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Frontiers of Structural and Civil Engineering

ISSN 2095-2430

ISSN 2095-2449(Online)

CN 10-1023/X

Postal Subscription Code 80-968

2018 Impact Factor: 1.272

Front Struc Civil Eng    0, Vol. Issue () : 69-82    https://doi.org/10.1007/s11709-014-0231-4
CASE STUDY
Evaluation of site response characteristic using nonlinear method (Case study: Babol, Iran)
Asskar Janalizadeh CHOOBBASTI, Sadegh REZAEI, Farzad FARROKHZAD(), Pedram Haidarzaeh AZAR
Department of Civil Engineering, Babol University of Technology, Babol, Mazandaran 484, Iran
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Abstract

In this the present study, an attempt has been made to evaluate the seismic hazard considering local site effects by carrying out detailed geotechnical site characterization in Babol, Iran. Use of geotechnical data and synthesis of drilling data extracted from the Babol’s subsurface database have enabled authors to determine the geotechnical properties of each site. These data are consisted of twenty five boreholes up to depth of 40 m. Based on the obtained data from geotechnical investigation the study area is divided to five zones. Dynamic analysis was performed in time domain, using fully nonlinear model by PLAXIS. A series of analysis in the study area showed the site period, ranging from 0.4 to 0.8 s. Finally the obtained response spectra from fully nonlinear method were compared with site response spectra of Iran’s 2800 (earthquake) code.

Keywords fully nonlinear method      site effect      dynamic analysis      response spectra     
Corresponding Author(s): FARROKHZAD Farzad,Email:FarzadFarokhzad@yahoo.com   
Issue Date: 05 March 2014
 Cite this article:   
Asskar Janalizadeh CHOOBBASTI,Sadegh REZAEI,Farzad FARROKHZAD, et al. Evaluation of site response characteristic using nonlinear method (Case study: Babol, Iran)[J]. Front Struc Civil Eng, 0, (): 69-82.
 URL:  
https://academic.hep.com.cn/fsce/EN/10.1007/s11709-014-0231-4
https://academic.hep.com.cn/fsce/EN/Y0/V/I/69
Fig.1  Study area and zonation map
distance to fault/kmmagnitude/Mcountrystation
225.19USAAnza (Horse Canyon)
107.62Taiwan,ChinaChi-Chi
236.19USAMorgan Hill
126.93USALoma Prieta
Tab.1  Specifications of strong motions used for near field analysis
distance to fault/kmmagnitude/Mcountrystation
706.20USSRGeorgia
556.50ItalyFriuli
616.50USABorrego Mountain
505.19USAAnza (Horse Canyon)
Tab.2  Specifications of strong motions used for middle field analysis
distance to fault/kmmagnitude/Mcountrystation
88.66.50USABorrego mountain
68.26.50USABorrego mountain
71.57.62Taiwan,ChinaChi-Chi
1107.62Taiwan,ChinaChi-Chi
Tab.3  Specifications of strong motions used for far field analysis
Fig.2  Acceleration time history of near field earthquakes
Fig.3  Acceleration time history of middle field earthquakes
Fig.4  Acceleration time history of far field earthquakes
Fig.5  Geometry model, boundary conditions and finite element mesh
Fig.6  Faults of study area
Fig.7  Location of geotechnical boreholes
layers1234
φ/(o)030034
C/(kg·cm-1)0.7000.500
γwet/(g·cm-3)1.972.011.871.98
γd/(g·cm-3)1.531.561.661.56
ω/%28.7617.524.524
LL/%5441
PL/%2522
E/(kg·cm-2)400300400280
ν0.350.300.350.30
Tab.4  Material properties for zone A (layers 1-4)
Fig.8  Comparison of normalized response spectra of zone A. (a) Near field; (b) middle field; (c) far field
layers123
φ/(o)0357
C/(kg·cm-1)1.1700.26
γwet/(g·cm-3)1.902.011.92
γd/(g·cm-3)1.401.561.46
ω/%3427.531
LL/%3243
PL/%1617
E/(kg·cm-2)400100400
ν0.250.300.25
Tab.5  Material properties for zone B (layers 1-3)
Fig.9  Comparison of normalized response spectra of zone B. (a) Near field; (b) middle field; (c) far field
layers123
φ/(o)7325
C/(kg·cm-1)0.280.060.16
γwet/(g·cm-3)1.971.971.97
γd/(g·cm-3)1.501.501.53
ω/%263031
LL/%3740
PL/%2020
E/(kg·cm-2)90100400
ν0.250.300.25
Tab.6  Material properties for zone C (layers 1-3)
Fig.10  Comparison of normalized response spectra of zone C. (a) Near field; (b) middle field; (c) far field
layers123
φ/(o)0380
C/(kg·cm-1)1.1300.25
γwet/(g·cm-3)1.941.902.00
γd/(g·cm-3)1.531.501.54
ω/%283529
LL/%4434
PL/%2220
E/(kg·cm-2)500750500
ν0.400.300.40
Tab.7  Material properties for zone D (layers 1-3)
Fig.11  Comparison of normalized response spectra of zone D. (a) Near field; (b) middle field; (c) far field
layers123
φ/(o)036.50
C/(kg·cm-1)0.260.170.24
γwet/(g·cm-3)1.942.192.00
γd/(g·cm-3)1.531.501.54
ω/%283332
LL/%5742
PL/%2827
E/(kg·cm-2)4015040
ν0.350.300.35
Tab.8  Material properties for zone E (Layers 1-3)
Fig.12  Comparison of normalized response spectra of zone E. (a) Near field; (b) middle field; (c) far field
Fig.13  Babol city microzonation map by natural period
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