.5
00.01 0.1 1 10
Period (sec)
00.01 0.1 1 10
Period (sec)
Mid-America Earthquake Center
Period (sec)
Site 6Period (sec)
13PSHA-NL: V-Simplified NEHRP style depth dependent Site Factors
Uplands Profile
0.7 0.8 0.9 1 1.1 1.2 1.3 1.4
0
Fa
1 1.5 2 2.5 3 3.5Fv
200
400
h (m
)
600
Dep
th
Ss=1.0gSs=0.75g
Ss>=1.25gS
l=0.4g
Sl=0.3g
S >=0 5g
800 PSHA-NL (PS)
PSHA-NL (FF)
NEHRP
Sl>=0.5g
Mid-America Earthquake Center
1000
NEHRP
14Incorporate updated Hazard maps with depth dependent site factors:2% in 50 year hazard map of PGA in ME
37
Carbondale
37
Carbondale(a) USGS B/C boundary (b) With NEHRP Class Site D
35
36
Memphis35
36
Memphis
Unit: g
1.4
1.6
CarbondaleCarbondale
-93 -92 -91 -90 -89 -8834
-93 -92 -91 -90 -89 -8834
(d) PSHA NL(FF) using 0 6
0.8
1
1.2
atitu
de
36
37
36
37(d) PSHA-NL(FF) using spectrum ratio
(c) PSHA-NL(FF) using proposed site coefficients
0
0.2
0.4
0.6
La
Memphis3535
Memphis
Mid-America Earthquake Center
-93 -92 -91 -90 -89 -8834
-93 -92 -91 -90 -89 -8834
Longitude
15Incorporate updated Hazard maps with depth dependent site factors:2% in 50 year hazard map of 0.2 Sec SA in ME
37
Carbondale
37
Carbondale(a) USGS B/C boundary (b) With NEHRP Class Site D
35
36
Memphis35
36
Memphis
Unit: g
3.2
3.6
-93 -92 -91 -90 -89 -8834
CarbondaleCarbondale-93 -92 -91 -90 -89 -88
34
1.6
2
2.4
2.8
Latit
ude
36
37
36
37
Ca bo da e(d) PSHA-NL(FF) using spectrum ratio
(c) PSHA-NL(FF) using proposed site coefficient
0
0.4
0.8
1.2
Memphis3535
Memphis
Mid-America Earthquake Center-93 -92 -91 -90 -89 -88
34-93 -92 -91 -90 -89 -88
34
Longitude
16Incorporate updated Hazard maps with depth dependent site factors:2% in 50 year hazard map of 1.0 sec SA in ME
37
Carbondale
37
Carbondale(a) USGS B/C boundary (b) With NEHRP Class Site D
35
36
Memphis 35
36
Memphis
Uint: g
2 1
2.4
2.7
-93 -92 -91 -90 -89 -8834
CarbondaleCarbondale
-93 -92 -91 -90 -89 -8834
(d) PSHA NL(FF) using(c) PSHA NL(FF) using 0 9
1.2
1.5
1.8
2.1
atitu
de
36
37
36
37(d) PSHA-NL(FF) using spectrum ratio
(c) PSHA-NL(FF) using proposed site coefficient
0
0.3
0.6
0.9La
Memphis3535
Memphis
Mid-America Earthquake Center
-93 -92 -91 -90 -89 -8834
-93 -92 -91 -90 -89 -8834
Longitude
17
Conclusions
• NEHRP site factors do not account for effect of d d itdeep deposits.
• A possible remedy is the inclusion of depth dependent site factors.
• For important bridges/structures site specific p g panalyses are needed
• DEEPSOILDEEPSOIL …..
Mid-America Earthquake Center