supervisors: julie régnier, etienne bertrand, and ...€¦ · paper id: 11582 conclusions the...
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Paper ID: 11582Paper ID: 11582
Supervisors: Julie Régnier, Etienne Bertrand, and
Françoise Courboulex
David Alejandro Castro Cruz
1
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Paper ID: 11582Paper ID: 11582
Context2
Non-linear effects
How the non linear behavior affects a ground motion?
Non-linear
effects
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Paper ID: 11582Paper ID: 11582
Data network
The Kik-Net data, Japan (Aoi, et al., 2004) is used in this
study. This data set has two stations by site, one at
surface and another in downhole.
3
650 sites
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Paper ID: 11582Paper ID: 11582
Site effects
We computed an empirical transfer function (Borehole
Spectral Ratio - BSR) to quantify the site effects.
4
Fourier Spectrum at
surface
Fourier Spectrum on
bedrock
𝐵𝑆𝑅(𝑓) =|𝐸𝑊𝑠𝑢𝑟𝑓|
2 + |𝑁𝑆𝑠𝑢𝑟𝑓|2
|𝐸𝑊𝑑𝑒𝑝𝑡ℎ|2 + |𝑁𝑆𝑑𝑒𝑝𝑡ℎ|
2
Station: IBRH11
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Paper ID: 11582Paper ID: 11582
Non-Linear effects
We computed an empirical transfer function (Borehole
Spectral Ratio - BSR) to quantify the site effects.
5
Fourier Spectrum at
surface
Fourier Spectrum on
bedrock
𝐵𝑆𝑅(𝑓) =|𝐸𝑊𝑠𝑢𝑟𝑓|
2 + |𝑁𝑆𝑠𝑢𝑟𝑓|2
|𝐸𝑊𝑑𝑒𝑝𝑡ℎ|2 + |𝑁𝑆𝑑𝑒𝑝𝑡ℎ|
2
Station: IBRH11
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Paper ID: 11582Paper ID: 11582
Non-Linear effects
We computed an empirical transfer function (Borehole
Spectral Ratio - BSR) to quantify the site effects.
6
Fourier Spectrum at
surface
Fourier Spectrum on
bedrock
𝐵𝑆𝑅(𝑓) =|𝐸𝑊𝑠𝑢𝑟𝑓|
2 + |𝑁𝑆𝑠𝑢𝑟𝑓|2
|𝐸𝑊𝑑𝑒𝑝𝑡ℎ|2 + |𝑁𝑆𝑑𝑒𝑝𝑡ℎ|
2
Station: IBRH11
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Paper ID: 11582Paper ID: 11582
Non-Linear effects7
Station: IBRH11
Shift to lower
frequencies on
the amplification
Decrease of the
amplification
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Paper ID: 11582Paper ID: 11582
Frequency shift parameter (fsp)8
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Paper ID: 11582Paper ID: 11582
Frequency shift parameter (fsp)9
𝐵𝑆𝑅𝑙𝑖𝑛𝑒𝑎𝑟 = ൗ[ σ𝑖=1𝑛 𝐵𝑆𝑅𝑤𝑒𝑎𝑘 𝑖 𝑓 ]
𝑛
BSRlinear is the average from the BSRs from weak ground
motions
Station: IBRH11
Fourier Spectrum at
surface
Fourier Spectrum on
bedrock
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Paper ID: 11582Paper ID: 11582
Frequency shift parameter (fsp)10
Frequency Shift Parameter (fsp): It measures the
logarithmic ten frequency lag with respect to BSRlinear
𝐵𝑆𝑅𝑙𝑖𝑛𝑒𝑎𝑟 𝑓 𝑓𝑠𝑝 → 𝐵𝑆𝑅
𝑓𝑠𝑝 < 1 → Shift to lower
frequencies
𝑓𝑠𝑝 = 1 → No shift
𝑓𝑠𝑝 > 1 → Shift to higher
frequencies
𝑓𝑠𝑝
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Paper ID: 11582Paper ID: 11582
Frequency shift parameter (fsp)11
𝐵𝑆𝑅𝑙𝑖𝑛𝑒𝑎𝑟 𝑓 𝑓𝑠𝑝 → 𝐵𝑆𝑅
fsp value is related with the intensity of the ground
motion.
𝑓𝑠𝑝 =1
1 +𝑃𝐺𝐴𝑑𝑜𝑤𝑛ℎ𝑜𝑙𝑒
𝑃𝐺𝐴𝑟𝑒𝑓𝑑𝑜𝑤𝑛ℎ𝑜𝑙𝑒
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Paper ID: 11582Paper ID: 11582
Frequency shift parameter (fsp)12
fsp curves are related with the site:
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Paper ID: 11582Paper ID: 11582
Frequency shift parameter (fsp)13
Comparison between 466 stations
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Paper ID: 11582Paper ID: 11582
Frequency shift parameter (fsp)14
Comparison between 466 stations
Vs30=521 m/s
Vs30=399 m/s
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Paper ID: 11582Paper ID: 11582
Frequency shift parameter (fsp)15
Comparison between 466 stations
Vs30=241 m/s
Vs30=204 m/s
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Paper ID: 11582Paper ID: 11582
fsp relationship with decay of
stiffness (G/Gmax)16
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Paper ID: 11582Paper ID: 11582
Frequency shift parameter (fsp)17
fsp in equivalent linear analysis
𝑮
𝑮𝒍𝒊𝒏𝒆𝒂𝒓≈ 𝒇𝒔𝒑
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Paper ID: 11582Paper ID: 11582
Frequency shift parameter (fsp)18
PGV/Vs30 as proxy
of strain (Chandra
et al., 2015) (Idriss,
2011)
fsp is related with
the loss of stiffness
Data from PRENOLIN Project (Régnier et al. 2018)
Comparison with laboratory data:
Station: KSRH10
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Paper ID: 11582Paper ID: 11582
Conclusions
The frequency shift parameter (fsp) can quantify the
influence of the non-linearity of the soil in a ground
motion.
fps curves are linked with the site characteristic.
The fsp curves show a similar trend with the shear
modulus reduction curves.
19
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ευχαριστώ πολύ
Thank you
I will be attentive to any question
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Frequency shift parameter (fsp)21
Comparison with different stations
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fsp curves22