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    Structural Dynamics and EarthquakeEngineering

    Course 5

    Single degree of freedom systems

    Seismic response of linear elastic systems

    Elastic response spectra

    Inelastic response

    Course notes are available for download athttp://www.ct.upt.ro/users/AurelStratan/

    Seismic action

    Ground acceleration: accelerogram

    Properties of a SDOF system (m, c, k) +

    Relative displacement, velocity and acceleration of aSDOF system

    ( )gu t

    gmu cu ku mu+ + =

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    Seismic action

    North-south component of the El Centro, Californiarecord during Imperial Valley earthquake from 18.05.1940

    Determination of seismic response

    Equation of motion:

    /m:

    Numerical methods

    central difference method

    Newmark method ...

    Response depends on:

    natural circular frequency n (or natural period Tn)

    critical damping ratio

    ground motion

    22n n g

    u u u u + + =

    gmu cu ku mu+ + =

    ( ), ,nu u t T

    gu

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    Seismic response

    Elastic response spectra

    Response spectrum: representation of peak values of

    seismic response (displacement, velocity, acceleration)of a SDOF system versus natural period of vibration, for agiven critical damping ratio

    ( ) ( )0 , max , ,n nt

    u T u t T =

    ( ) ( )0 , max , ,n ntu T u t T =

    ( ) ( )0 , max , ,t t

    n nt

    u T u t T =

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    Elastic displacement response spectrum: Du0

    Pseudo-velocity and pseudo-acceleration

    Spectral pseudo-velocity:

    units of velocity

    different from peak velocity

    Strain energy

    2n

    n

    V D DT

    = =

    ( )22 2 2

    00

    2 2 2 2

    n

    S

    k Vku kD mV E

    = = = =

    Spectral pseudo-acceleration:

    units of acceleration

    different from peak acceleration

    2

    0 0 0S nf ku m u mA= = =

    2

    2 2

    0

    2n n

    n

    u D DT

    = = =

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    2n

    n

    V D DT

    = =

    2

    2 2n

    n

    A D DT

    = =

    D

    Combined D-V-A spectrum

    Displacement, pseudo-velocity and pseudo-acceleration

    spectra:

    same information

    different physical meaning

    A line inclined at +45 for lgA - lg2= const. spectralpseudo-acceleration: an axis inclined to -45

    Similarly, spectral displacement: an axis inclined to +45

    2

    2

    n

    n

    n n

    TAV D or A V D

    T

    = = = =

    ( )2nT A V = lg lg lg 2 lgnT A V+ =

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    Combined D-V-A spectrum

    Characteristics of elastic response spectra

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    Characteristics of elastic response spectra

    Characteristics of elastic response spectra

    ForTnTf spectral displacement Dis close to

    spectral pseudo-acceleration A is small

    BetweenTaand Tc A > BetweenTband Tc A can be considered constant

    BetweenTdand Tf D>

    BetweenTdand Te Dcan be considered constant

    BetweenTcand Td V>

    BetweenTcand Td Vcan be considered constant

    0gu

    0gu

    0gu

    0gu

    0gu

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    Characteristics of elastic response spectra

    Tn>Td response region sensible to displacements Tn

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    Elastic design spectra

    idealized "smooth" spectra based on statistical interpretation (median; median plus

    standard deviation)of severalrecordscharacteristicfor a given site

    Elastic design spectra

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    Elastic design spectra

    TB T

    C T

    DT

    PSA

    TB T

    C T

    DT

    PSV

    TB T

    C T

    DT

    SD

    Inelastic response of SDOF systems

    Most structures designed for seismic forces lower than

    the ones assuring an elastic response during the designearthquake

    design of structures in the elastic range for rare seismic eventsconsidered uneconomical

    in the past, structures designed for a fraction of the forcesnecessary for an elastic response, survived major earthquakes

    f S f S f S

    u u u um

    a b c d

    f S

    u

    a

    b

    c

    d

    f S

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    Inelastic response of SDOF systems

    Elasto-plastic system: stiffness k

    yield force fy yield displacement uy

    Elasto-plastic idealization:equal area under the actualand idealised curves up to

    the maximum displacement um

    Cyclic response of the elasto-

    plastic system

    Corresponding elastic system

    Corresponding elastic system:

    same stiffness

    same mass

    same damping

    Inelastic response:

    yield force reduction factor Ry

    ductility factor

    the same periodof vibration (atsmall def.)

    0 0

    y

    y y

    f uR

    f u= =

    m

    y

    u

    u =

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    Equation of motion

    Equation of motion:

    /m

    Seismic response of an inelastic SDOF system dependson:

    natural circular frequency of vibration n

    critical damping ratio yield displacement uy force-displacement shape

    ( ),S gmu cu f u u mu+ + =

    ( )22 ,n n y S gu u u f u u u + + =

    ( ),Sf u u

    ( ) ( ), ,S S yf u u f u u f=

    Effects of inelastic force-displacement relationship

    4 SDOF systems

    (El Centro):

    Tn = 0.5 sec

    = 5%

    Ry = 1, 2, 4, 8

    Elastic system:

    vibr. about theinitial positionof equilibrium

    up=0

    Inelastic syst.:

    vibr. about anew position ofequilibrium

    up0

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    Elastic inelastic

    Design of a structure responding in the elastic range:f0fRd

    Design of a structure responding in the inelastic range:umuRd Rd

    ductility demand ductility capacity

    um/u0ratio

    El Centro

    ground motion

    = 5%

    Ry = 1, 2, 4, 8

    Tn>Tf um independent

    of Ry umu0

    Tn>Tc umdepends on

    Ry umu0

    Tn u0

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    Ry-relationship: idealisation

    Tnin the displacement- and velocity-sensitive region: "equal displacement" rule um/u0=1 Ry=

    Tnin the acceleration-sensitive region:

    "equal energy" rule um/u0>1

    Tn