geotechnical earthquake engineering · 2017. 8. 4. · h h t hh ht 2 2 s and p v v ω excitation...

27
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 35

Upload: others

Post on 08-Feb-2021

0 views

Category:

Documents


0 download

TRANSCRIPT

  • 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 – 35

  • IIT Bombay, DC 2

    Module – 9

    Seismic Analysis and

    Design of Various

    Geotechnical Structures

  • IIT Bombay, DC 3

    Seismic Design of

    Retaining Wall

  • Earth Pressures on Retaining Walls

    D. Choudhury, IIT Bombay, India 4

    Earth pressures-

    › at rest earth pressure

    › active earth pressure

    › passive earth pressure

    Earth pressure conditions

  • Failure of Retaining Walls

    D. Choudhury, IIT Bombay, India 5

    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 6

  • Pseudo-static Method

    7

    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.

  • D. Choudhury, IIT Bombay, India

    Available Literature

    Mononobe-Okabe (1926, 1929)

    Madhav and Kameswara Rao (1969)

    Richards and Elms (1979)

    Saran and Prakash (1979)

    Prakash (1981)

    Nadim and Whitman (1983)

    Steedman and Zeng (1990)

    Ebeling and Morrison (1992)

    Das (1993)

    Kramer (1996)

    Kumar (2002)

    Choudhury and Subba Rao (2005)

    Choudhury and Nimbalkar (2006)

    And many others…………..

    D. Choudhury, IIT Bombay, India

  • Pseudo-static Method

    • Richards and Elms (1979) proposed a method for seismic design of

    gravity retaining walls which is based on permanent wall displacements. (Displacement based approach)

    10

    2 3

    max max

    40.087pem

    y

    v ad

    a

    Displacement should be calculated by

    following formula, and should be checked

    against allowable displacement.

    where, vmax is the peak ground velocity, amax

    is the peak ground acceleration, ay is the

    yield acceleration for the wall-backfill system.

    Seismic forces on gravity

    retaining wall

    Richards and Elms (1979)

    Richards, R. Jr., and Elms, D. G. (1979). Seismic behavior of gravity retaining walls. Journal of

    Geotechnical Engineering, ASCE, 105: 4, 449-469.

  • Pseudo-static Method

    • Choudhury and Subba Rao (2002) gave design charts for the

    estimation of seismic passive earth pressure coefficient for negative

    wall friction case. (Canadian Geotech. Journal, 2002)

    11

    • The application of this case is for anchor uplift

    capacity.

    • Design charts are given for calculation of various

    parameters like kpγd, which can be used to

    compute seismic passive resistance, which is

    given by, 2

    pd pcd pqd pγd

    1 1P = 2cHK +qHK γH K

    2 cosδ

    where Ppd is seismic passive resistance,

    Kpγd, Kpqd, and Kpcd are the seismic

    passive earth pressure coefficients.

    Choudhury, D. and Subba Rao, K. S. (2002). Seismic passive earth

    resistance for negative wall friction, Canadian Geotechnical Journal, 39:5,

    971–981.

  • Pseudo-static Method

    • Choudhury et al. (2004) presented a comprehensive review for

    different methods to calculate seismic earth pressures and their

    point of applications. (Current Science, 2004)

    12

    2 2 22 cos 2 sin (cos cos )

    2 cos (sin sin )d

    H H th H

    H t

    22 and

    psVV

    ω excitation frequency, Vs and Vp are

    shear and primary wave velocities

    respectively, H is height of retaining wall.

    Expression for the point of application of

    seismic passive resistance by,

    Choudhury, D., Sitharam, T. G. and Subba Rao, K. S.

    (2004). Seismic design of earth retaining structures and

    foundations. Current Science, India, 87:10, 1417-1425.

  • Seismic Passive Resistance by Pseudo-static Method

    D. Choudhury, IIT Bombay, India 13

    Subba Rao, K. S., and Choudhury, D. (2005). Seismic passive earth pressures in soils.

    Journal of Geotechnical and Geoenvironmental Engineering, ASCE, 131:1, 131- 135.

  • Pseudo-static Method

    • Subba Rao and Choudhury (2005) gave design charts for

    seismic passive earth resistance coefficients by using a

    composite failure surface for positive wall friction angle. (Jl. of

    Geotechnical and Geoenvironmental Engg., ASCE, 2005)

    D. Choudhury, IIT Bombay, India 14

    • Design charts were proposed for the

    direct computation of seismic passive

    earth resistance coefficients for various

    input parameters.

    • The application of this case is for bearing

    capacity of foundations.

  • Pseudo-static Method

    • Shukla et al. (2009) have described the derivation of an analytical

    expression for the total active force on the retaining wall for c-ϕ soil backfill considering both the horizontal and vertical seismic coefficients.

    • The seismic active earth pressure is given by,

    8

    21 (1 )2

    ae v ae aecP H k K cHK

    where, sin( )

    cos( )tan

    cos (cos tan sin )

    cae

    c

    K

    2cos (1 tan )

    tan (cos tan sin )

    caec

    c c

    K

    and

    tan1

    h

    v

    k

    k

    and αc is critical failure plane angle, ϕ shearing

    resistance of soil Shukla, S. K., Gupta, S. K. and Sivakugan, N. (2009). Active earth pressure on retaining wall

    for c-ϕ soil backfill under seismic loading condition. Journal of Geotechnical and Geoenvironmental Engineering, ASCE, 135:5, 690‒696.

  • Pseudo-static Method

    Major limitations

    › Representation of the complex, transient, dynamic effects of earthquake shaking by single constant unidirectional

    pseudo-static acceleration is very crude.

    › Relation between K and the maximum ground acceleration is not clear i.e. 1.9 g acceleration does not mean K = 1.9

    Advantages

    › Simple and straight-forward

    › No advanced or complicated analysis is necessary.

    › It uses limit state equilibrium analysis which is routinely

    conducted by Geotechnical Engineers.

    D. Choudhury, IIT Bombay, India 9

  • Development of Modern Pseudo-Dynamic Approach

    Soil amplification is considered.

    Frequency of earthquake excitation is considered.

    Time duration of earthquake is considered.

    Phase differences between different waves can be considered.

    Amplitude of equivalent PGA can be considered.

    Considers seismic body wave velocities traveling during earthquake.

    Advantages

    Pseudo-Dynamic Approach by

    Steedman and Zeng (1991),

    Choudhury and Nimbalkar (2005)

    Choudhury and Nimbalkar, (2005), in Geotechnique, ICE Vol. 55(10), pp. 949-953.

    ah(z, t) = {1 + (H – z).(fa – 1)/H}ah sin [{t – (H – z)/Vs}]

    av(z, t) = {1 + (H – z).(fa – 1)/H}av sin [{t – (H – z)/Vp}]

  • H

    h0

    ( ) m(z)a (z, t)dz hQ t 2

    2 Hcosw (sin sin )4 tan

    ha w wtg

    =

    where, = TVs is the wavelength of the vertically propagating

    shear wave and = t-H/Vs.

    H

    v

    0

    ( ) m(z)a (z, t)dz vQ t 2

    2 Hcos (sin sin )4 tan

    va tg

    The total (static plus dynamic) passive resistance is given by,

    where, = TVp, is the wavelength of the vertically propagating primary

    wave and = t – H/Vp.

    ah(z, t) = ah sin [{t – (H – z)/Vs}]

    where = angular frequency; t = time elapsed; Vs = shear wave velocity;

    Vp = primary wave velocity

    sin( ) cos( ) sin( )

    cos( )

    h vpe

    W Q QP

    av(z, t) = av sin [{t – (H – z)/Vp}] and

    Choudhury, D. and Nimbalkar, S. (2005), in Geotechnique, ICE London, U.K., Vol. 55, No. 10, 949-953. 8

  • ( ) sin( )( )

    tan cos( )

    cos( ) sin

    tan cos( )

    sin( ) sin

    tan cos( )

    pe

    pe

    h

    s

    v

    p

    dP t zp t

    dz

    k z zt

    V

    k z zt

    V

    The coefficient of seismic passive resistance (Kpe) is given by,

    The seismic passive earth pressure distribution is given by,

    where and

    Choudhury, D. and Nimbalkar, S. (2005), in Geotechnique, London, U.K., Vol. 55, No. 10, 949-953.

  • Typical non-linear variation of seismic passive earth pressure

    Choudhury and Nimbalkar (2005)

    1.0

    0.8

    0.6

    0.4

    0.2

    0.0

    0 1 2 3 4 5 6

    kv = 0.5k

    h, = 30

    0, = , H/ = 0.3, H/ = 0.16

    z/H

    ppe

    /H

    kh=0.0

    kh=0.1

    kh=0.2

    kh=0.3

    Choudhury, D. and Nimbalkar, S. (2005), in Geotechnique, London, U.K., Vol. 55, No. 10, 949-953.

  • 0.3 0.4 0.5 0.6 0.7 0.8 0.9 1.0

    2

    3

    4

    5

    6

    kh = 0.2, k

    v = 0.0, = 30

    0, = 16

    0

    fa=1.0

    fa=1.2

    fa=1.4

    fa=1.8

    fa=2.0

    Kp

    e

    H/TVs

    Effect of amplification factor on seismic passive earth pressure ah(z, t) = {1 + (H – z).(fa – 1)/H}ah sin [{t – (H – z)/Vs}]

    Nimbalkar and Choudhury (2008)

    Nimbalkar, S. and Choudhury, D. (2008), in Journal of Earthquake and Tsunami, Singapore, Vol. 2(1), 33-52.

  • D. Choudhury, IIT Bombay, India

    1.0

    0.8

    0.6

    0.4

    0.2

    0.0

    0 1 2 3 4 5

    H/ = 0.3, H/ = 0.16

    kh= 0.2, k

    v= 0.5k

    h, = 30

    0, = /2

    ppe

    /H

    z/H

    Mononobe-Okabe method

    Present study

    Comparison of proposed pseudo-dynamic method

    with existing pseudo-static method – Passive case

  • D. Choudhury, IIT Bombay, India

    Comparison of proposed pseudo-dynamic method

    with existing pseudo-static methods – Passive case

    0.0 0.1 0.2 0.30

    1

    2

    3

    4

    5

    6

    7

    8

    Mononobe-Okabe method

    Choudhury (2004)

    Present study

    Kpe

    kh

    = 350, = /2, k

    v = 0.5k

    v, H/ = 0.3, H/ = 0.16 Choudhury and

    Nimbalkar

    (2005) in

    Geotechnique

  • Choudhury and Nimbalkar (2006)

    Seismic Active Earth Pressure by Pseudo-Dynamic Approach

    Choudhury, D. and Nimbalkar, S. (2006), “Pseudo-dynamic approach of seismic active earth pressure behind retaining

    wall”, Geotechnical and Geological Engineering, Springer, The Netherlands, Vol 24, No.5, pp.1103-1113.

  • D. Choudhury, IIT Bombay, India

    H

    h0

    ( ) m(z)a (z, t)dz hQ t 2

    2 Hcosw (sin sin )4 tan

    ha w wtg

    =

    where, = TVs is the wavelength of the vertically propagating

    shear wave and = t-H/Vs.

    H

    v

    0

    ( ) m(z)a (z, t)dz vQ t 2

    2 Hcos (sin sin )4 tan

    va tg

    The total (static plus dynamic) active thrust is given by,

    where, = TVp, is the wavelength of the vertically propagating primary

    wave and = t – H/Vp.

    sin( ) ( )cos( ) ( )sin( )( )

    cos( )

    h vae

    W Q t Q tP t

    ah(z, t) = ah sin [{t – (H – z)/Vs}]

    where = angular frequency; t = time elapsed; Vs = shear wave velocity;

    Vp = primary wave velocity.

    av(z, t) = av sin [{t – (H – z)/Vp}] and

  • D. Choudhury, IITB Choudhury and Nimbalkar (2006)

    1 22 2

    1

    2

    1 sin cos sin

    tan cos 2 tan cos 2 tan cos

    where,

    m 2 cos 2 sin 2 sin 2

    m

    ph S v

    ae

    S

    s s

    TVk TV km m

    H H

    TVt H t H t

    T TV H T TV T

    K

    2 cos 2 sin 2 sin 2pp p

    TVt H t H t

    T TV H T TV T

    ( ) z sin( )( )

    tan cos( )

    cos( ) sin

    tan cos( )

    sin( ) sin

    tan cos( )

    aeae

    h

    s

    v

    p

    P tp t

    z

    k z zw t

    V

    k z zw t

    V

    The seismic active earth pressure distribution is given by,

    The seismic active earth pressure coefficient, Kae is defined as

  • Typical non-linear variation of

    seismic active earth pressure

    1.0

    0.8

    0.6

    0.4

    0.2

    0.0

    0.0 0.1 0.2 0.3 0.4 0.5 0.6

    kv=0.5k

    h, =30

    0, ,H/=0.3, H/=0.16

    z/H

    pae

    /H

    kh=0.0

    kh=0.1

    kh=0.2

    kh=0.3

    Choudhury and Nimbalkar (2006), in

    Geotechnical and Geological Engineering,

    24(5), 1103-1113.

    0.3 0.4 0.5 0.6 0.7 0.8 0.9 1.0

    0.2

    0.4

    0.6

    0.8

    1.0

    kh = 0.2, k

    v = 0.0, = 33

    0, = 16

    0

    fa=1.0

    fa=1.2

    fa=1.4

    fa=1.8

    fa=2.0K

    ae

    H/TVs

    ah(z, t) = {1 + (H – z).(fa – 1)/H}ah sin [{t – (H – z)/Vs}]

    Effect of soil amplification on

    seismic active earth pressure

    Nimbalkar and Choudhury (2008),

    in Journal of Earthquake and Tsunami, 2(1), 33-52.

    D. Choudhury, IIT Bombay