Quantifying Mainshock Aftershock Collapse Probabilities for Woodframe Buildings. John W. van de Lindt and Negar Nazari The University of Alabama

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Quantifying Mainshock Aftershock Collapse Probabilities for Woodframe Buildings John W. van de Lindt and Negar Nazari The University of Alabama Yue Li Michigan Technological University Aftershocks Great Tohoku earthquake 2011 M7.9 less than an hour later Chile earthquake 2010 M7.2 12 days later New Zealand M6.3 more than 4 months later Indonesia yesterday M8.2 an hour or two later Energy content can differ Location differs, triggering. J. van de Lindt J. van de Lindt 1

Some of the challenges Performance-based earthquake engineering framework - conceptual Yeo and Cornell (2005) Occurrence time very difficult to predict Markov process models Location very difficult to predict Aftershocks do collapse buildings Gas station following 1999 Chi-Chi Taiwan EQ (Lew et al 2000) 9-Story RC building following 1995 Kobe EQ (Whittaker et al, 1997). 2011 Christchurch EQ Benchmark Structure 1. Run at NEES@buffalo testing facility with steel frame attaching two shake tables, allowing fullsize building to be tested 2. Five ground motion levels involving scaling of two recorded earthquake ground motions 3. Five test phases (configurations) 4. Testing lead by A. Filiatrault and students 2

Numerical Modeling Story diaphragm behaves like a rigid body in 3 D space Inter story drift is a combination of contributions from shear deformation and global rotation Vertical stiffness element: Support and hold down 3

Comparison of global story hysteresis Wood Building : NEESWood Benchmark Test 4

Using Data Available in NEEShub for Model Calibration Collapse Model Calibration SAWS type hysteretic spring (CUREE model) The 10 parameter model widely accepted as a reasonable model load resistance behavior of wood shearwall components. Calibrated to match the larger hysteretic loops, then adjusted for collapse point 5

Model Calibration(cont d) Equivalent SDOF model 28 shear wall spring model being used currently, but not in this study/presentation Procedure to Quantify the Effect of Aftershocks STEP1: IDA using calibrated model for earthquake records (mainshock) STEP2: Determining collapse spectral acceleration and corresponding recordspecific collapse drift based on 20% rule, i.e. bounds. STEP3: Develop mainshock aftershock record combinations using psi*mainshock + C*aftershock. STEP5: identify distribution of psi values from step4 STEP4: Run mainshock aftershock combinations to determine smallest scaling of mainshock + C*aftershock that will collapse structure. Aftershock collapse is based on collapse drift for that earthquake from step 2. 6

STEP1: IDA using calibrated model for mainshock only Identify the collapse drift specific to each earthquake. Assumption This EQ-specific collapse drift remains applicable for the same earthquake at lower intensity STEP2: Determining collapse bounds and corresponding drift based on 20% slope in IDA curve for each mainshock Sa(g) drift(%) EQ Lower value Average Upper value Lower value Average Upper value 1 0.9 1.05 1.2 4.312405093 7.8081863 11.30396759 2 1.1 1.15 1.2 4.278914352 6.1104479 7.941981481 16 1.3 1.35 1.4 3.481387963 4.4651338 5.44887963 8 1.4 1.45 1.5 11.43312037 13.983766 16.53441204 6 1.6 1.65 1.7 1.850526389 2.6008704 3.351214352 11 1.6 1.65 1.7 11.855375 14.680359 17.50534259 13 1.6 1.65 1.7 4.478803704 6.5693 8.659796296 5 1.7 1.8 1.9 11.01750926 12.967 14.91649074 19 1.7 1.8 1.9 12.88885648 14.102155 15.3154537 14 1.9 1.95 2 3.733105556 4.6694509 5.605796296 18 1.9 1.95 2 8.380111111 10.861847 13.34358333 7 2 2.05 2.1 8.657569444 10.187428 11.71728704 9 2 2.05 2.1 7.88850463 9.7581968 11.62788889 12 2 2.05 2.1 9.377328704 10.457275 11.53722222 17 2.1 2.15 2.2 5.787310185 6.586794 7.386277778 15 2.2 2.25 2.3 4.89875463 6.2557755 7.612796296 21 2.2 2.25 2.3 7.380824074 10.129674 12.87852315 3 2.3 2.35 2.4 6.020287037 8.467419 10.91455093 4 2.4 2.45 2.5 11.15874537 13.059424 14.96010185 20 2.5 2.5 2.5 8.190814815 8.1908148 8.190814815 10 2.5 2.5 2.5 4.046585 4.046585 4.046585 22 2.5 2.5 2.5 3.893768056 3.8937681 3.893768056 7

Collapse Drifts from IDA s Reasonable? East Wall West Wall Collapse Drifts from IDA s Reasonable? 5.4% 6% 8

Approximate Validation Mean = 8.6% from the numerical system model Isolated garage wall achieved 6%. Approximate validation Dependence on ground motion neglected. Sa(g) drift(%) EQ Lower value Average Upper value Lower value Average Upper value 1 0.9 1.05 1.2 4.312405093 7.8081863 11.30396759 2 1.1 1.15 1.2 4.278914352 6.1104479 7.941981481 16 1.3 1.35 1.4 3.481387963 4.4651338 5.44887963 8 1.4 1.45 1.5 11.43312037 13.983766 16.53441204 6 1.6 1.65 1.7 1.850526389 2.6008704 3.351214352 11 1.6 1.65 1.7 11.855375 14.680359 17.50534259 13 1.6 1.65 1.7 4.478803704 6.5693 8.659796296 5 1.7 1.8 1.9 11.01750926 12.967 14.91649074 19 1.7 1.8 1.9 12.88885648 14.102155 15.3154537 14 1.9 1.95 2 3.733105556 4.6694509 5.605796296 18 1.9 1.95 2 8.380111111 10.861847 13.34358333 7 2 2.05 2.1 8.657569444 10.187428 11.71728704 9 2 2.05 2.1 7.88850463 9.7581968 11.62788889 12 2 2.05 2.1 9.377328704 10.457275 11.53722222 17 2.1 2.15 2.2 5.787310185 6.586794 7.386277778 15 2.2 2.25 2.3 4.89875463 6.2557755 7.612796296 21 2.2 2.25 2.3 7.380824074 10.129674 12.87852315 3 2.3 2.35 2.4 6.020287037 8.467419 10.91455093 4 2.4 2.45 2.5 11.15874537 13.059424 14.96010185 20 2.5 2.5 2.5 8.190814815 8.1908148 8.190814815 10 2.5 2.5 2.5 4.046585 4.046585 4.046585 22 2.5 2.5 2.5 3.893768056 3.8937681 3.893768056 Northridge 1994 Mainshock Collapse 1.05g Psi = 1.0 With Aftershock Record @ 0.8S mainshock a Loma Prieta 1989 0.97g 0.92 Kocaeli, Turkey 1999 1.03g 0.98 Northridge 1994 0.88g 0.85 Chi Chi, Taiwan 1999 0.98g 0.93 9

Imperial Valley 1979 Mainshock Collapse 1.8g Psi = 1.0 With Aftershock Record @ 0.8S mainshock a Kocaeli, Turkey 1999 1.37g 0.76 Superstition Hills 1987 1.43g 0.79 Kocaeli, Turkey 1999 1.51g 0.84 Imperial Valley 1979 1.00g 0.56 Some next steps Correlation of psi and C Application of recurrence relationship for occurrence probability of aftershocks Inclusion of spatial statistics Collapse obviously important; Correlation of damage states for 2 nd gen PBEE Generalize with a portfolio of representative buildings Steel frame buildings collaborative work at MTU (Y. Li, PI) 10

Thank you! This material is based upon work supported by the National Science Foundation. Any opinions, findings, and conclusions or recommendations expressed in this material are those of the investigators and do not necessarily reflect the views of the National Science Foundation. My Contact Info: John W. van de Lindt jwvandelindt@eng.ua.edu Foot bridge in downtown Christchurch J. van de Lindt 11