NATIONAL GEOSPATIAL-INTELLIGENCE AGENCY NGA DNC NGA DNC DNC Bulletin Improvements.
Directionality of ground motions in the NGA-West2 database• NGA-West2 database • We used subsets...
Transcript of Directionality of ground motions in the NGA-West2 database• NGA-West2 database • We used subsets...
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Directionality of ground motions in the NGA-West2 database
Shrey K. Shahi & Jack W. Baker Stanford University
Directionality Working Group: Brian Chiou, Nicolas Luco, Mahmoud Hachem, Tom Shantz, Paul Somerville, Paul Spudich, Jon Stewart, Badie Rowshandel
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Motivation
• “Maximum-direction” spectral accelerations have received increasing attention in the engineering community in recent years (e.g., 2009 NEHRP Provisions)
• NGA-West2 models will provide predictions of “SaRotD50” spectra
• We provide a modification to convert those predictions to maximum-direction spectra
• We also report on orientations of the maximum direction motions, and suggest how to use these models for engineering analysis
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3 Example 1-second oscillator responses to multi-component motions
HWA031 recording from Chi-Chi-04, 1999 earthquake
Gilroy Array #6 recording from Morgan Hill,1984 earthquake
Sa(1s) / SaRotD100(1s) Displacement / Maximum displacement SaRotD100 orientation
SaRotD0 orientation
SaRotD50 orientation
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Model formulation for SaRotD100 at a specified period
100100 50
50
100 100 50 50
ln ln( / ) ln( )
RotDRotD RotD
RotD
RotD RotD RotD RotD
SaSa SaSa
Sa Sa Sa Sa
=
= +
This study Primary GMPE
5 300 ( , , ,..l .)n( )RotD Sf M R VSa η ε= + +100 50ln( / ) ' 'RotD RotD aSa Sa η ε= + +
Complex prediction Simple prediction (constant?)
Independent of primary GMPE
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Results to discuss today
• SaRotD100 /SaRotD50 ratios • Orientation of SaRotD100 relative
to strike
• Difference in orientation of SaRotD100(T1) and SaRotD100(T2)
• Change in Sa(T) at angles away from the SaRotD100 orientation
• Amplitude of Sa(T) in a specified direction
T’ = 3 s
T* = 1.5 s
Oscillator responses to 1979 Imperial Valley-06, El Centro Differential Array recording
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Data set
• NGA-West2 database
• We used subsets of the data chosen by the modelers (as of 11/1/2011), to ensure use of appropriate data and to be compatible with NGA West 2 models for SaRotD50
• Sa values computed for – 5% damping only – 21 periods – All orientations in 1º
increments
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Histograms of SaRotD100/SaRotD50
T = 0.2 s T = 1.0 s
Num
ber
of g
roun
d m
otio
ns
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Median SaRotD100/SaGMRotI50 ratios, versus previous models
There is a clear period dependence in these ratios
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These ratios differ from the NEHRP Provisions ratios
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Variation in SaRotD100/SaGMRotI50 with closest distance (Rrup)?
T = 0.2 s T = 1 s
Other variables (M, directivity parameters) had less strong effects
Rrup (km) Rrup (km)
Rrup
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Model with Rrup dependence
100 50 0 1ln( / ) ' '·( 60)Rot rupD RotD a a RSa Sa η ε= + ++ −
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Standard deviations (example numbers for Sa(1s))
100 100 50 50ln ln( / ) ln( )RotD RotD RotD RotDSa Sa Sa Sa= +
This study Primary GMPE
50 30ln( ) ( , , ,...)RotD SSa f M R V η ε= + +100 50ln( / ) ' 'RotD RotDSa Sa a η ε= + +
This study: Campbell Bozorgnia
(2008) NGA:
σ = 0.623 σ’ = 0.629
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Orientation of SaRotD100 (using α as angle to strike parallel)
Site
Fault rupture
α Strike parallel orientation
• Dependence of α on various parameters was studied
• A parametric model to predict the distribution of α is proposed
Oscillator responses to 1979 Imperial Valley-06, El Centro Differential Array recording
T’ = 3 s
T* = 1.5 s
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Dependence of α on M and Rrup
Rrup bins
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Distribution of α for varying T, with Rrup between 0 and 5 km
Apparent division at 0.5 or 1 second
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Observations regarding distributions of α
Some dependence on distance and period (consistent with previous work)
– The distribution tends towards fault normal for R < 5 km and T ≥ 0.5 s (This is not the same as saying α is always fault normal)
– The distribution is apparently uniform otherwise
No obvious dependence on magnitude, directivity parameters, etc.
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Other models for directionality
α
The direction of SaRotD100(T) will vary with period
1. By how much will the azimuths of SaRotD100(T*) and SaRotD100(T’) vary?
2. If we identify a target SaRotD100 at one period (T*), what will the spectral value be at some other period (T’)?
T’ = 3 s
T* = 1.5 s
Oscillator responses to 1979 Imperial Valley-06, El Centro Differential Array recording
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Distribution of α*-α’ for various T* and T’
T* = 1 s, T’ = 2 s T* = 0.1 s, T’ = 0.2 s
T* = 1 s, T’ = 5 s T* = 0.1 s, T’ = 0.5 s
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19 Median ratio of Saφ/SaRotD50, as a function of distance from SaRotD100 orientation
Geo
met
ric
mea
n Saφ/S
a Rot
D50
Example 1s response case:
φ = Angle relative to SaRotD100 (degrees)
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Individual ground motion example
TCU076 station, 1999 Chi-Chi earthquake Rrup = 3 km, M = 7.6
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Example predictions using above results
M = 7, Rclst = 2.5 km, VS30 = 760 m/s
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Conclusions
• Observed ratios of SaRotD100/ SaRotD50 are consistent with previous studies – Dependent on period and (weakly) on distance – No clear dependence on other properties (magnitude, directivity-related parameters)
• Orientations of SaRotD100 appear to be uniform beyond 5 km closest distance – Within 5 km and for T ≥ 0.5s, there is a tendency towards fault-normal orientation
• Orientations of SaRotD100 vary with period, for a given ground motion, which complicates target spectrum calculation and ground motion selection
• We aim to address that problem by providing models for: – Difference in orientation of SaRotD100 at two periods – Deviation from SaRotD100 as a function of the above orientation difference
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Thanks to the project technical review team:
• Brian Chiou • Nicolas Luco • Mahmoud Hachem • Tom Shantz • Paul Somerville • Paul Spudich • Jon Stewart • Badie Rowshandel
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Fault normal spectra versus SaRotD50
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Is SaRotD100 = SaFN for directivity ground motions?
• Each ground motion in the NGA West 2 database classified as pulse or non-pulse
– Improved pulse-classification algorithm (Shahi and Baker) – Documentation in progress
• Source-site geometry used to manually identify Pulse-like ground motions caused by directivity
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SaRotD100 orientation for directivity ground motions
Data pooled from 21 periods
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SaRotD100 orientation for directivity ground motions
Data for period closest to Tp
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Effect of Chi-Chi
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Effect of changing the dataset
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Any variation in this ratio with distance (M)?
T = 7.5 s T = 3 s
T = 0.1 s T = 1 s
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Any variation in this ratio with s? (Strike slip only)
T = 7.5 s T = 3 s
T = 0.1 s T = 1 s
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Any variation in this ratio with θ? (Strike slip only) T = 0.1 s T = 1 s
T = 3 s T = 7.5 s
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Any variation in this ratio with D? (Non-strike-slip only)
T = 7.5 s T = 3 s
T = 0.1 s T = 1 s
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Regression analysis to evaluate significance of above parameters
• Both forward and backward step-wise regression was used to select statistically significant parameters
• Some dependence on M and R (depends upon period)
• Some dependence on directivity parameters at higher periods • Our recommendation : a simple model dependent on R only
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Distribution of α for different M-R bins
T = 1 s
Distance range (km) M
agnitude range
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Distribution of α for different M-R bins
Data pooled from all periods
Distance range (km) M
agnitude range
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Distribution of α for different R bins
Data pooled from all periods
Distance range (km)
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Models for α? Two options:
1. Parametric model for distribution of α (i.e., equation for a probability distribution) – Linearly-varying distribution of α for R < 5 km (function of T) – Uniform distribution for R > 5 km
2. Just report histogram values at different T for R < 5 km – Simpler, but hard to do calculations with
R < 5 km, T = 0.1s R < 5 km, T = 7.5s
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Direction of RotD100 with θ
T = 3 s
T = 0.1 s T = 1 s
T = 7.5 s
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Zooming in towards high θ
T = 3 s
T = 0.1 s T = 1 s
T = 7.5 s
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Only records with high amplification
T = 3 s
T = 0.1 s T = 1 s
T = 7.5 s
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• When θ is high some Sa,RotD100 values are found in fault parallel orientation. This may be due to the radiation patterns
• Due to low sample size and presence of randomness we cant make confident conclusions.
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Distribution of α*-α’ for different T*,T’ T* = 1 s, T’ = 2 s T* = 0.1 s, T’ = 0.2 s
T* = 1 s, T’ = 5 s T* = 0.1 s, T’ = 0.5 s
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45 Median ratio of Sa(Φ)/SaRotD50, as a function of distance from SaRotD100 orientation