Geotechnical Earthquake Engineering · Seismic analysis/design of retaining walls mainly consists...

34
Geotechnical Earthquake Engineering by Dr. Deepankar Choudhury Humboldt Fellow, JSPS Fellow, BOYSCAST Fellow Professor Department of Civil Engineering IIT Bombay, Powai, Mumbai 400 076, India. Email: [email protected] URL: http://www.civil.iitb.ac.in/~dc/ Lecture 34

Transcript of Geotechnical Earthquake Engineering · Seismic analysis/design of retaining walls mainly consists...

  • Geotechnical Earthquake

    Engineering

    by

    Dr. Deepankar Choudhury Humboldt Fellow, JSPS Fellow, BOYSCAST Fellow

    Professor

    Department of Civil Engineering

    IIT Bombay, Powai, Mumbai 400 076, India.

    Email: [email protected]

    URL: http://www.civil.iitb.ac.in/~dc/

    Lecture – 34

  • IIT Bombay, DC 2

    Module – 8

    Site Response Analysis

  • Example # 1

    Case Study

    on

    Seismic Ground Response Analysis

    for Mumbai, India

    D. Choudhury, IIT Bombay, India

    Ref.: V. S. Phanikanth, Deepankar Choudhury and G. R. Reddy

    (2011); "Equivalent-linear seismic ground response analysis of

    some typical sites in Mumbai", Geotechnical and Geological

    Engineering, Springer, Vol. 29(6), 1109-1126.

  • 4

    EQUIVALENT LINEAR GROUND

    RESPONSE ANALYSIS FOR MUMBAI

    Mangalwadi site near Girgaon (MBH#1, MBH#2);

    Walkeswar site (WBH#1, WBH#2) ; and

    BJ Marg near Pandhari Chawl site (BBH#1, BBH#2

    & BBH#3)

    Equivalent-linear Ground response Analysis for some

    typical Mumbai Soil sites:

  • D. Choudhury, IIT Bombay, India

    Typical bore hole data at soil site MBH#1 at Mumbai [Phanikanth et al. 2011, Geotech. and Geological Engg., Springer]

  • D. Choudhury, IIT Bombay, India

    Acceleration-time history of

    4 different input motions [Phanikanth et al. 2011, Geotech.

    and Geological Engg., Springer]

  • D. Choudhury, IIT Bombay, India

    Output Acceleration-time history at GL for soil site MBH#1 at

    Mumbai when input was 2001 Bhuj motion

    [Phanikanth et al. 2011, Geotech. and Geological Engg., Springer]

    Software used, DEEPSOIL v3.5beta (2008)

  • D. Choudhury, IIT Bombay, India

    Acceleration response spectra at ground level with 5% damping for

    soil site MBH#1 at Mumbai under various earthquake motions [Phanikanth et al. 2011, Geotech. and Geological Engg., Springer]

  • D. Choudhury, IIT Bombay, India

    Typical soil amplification for earthquake acceleration at various

    soil sites in Mumbai under different earthquake motions [Phanikanth et al. 2011, Geotech. and Geological Engg., Springer]

  • D. Choudhury, IIT Bombay, India

    Acceleration Response Spectra for site MBH#1 at various layers

    for input motions (a) Bhuj 2001 (b) Loma Prieta 1989 (c) Loma

    Gillory 1989 (d) Kobe 1995 [Phanikanth et al. 2011, Geotech. and Geological Engg., Springer]

  • D. Choudhury, IIT Bombay, India

    Comparison of frequencies and validation of model for

    ground response analysis in Mumbai subjected to 2001 Bhuj motion [Phanikanth, 2011, Ph.D. Thesis., IIT Bombay]

  • D. Choudhury, IIT Bombay, India

    Seismic Zonation Map of India as per BIS 1962 and 1966

  • D. Choudhury, IIT Bombay, India

    Seismic Zonation Map of India as per BIS 1970 and 1984

  • D. Choudhury, IIT Bombay, India

    Seismic zonation map of India [as per IS 1893 – Part 1 (2002)]

    with highlight on Soil Characterization

    • Only 3 types of soil!!!

    Soft soil

    Medium soil

    Hard rock

    • Characterization of Soil Based

    on SPT ‘N’ Value, irrespective of

    soil type !!

    • No DYNAMICS (for soil

    characterization) is involved!!!

  • Soil Classification for Seismic Design in USA (NEHRP-2003)

    Choudhury (2010) in Structural Longivity, 3(2), 155-170.

  • Dr. Deepankar Choudhury, IIT Bombay

    Soil Classification as per Eurocode 8 (2004)

  • Dr. Deepankar Choudhury, IIT Bombay

    Comparison of Soil Classification as per

    Modern Seismic Codes Worldwide

  • Dr. Deepankar Choudhury, IIT Bombay

    Soil Amplification Factor for various control Periods

    for different subsoil class for

    Earthquake Type 1 (Ms > 5.5) as per Eurocode 8

    Soil Amplification Factor for various control Periods

    for different subsoil class for

    Earthquake Type 2 (Ms < 5.5) as per Eurocode 8

  • Example # 2

    Case Study

    on

    Seismic Ground Response Analysis

    for Four Ports in Gujarat, India

    D. Choudhury, IIT Bombay, India

    Ref.: Jaykumar Shukla and Deepankar Choudhury (2012); "Seismic

    hazard and site-specific ground motion for typical ports of Gujarat",

    Natural Hazards, Springer, Vol. 60(2), 541-565.

  • Location of selected

    Ports in Gujarat, India

    7/11/2013

    67, E 68, E 69, E 70, E 71, E 72, E 73, E 74, E 75, E

    19, N

    20, N

    21, N

    22, N

    23, N

    24, N

    25, N

    26, N

    F18

    F17

    F14 F15

    F13

    F12 F25A F5

    F2

    F1

    F4

    F3F6

    F7

    F8

    F10

    F9

    F33

    F35

    F34

    F37

    F38 F42

    F41

    F43

    F45 F46

    F31

    F32

    F24

    F49F23

    F48

    F24

    F26

    F21

    F28

    F29

    F30

    Kandla port site

    Mundra port site

    Hazira port site

    Dahej port site

    Fn Fault line

    Legend

    0 N

    Shukla and Choudhury (2012) in Natural Hazards, 60(2), 541-565.

  • Uniform Hazard Spectra for

    Kandla and Mundra port sites

    • UHS obtained are for rock sites

    • Compared with of IS:1893 -Part 1 (2002)

    specified spectra for rock sites – MCE Spectra

    • As per IS:1893 – Part I (2002), Design Basis

    Earthquake can be taken as 50% of MCE.

    0.0 0.5 1.0 1.5 2.0 2.5 3.0 3.5 4.0

    0.0

    0.5

    1.0

    1.5

    2.0

    2.5

    Retrun Period 2475 years

    Retrun Period 475 years

    Retrun Period 72 years

    IS 1893 (2002)- Zone V

    Sp

    ectr

    al A

    ccel

    erat

    ion

    (g

    )

    Spectral Period (s)

    Kandla Port Site

    0.0 0.5 1.0 1.5 2.0 2.5 3.0 3.5 4.0

    0.0

    0.5

    1.0

    1.5

    2.0

    Sp

    ectr

    al A

    ccel

    erat

    ion

    (g

    )

    Spectral Period (s)

    Mundra Port Site

    Retrun Period 2475 years

    Retrun Period 475 years

    Retrun Period 72 years

    IS 1893 (2002)- Zone V

    Shukla and Choudhury (2012) in Natural Hazards, 60(2), 541-565.

  • Stiff Clay

    Typical Geotechnical Characterization

    0 200 400 600 800 1000 1200

    25

    20

    15

    10

    5

    0

    200 400 600 800

    40

    35

    30

    25

    20

    15

    10

    5

    0

    Average (used in present study) Imai, 1977 (for all soils) Jinan, 1987 (for all soils)

    Imai and Yoshimura, 1970 (for all soils)) Imai and Tonouchi, 1982 (for all soils) Iyisan (for all soils)

    Jafari et al., 1997 (for all soils) Yokota et al., 1991 (for all soils) Seed and Idriss, 1981 (for all soils)

    Athanasopoulos, 1995 (for all soils) Kiku, 2001 (for all soils)

    Dep

    th (

    m)

    Shear Wave Velocity (m/sec)

    Kandla Port siteB

    Mundra Port site

    Dep

    th (

    m)

    Shear Wave Velocity (m/sec)

    Silty Clay

    Stiff Clay

    Silty Sand

    Stiff Clay

    Sandy

    Gravel

    Silty Sand

    Dense

    SiltySand

    Shear wave velocities are estimated from 10

    empirical correlations and then averaged.

    0 20 40 60 80

    40

    35

    30

    25

    20

    15

    10

    5

    0

    0 20 40 60 80 100

    Mundra port site

    Dep

    th (

    m)

    SPT N-Value

    Borehole 1

    Borehole 2

    Kandla port site A

    Borehole 1

    Borehole 2

    Site characterization from available

    geotechnical investigations

    Shukla and Choudhury (2012) ASCE GSP No. 225, 1650-1659.

  • Typical synthetic time

    history for Kandla Port

    0 10 20 30 40 50 60 70 80 90 100

    -0.8

    -0.4

    0.0

    0.4

    0.8

    Spec

    tral

    Acc

    eler

    atio

    ns (g

    )

    Time (sec)

    Bhuj Earthquake 2001 (recorded at Ahemedand passport office, N-W component)

    Level 3 ground motion(2475 years return period)

    Level 2 ground motion(475 years return period)

    Level 1ground motion(72 years return period)

    Kandla Port

    Shukla and Choudhury (2012) in Natural Hazards, 60(2), 541-565.

  • Ground Response Analysis

    0.01 0.1 1 10

    0.1

    1

    10

    Pse

    ud

    o-

    Acc

    eler

    atio

    n (

    g)

    Period (sec)

    Layer 1, Damping: 5.0%

    Layer 2, Damping: 5.0%

    Layer 3, Damping: 5.0%

    Layer 4, Damping: 5.0%

    Kandla Port - Level 3 ground motions

    0.1 1 10

    0.0

    0.5

    1.0

    1.5

    2.0

    2.5

    Kandla Port - Level 3 ground motions

    Am

    pli

    fica

    tio

    n r

    atio

    Frequency(Hz)

    Layer 1 to Bedrock

    Layer 2 to Bedrock

    Layer 3 to Bedrock

    Layer 4 to Bedrock

    Layer

    NO

    Avera

    ge

    SPT-

    value

    Description Modulus reduction

    curve and damping

    curve selected

    1 10 Soft clay Sun et al. (1988)

    2 17 Stiff clay Vucetic and Dobry

    (1991)

    3 35-40 Medium silty

    sand

    Idriss (1990), upper

    range

    4 50 Stiff to very stiff

    clay

    Vucetic and Dobry

    (1991)

    • Ground Response analysis is carried out using

    equivalent liner model using SHAKE91 (Schnabel et al.,

    1972).

    • Modulus reduction curves and damping curves are

    selected based on the Soil properties

    • Typical results in form of Pseudo-acceleration response

    spectra and transfer function (amplification factor)

    Shukla and Choudhury (2012) in Natural Hazards, 60(2), 541-565.

  • Important observations Contributing faults:

    • Kandla port :F13, F25A, F14 ; Mundra port:F25A and F13 ; Dahej port : F33 and

    F30; Hazira port : F34

    • IS:1893 part 1:2002, underestimates the seismic ground motions for the two port sites

    of Kachchh region however for Dahej and Hazira ports they are in agreement.

    Ground

    Motion

    level

    Peak ground accelerations (g) IS:1893

    Part 1 (2002 )

    Mundra

    port site

    Kandla

    port site

    Hazira

    port site

    Dahej

    port site

    Zone V Zone III

    Level 1 0.07 0.12 0.05 0.04 ---

    Level 2 0.19 0.25 0.10 0.10 0.18 0.08

    Level 3 0.33 0.40 0.17 0.18 0.36 0.16

    Peak ground accelerations obtained for port sites

  • IIT Bombay, DC 26

    End of

    Module – 8

  • IIT Bombay, DC 27

    Module – 9

    Seismic Analysis and

    Design of Various

    Geotechnical Structures

  • IIT Bombay, DC 28

    Seismic Design of

    Retaining Wall

  • Introduction

    Retaining walls

    › are built for the purpose of holding back earth which would

    otherwise move downwards.

    › knowledge of seismic earth pressure is very important for

    design of retaining structures in the earthquake prone areas.

    D. Choudhury, IIT Bombay, India 29

    Typical Retaining wall sections commonly used in practice (Source:http://www.stonescapecontracting.com/images/images/walls/Retaining_Walll_Type_Function_lg.jpg)

  • Earth Pressures on Retaining Walls

    D. Choudhury, IIT Bombay, India 30

    Earth pressures-

    › at rest earth pressure

    › active earth pressure

    › passive earth pressure

    Earth pressure conditions

  • Failure of Retaining Walls

    D. Choudhury, IIT Bombay, India 31

    Failure of gravity retaining wall

    (Source: http://www.geofffox.com) (Source: http://www.parmeleegeology.com/)

    Retaining walls may fail during an earthquake, if they are not

    designed to resist additional destabilizing earthquake forces.

  • Seismic Analysis and Design of Retaining Walls

    Seismic analysis/design of retaining walls mainly consists of

    › Determining magnitude of additional destabilizing forces that act during an earthquake

    › Determining seismic active and passive earth pressures due to all destabilizing forces (static + seismic)

    › Design section based on above parameters using

    1. Force based approach

    2. Displacement based approach – for performance based

    design

    D. Choudhury, IIT Bombay, India 32

  • Pseudo-static Method

    33

    Theoretical background of seismic coefficient lies in the

    application of D´Alembert´s principle of mechanics.

    Example of elementary seismic

    slope stability analysis

    (Towahata, 2008)

    D’Alembert’s principle of

    mechanics

    Towhata, I., (2008), Geotechnical Earthquake Engineering, Springer,

    Tokyo, Japan.

  • D. Choudhury, IIT Bombay, India

    Conventional Seismic Design of Retaining Walls

    Pseudo-Static Approach Proposed by Mononobe-Okabe (1929)

    Questions: Value of kh and kv to be used for design?

    Soil amplification?

    Variation of seismic acceleration with depth and time?

    Effect of dynamic soil properties? etc.