Integra)ng Modal Analysis and Seismic
Interferometry for full structural dynamic
response: Gio:o’s Bell Tower.
Giorgio Lacanna
1, Renato Lancello:a
2, Maurizio Ripepe
1
1 Università di Firenze 2 Politecnico di Torino
Ambient Vibra)on Test
Classic Method Opera)onal Modal Analysis:
Ø OMA is passive seismic tool for Structural frequencies, Modal shapes and Damping iden)fica)on. We applied the Enhanced Frequency Domain Decomposi)on (EFDD)
Ø Calibrate Numerical Model
Ø Structural Health Monitoring (SHM) purposes.
Ambient Vibra)on Test is commonly used to iden)fy the dynamic response of the Building.
Seismic Interferometry is performed on the same seismic data:
Ø IRFs (Impulsive Response Func)on) allow to es)mate seismic wave velocity (Vs and Vp).
Ø Vs a new parameter for SHM (Velocity is less affect by SSI than frequency).
Ø Seismic Wave analysis integrated with the structural frequencies gives
Dynamic Monitoring
10 Seismic Sta)ons equipped:
•
Broadband 3-‐component
seismometrs (Lennartz 5s,
Guralp 10s, Guralp30s)
•
Digi)zer 24 bit (Guralp, CMG-‐
DM24) sampling at 100Hz
•
Synchroniza)on using GPS
Automa)c Iden)fica)on Modal Parameters – EFDD
Assump)on -‐-‐> Modal Shapes are sta)onary for 3 hours
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MODAL
COHERENCE
Rainieri & Fabrocino, 2010 Lacanna et al, 2016
Mean
C
Standard devia)onC
First singular values6 Modal Frequencies Iden)fied
0.623
0.647
2.543
3.081
3.156
5.731
First and Second Modal Shapes
1° Longitudinal -‐ 0.623 Hz 2° Transversal -‐ 0.647 Hz
+
=
1°+2° Shapes Mode
51°N
141°N
1° and 2° Shapes Mode moves together along the diagonal of the square plan of Gio:o’s Bell Tower
The two first Shapes Mode are coupled and resul)ng in circular movement slightly eccentric in North-‐South direc)on
III° -‐IV° -‐V °-‐ VI° Modal Shapes
III° – 2.543 Hz IV° – 3.081 Hz V° – 3.156 Hz
4° and 5° Shapes Mode as the first two modes moves approximately
to the diagonal of the square plan of Gio:o’s Bell Tower
Automa)c Tracking of Modal frequencies
Frequency (Hz)
Mean Frequency (Hz) Min (%) Frequency (Hz) Max (%)
0.623 0.618 (0.76) 0.628 (0.80)
0.647 0.642 (0.81) 0.652 (0.73)
2.543 2.520 (0.90) 2.573 (1.18)
3.081 3.052 (0.93) 3.105 (0.79)
3.156 3.134 (0.68) 3.174 (0.57)
A posi)ve correla)on is found between the 6 modal frequencies
and temperature.
Frequency changes ≤ 1.1 %
The Modal frequencies are detected automa)cally for 36 hours and compared with temperature
Flexible structure
The building horizontal displacement is a sum of three terms
Transla=on Rota=on
Soil founda=on Deforma=on of Building
(Luco 1987, Todorovska 2008)
The modal frequencies extracted with OMA (f0) is related to the mechanical
proper)es of the building but is also affected by the soil-‐structure interac)on For Flexible structure ffixed is given by basic equa)on:
=4.26 m Iner=a radius cross-‐sec=on
=84 m Eleva=on of the building Compressional P-‐wave velocity
the seismic velocity
is es)mated by interferomety
Seismic Interferometry
Evaluates the IRFs through the deconvolu)on of the signals:
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∗ (!)
!!"#(!)
!
+ !
urefà Sta=on locate to the Top
Sneider & Safak, BSSA 2006
2040 m/s
North
Sta=ons Sta=ons South
2040 m/s
R
2=0.99
=0.70 Hz
The velocity is es)mated from the slope of the travel )me
Using least square fit
Rocking Frequency
OMA tecnique Interferometry Geometrical proper)es
ROCKING FREQUENCY:
18 m 7 mVs =380 m/s
The soil structure interac)on reduces the fixed-‐base frequency by 8% and it is expected by considering the high Vs=380 m/s of the soil founda)on
Rocking S)ffnnes
Results
Ø
AutomaLc idenLficaLon EFDD technique on GioRo’ Bell Tower:
Iden=fies 6 main frequencies and associated modal shapesØ The 1° -‐ 2° modes move to the diagonal of the square plan
Seismic Interferometry technique on GioRo’ Bell Tower:
Ø Seismic velocity Vp=2040 m/s à Fixed base frequency
IntegraLng results of the two techniques
Ø Provides detail informa=on on the degree of soil-‐structure interac=on.
Ø The rocking frequency is consistent with the geotechnical proper=es and it reduces the fixed base frequency of 10%
Ø The value fR=1.36 Hz can be used to validate analy=cal rela=onship to compute
the rocking s=ffness for advanced seismic analysis
Conclusions
The full structural dynamic iden)fica)on (OMA-‐ Interferometry) shows a Weak contribu)on of soil-‐structure interac)on