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    Rakesh Singh Rajput et al. / International Journal of Engineering Science and Technology

    Vol. 2(12), 2010, 7797-7811

    NON-AXISYMMETRIC DYNAMIC

    RESPONSE OF IMPERFECTLY

    BONDED BURIED ORTHOTROPIC

    THIN EMPTY CYLINDRICAL SHELLDUE TO INCIDENT SHEAR WAVE (SV

    WAVE)

    RAKESH SINGH RAJPUT*

    Reader, Mechanical Engineering, Directorate of Technical Education,

    Bhopal, M. P., India

    [email protected]

    SUNIL KUMARProfessor, Mechanical Engineering, Rajeev Gandhi Technical University

    Bhopal, M. P., India

    [email protected]

    ALOK CHAUBEY

    Professor, Mechanical Engineering, Rajeev Gandhi Technical University

    Bhopal, M. P., [email protected]

    J. P. DWIVEDI

    Professor, Mechanical Engineering, IT-BHU

    Varanasi, U. P., India

    Abstract

    This paper is deals with the non-axisymmetric dynamic response of imperfectly bonded buried orthotropic thin

    empty pipelines subjected to incident shear wave (SV-wave). In the thin shell theory the effect of sheardeformation and rotary inertia is not considered. The pipeline has been modeled as an infinite thin cylindrical

    shell imperfectly bonded to surrounding. A thin layer is assumed between the shell and the surrounding medium

    (soil) such that this layer possesses the properties of stiffness and damping both. The degree of imperfection of

    the bond is varied by changing the stiffness and the damping parameters of this layer. The non axisymmetric

    results are comparing with axisymmetric.

    Key words: - Shear wave, Orthotropic, Imperfect bond, Seismic Wave, Non-Axisymmetric, DynamicResponse, Buried Pipelines, and Thin Shell.

    1. IntroductionDuring past few years a number of studies like Cole Ritter and Jordon (1979) and Singh et al (1987) on the

    axisymmetric dynamic response of buried orthotropic pipe/shells have been reported. Later Chonan (1981);Dwivedi and Upadhyay (1989; 1990; 1991); and Dwivedi et al (1991) have analyzed the axisymmetric problems

    of imperfectly bonded shell for the pipesmade of orthotropic materials.

    *Corresponding Author

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    Upadhyay and Mishra (1988) have presented a good account of work on non-axisymmetric response of buried

    thick orthotropic pipelines under seismic excitation. Again Dwivedi et al (1992a; 1992b); Dwivedi et al(1993a; 1993b; 1996); and Dwivedi et al (1998) have analyzed the non-axisymmetric problems of imperfectly

    bonded buried thick orthotropic cylindrical shells. Kauretzis et al (2007) have presented analytical calculations

    of blast induced strains on buried pipe lines. Hasheninajad and Kazemirad (2008) have reported dynamicresponse of eccentric tunnel in poro-elastic soil under sesmic excitation. Lee et al (2009) have done the risk

    analysis of buried pipelines using probabilistic method. But in all these analyses pipelines have been modeled

    as thick shell. As far as the non-axisymmetric dynamic response of thin shell is concerned, no work has beenreported so far. There is no work available discussing the effect of bond imperfection on the non axisymmetric

    response of buried thin pipes made of orthotropic materials. Therefore, in present paper, the effect of imperfect

    bond on the non- axisymmetric dynamic response of buried orthotropic thin pipelines has been analyzed.

    2. Basic Equations and FormulationThe cylindrical pipeline has been modeled as an infinitely long cylindrical shell of mean radius R and

    thickness h. It is considered to be buried in a linearly elastic, homogeneous and isotropic medium of infinite

    extent. Basic approach of the formulation is to obtain the mid plane displacements of the shell by solving theequations of motion of the orthotropic shell. Traction terms in the equations of motion are obtained by solving

    the three-dimensional wave equation in the surrounding medium. Appropriate boundary conditions are applied

    at the shell surfaces. Equations arising out of boundary conditions along with the equations of motion of the

    shell are simplified to yield a response equation in matrix form. Equation governing the non axis-symmetric

    motion of an infinitely long orthotropic cylinder has been derived following the approach of Herrmann andMirsky (1957).

    The cylindrical shell buried in a linearly elastic, homogeneous and isotropic medium of infinite medium, a thin

    layer is assumed between the shell and the surrounding medium (soil). The degree of imperfection of the bond is

    varied by changing the stiffness and the damping parameters of this layer. The shell is excited by a shear

    vertical wave (SV- wave). A wavelength (=2/) is considered which strikes the shell at an angle withthe axis of the shell. Let a cylindrical polar co-ordinate system (r,, x) which is defined in such a way that xcoincides with the axis of the shell and, in addition, z is measured normal to the shell middle surface, which is

    given as

    h/2zh/2-, Rrz (1)The equation of motion of shell in the matrix form is given as Rajput et.al (2010)

    [{L} {U}] + {P*} = 0 (2)

    Where [L] is 3 3 a matrix and {U} = [w v u] T

    With w, v and u as the displacement components of the middle surface of the shell in the radial, tangential andaxial directions respectively, the elements of {P*} are given by Herrman and Mirsky (1957) as:

    ,1P,1

    h/2

    h/2-

    *

    2

    2/

    _h/2

    *

    1 zh

    zz

    R

    z

    R

    zP

    ,1P,1

    h/2

    h/2-

    *

    4

    2/

    2/

    *

    3 zx

    h

    hzR

    z

    R

    zzP

    2/

    2/

    *

    5 1h

    hzxR

    zzP

    For the evaluation of {P*}, ij at z = (h/2) must be determined in the terms of incident and scattered field in thesurrounding ground. The total displacement field in the ground is written as

    d=d(i) + d(s)

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    Where i and s represents the incident and scattered parts respectively. By solving the wave equation in the

    surrounding infinite medium the components of incident and scattered fields can be written as (Chonan, S.,1981):

    )(expcos

    1

    5

    3

    '

    11

    '

    )( ctxin

    BR

    r

    Ir

    R

    n

    BR

    rIB

    R

    rI

    d

    n

    nn

    i

    r

    )(expsin

    )(

    5

    '

    311

    )( ctxin

    BR

    rI

    BR

    rI

    r

    RinB

    R

    rI

    r

    Rrn

    d

    n

    nn

    i

    )(expcos3211)( ctxinxBR

    rIB

    R

    rIid

    nn

    i

    x

    (3)

    Where B1 ='1B /R, B3 =

    '3B /R

    2 and B5 ='5B /R. (

    ) denotes differentiation with respect to the argument of

    the Bessel functions. The constants B1, B3 and B5 depend on the parameters of the incident wave and may be

    expressed as:

    3n52

    2n3

    1

    11n1

    A)1(B,

    Ai)1(B,

    Ai)1(B (4)

    )ctx(iexpncosBR

    rK

    r

    RnB

    R

    rKiB

    R

    rKd 6n4

    'n12

    'n

    )s(r

    )ctx(iexpnsinB

    R

    rK

    BR

    rK

    r

    RinB

    R

    rK

    r

    Rn

    d

    6'n

    4n12n

    )s(

    )ctx(iexpncos

    BR

    rKBR

    rKid 4n

    22n1)s(

    x

    (5)

    Where dr, d, dx are components of displacement vector,

    321 ;; AAA

    are amplitudes of P, SV and SH wave

    respectively.

    Here ./Band/,/ '662'

    44

    '

    22 RBRBBRBB are constants.Stress fields due to the incident wave can be obtained by plugging above equations into the stress-displacement

    relations of the medium, and are given by:

    )ctx(iexpncos

    BR

    rI

    r

    R

    R

    rI

    r

    Rn2

    BR

    rIi2

    BR

    rI2

    R

    rI2

    R

    5n'n

    3

    "

    n

    2

    1

    1"n

    2n

    22

    21

    )i(

    rr

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    )(expsin2

    2

    5

    2

    '"2

    3

    '

    1

    1

    '

    )(ctxin

    B

    R

    rI

    r

    nR

    R

    rI

    r

    R

    R

    rI

    BR

    rI

    r

    R

    R

    rI

    r

    Rin

    BR

    rI

    R

    rI

    r

    R

    r

    Rn

    R

    nnn

    nn

    nn

    i

    r

    )(expcos

    22

    51

    '2

    2

    2

    11

    '

    1

    )(ctxin

    BR

    rI

    r

    Rin

    R

    rIB

    R

    rIi

    Rn

    nn

    i

    rx

    )(expcos

    2

    2

    22

    6

    '

    4

    "2

    1

    2

    "22

    2

    2

    1

    )(ctxin

    BR

    rK

    r

    R

    R

    rK

    r

    Rn

    BR

    rKi

    BR

    rK

    R

    rK

    R

    nn

    n

    nn

    s

    r

    )(expsin2

    2

    6

    2

    '"2

    4

    '

    1

    2

    '

    )(ctxin

    BR

    rK

    r

    nR

    R

    rK

    r

    R

    R

    rK

    BR

    rK

    r

    R

    R

    rK

    r

    Rin

    BR

    rK

    R

    rK

    r

    R

    r

    Rn

    R

    nnn

    nn

    nn

    s

    r

    )(expcos

    22

    61

    4

    '2

    2

    2

    12

    '

    1

    )(ctxin

    BR

    rK

    r

    Rin

    BR

    rKB

    R

    rKi

    Rn

    nn

    s

    rx

    (6)

    WhereIn ( ) Modified Bessel function of first kind

    Jn ( ) Bessel function of first kind

    Kn ( ) Modified Bessel function of second kindWith the help of above equations the stresses at the outer surface of the shell (z = h/2 or r = R + h/2) can be

    obtained. Thus {P*} in Eq. (2) can be determined.

    Now the mid plane displacement and slopes are assumed to be of the form;

    0ww cosn exp[i(x-ct)]

    0vv sinn exp[i(x-ct)]

    0uu cosnexp[i(x-ct)] (7)

    Plugging Eq. (7) in Eq. (2) and (6) along with the expression for {P*}, a set of six simultaneous algebraicequations are obtained.Three more equations are obtained by imposing the boundary conditions at the inner and

    outer surfaces of the shell: i.e.,

    2/

    )()()( hRr

    s

    r

    i

    r ddw

    2/

    )()()()2/( hRr

    siddhv

    2/

    )()( )()2/(hRr

    s

    x

    i

    xx ddhu (8)Boundary conditions at the outer surface of the shell (r = R + h/2) are obtained by assuming that the shell and

    the continuum are joined together by a bond which is thin, elastic and inertia less. This implies that the stress at

    the shell-soil interface is continuous. To take the elasticity of the bond into account, the stresses in the bond are

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    assumed proportional to relative displacements between the shell and continuum. shear modulus of medium

    and density of shell material.

    2/2/ ])()([()( hRrxs

    xi

    xxxhRrrx Rrut

    ZS

    2/2/ )])([()( hRrsr

    irrrhRrrr w

    tZS

    2/2/ ])()([()( hRrsi

    hRrr Rrut

    ZS

    (9)

    ,.RSr

    R

    RS .

    and RSxx

    .

    are the non-dimensionalized stiffness coefficient of the bond in

    radial , tangential and axial direction respectively.

    1cZrr

    1cZ

    and1cZx

    x

    are the non-dimensionalized damping coefficient of the bond in

    radial, tangential and axial direction respectively.

    Thus a total of six algebraic equations are obtained. These six equations when simplified give the final response

    equation, which may be put into the form

    3523110 BBFB}}{{ FFUQ (10)

    ;6423

    6

    3

    4

    3

    2

    3

    0

    3

    0

    3

    0 T

    T

    BBBUVWAB

    AB

    AB

    Au

    Av

    AwU

    Where [Q] is a (6x6)) matrix and {F1}, {F2} and {F3} are (61) matrices. But for the response of shear verticalwave the amplitudes due to shear waves

    1B and 5B would be zero so the effect of {F1} and {F3} matrices

    would be eliminated. Putting values of 1B = 5B = 0 and substituting values of 3B Eq. (6) becomes as

    22

    20 F)1(}}{{

    AiUQ

    n

    (11)Elements of Matrix F

    ;222

    1 12

    122

    21

    31 nn II

    hF

    ;

    21

    2

    21

    2

    11132

    h

    IInhF nn

    ;22

    1 113

    3 nIih

    F

    ;

    21

    , 13513

    4

    h

    InFIF n

    n

    )](2)(){2[)({ 1"2

    1

    2

    2

    2

    1

    1

    1

    '3

    6

    nn

    rr

    rrn II

    iIF

    Elements of matrix Q in Eq. (11) and matrix L in Eq. (2) are same as provided in Rajput et.al (2010).

    3. Results and DiscussionsResults are presented for a transversely isotropic shell with r- as the plane of isotropy.Consequently zEE , xxz GG , xzx , zz , )1(2/EG zz . Thus wehave 23 , and )1(2/E/G z1xz4 . In addition 3.0xz has beentaken in the numerical calculations. Different values of 1 and 2 used are as follows 1 = 0.5, 0.1, 0.05 and

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    2 = 0.1,05,.02, has been varied between 0.1 to 10.0 to take into account different soil conditions around thepipe, = 0.1 corresponds to the soft soil , =1 for medium soil and for hard rocky soil = 10.0 For all the

    values of , m = 0.25 has been assumed. Thickness to radius ratio of the shell (h ) has been taken as 0.01

    and the density ratio of the surrounding medium to the shell ( ) has been taken as 0.75. Non-dimensional

    amplitude of the middle surface of the shell in the radial and axial directions (W andU) have been plottedagainst the non-dimensional wave number of the incident shear vertical wave (SV-wave) ( = 2R/). The shellresponse has been shown non-axisymmetric (n = 1) flexural mode and axisymmetric mode taking stiffness

    coefficient (x

    r ), damping coefficient ( x r ) as bond parameter and 1 , 2 as the shell

    orthotropic parameters.

    The bond parameters have been varied between zero and infinity,x =

    = r = x = = r = 0

    corresponds to perfect bonding between the shell and surround shell.

    Figure 1 to figure 3 shows the effect of stiffness coefficient on the axial displacement of the shell at different

    angle of incidence of wave, at different condition of the soil with increasing wave number

    Figure1. Axial displacement )(U vs. wave number ( ) withx = 0.1, 10,100 as

    Parameter

    10x 100x

    1.0x

    1.0x

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    Figure2. Axial displacement )(U vs. wave number ( ) withx = 0.1, 10,100 as

    Parameter

    Figure3. Axial displacement )(U vs. wave number ( ) withx = 0.1, 10,100 as

    Parameter

    100,10,1.0x

    1.0x

    100x

    1.0x

    100x

    1.0x

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    Figure 4to figure 6 shows the effect of damping coefficient on the axial displacement of the shell at different

    angle of incidence of wave, at different condition of the soil with increasing wave number

    Figure4. Axial displacement )(U vs. ( ) withx = 0.1, 10,100 as Parameter

    Figure5. Axial displacement )(U vs. wave number ( ) withx = 0.1, 10,100 as

    Parameter

    100,10,1.0x

    100x

    1.0x

    100,10,1.0x

    100,10,1.0x

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    Figure6. Axial displacement )(U vs. wave number ( ) withx = 0.1, 10,100 as

    Parameter

    Figure 7 to figure 10 shows the effect of stiffness coefficient on the radial displacement of the shell at different

    angle of incidence of wave, at different condition of the soil with increasing wave number

    Figure7. Radial displacement )W( vs. wave number ( ) withr = 0.1, 10,100 as

    Parameter

    100,10,1.0x

    100x

    100,10,1.0x

    1.0r

    100r

    100,10,1,0r

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    Figure8 Radial displacement )(W vs. wave number ( ) withr = 0.1, 10,100 as

    Parameter

    Figure9 Radial displacement )(W vs. wave number ( ) withr = 0.1, 10,100 as

    Parameter

    100r1.0r

    100,10,1,0r

    100,10,1.0r

    100,10,1.0r 1.0r

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    Figure10. Radial displacement )(W vs. wave number ( ) with r = 0.1, 10,100 asParameter

    Figure11. Radial displacement )(W vs. wave number ( ) withr = 0.1, 10,100 as

    Parameter

    100,10,1.0r

    100,10,1.0r

    100,10,1.0r

    100,10,1.0r

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    Figure12. Radial displacement )(W vs. ( ) with r = 0.1, 10,100 as Parameter.

    Conclusions

    Based on the results presented following general conclusions could be drawn-.

    Unlike the behavior observed in the non-axisymmetric mode a loose contact between the shell andthe surrounding soil does not always give more shell displacement as compared to those for a

    perfectly bonded shell. Therefore assuming a perfect bond may not always lead to a safe and

    conservative estimate of displacements.

    Effects of bond parameters depend upon the soil conditions and the incidence angle andwavelength of the incident wave. In hard and rocky surroundings bond imperfections show more

    prominent effects on the shell response.

    The flexural mode response assumes considerable importance in soft soil condition and at higher

    apparent wave speed. Flexural mode response due to incident shear vertical wave is significant only at large angle of

    incidence.

    For large angle of incidence radial deflection is higher in flexural modes at larger wavelength but atthis value it is the axial deflection in axisymmetric mode, which is higher. Thus for larger wavelength

    axisymmetric mode is more important because the most common cause of pipeline failure is excessive

    axial deformation, while at smaller wavelength the flexural mode has much importance for axialdisplacement.

    Both the shell orthotropic parameters influence the radial displacement equally well but 2 has astronger influence on the axial displacement than 1 . As the Stiffness and the damping coefficient isincrease the axial and radial response increase.

    Axial deflection and radial deflection both are increase when the value of bonding parameter stiffnesscoefficient (

    x r), damping coefficient (

    x r) increase from zero to infinity (perfect

    to imperfect bonding) as parameters.

    Nomenclature

    A Amplitude of the plane wave

    321 ;; AAA

    Amplitudes of P-SV-SH wave respectively

    B1 .,B6 Arbitrary constants

    '6

    '1 B.......B Arbitrary constants

    100,10,1.0r

    100r

    1.0r

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    c Apparent wave speed along the axis of the shell

    dr, d, dx Components of displacement vector

    ER, E, EX Young modulus of the shell.

    xr eee ;;

    Unit vector in co-ordinate direction

    {F1}, {F2}, {F3} Column vector

    Gx, Gxz, Gz Shear moduli of the shell

    H Vector displacement in the medium

    H'

    Displacement potential corresponding to SV wave

    Hr, H, HX Components of vector potential(Hx corresponding to SH wave)

    h Thickness of the shell

    h (=h/R) Non dimensional thickness of the shellIn ( ) Modified Bessel function of first kind

    Jn ( ) Bessel function of first kindKn ( ) Modified Bessel function of second kind

    kx, k Shear correction factor

    {L} Matrix operator

    xxxx MMMM ;;;

    Stress resultant moments

    xxxx NNNN ;;; Stress resultantsn Mode shape number in the tangential direction{P*} Column matrix

    R Mean radius of the shell

    r Radial coordinate

    t Time

    U Non-dimensional amplitude of the shell in axial directionu Displacement of the shell middle surface in the axial directionu0 Displacement amplitude of the shell middle surface in the axial direction

    uz, u, ux Displacement component of a point in the shell

    V Non-dimensional amplitude of the shell in the tangential directionv Displacement of the shell middle surface in the tangential direction

    v0 Displacement amplitude of shell middle surface in tangential direction

    W Non-dimensional amplitude of the shell in the radial directionw Displacement of the shell middle surface in the radial directionw0 Displacement amplitude of the shell middle in the radial directionx Coordinate along the shell axis

    z Coordinate normal to middle surface of the shell

    Angle of incidence of the wave(=2R/) Non-dimensional wave number of incident wave1, 2, 3, 4 Non-dimensional shell orthotropic parameters of the shellz Normal to middle surface of the shell Tangential direction Wave length of the incident wave Lames constant Modulus of rigidity

    xzGNon-dimensional modulus of rigidity of medium

    m Poisson ratio the mediumx, x, z, zx, xz Poisson ratios of the shell

    (= 2 cos / ) Apparent wave number Density of the shell materialm Density of the medium

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    m Non-dimensional density of the medium

    ij Components of stress tensor Scalar displacement potential in the mediumx Angle of rotation in r-x plane Symmetry constant =1for n=0, =2 for n=1xo Amplitude ofx Angle of rotation in r- plane

    Subscripts

    m Medium

    r Radial directionx Axial direction

    z Normal to middle surface of the shell

    Tangential direction

    Superscripts

    i Incident wave

    s Scattered wave

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    Biographical notes

    Rakesh Singh Rajput received M. Tech. from NIT Allahabad, India and pursuing Ph.D. from Rajeev Gandhi Technological University,

    Bhopal, India. He is a Reader in Mechanical Engineering, and working with Department of Technical Education (DTE), Govt. of M. P.,

    India. His research interests include machine design and mechanics. He has written book on Engineering Mechanics.Dr. Sunil Kumar is a Professor of Mechanical Engineering, Rajeev Gandhi Technological University, Bhopal, India. He has received M.

    Tech from IT-BHU, Varanasi, India and Ph. D. from IIT Delhi, India. He has more than 20 years of experience in teaching and research. His

    current area of research includes Combustion mechanics and System Dynamics.

    Dr. Alok Chaube is a Professor of Mechanical Engineering, Rajeev Gandhi Technological University, Bhopal, India. He has received M.Tech from IIT Delhi, India and Ph. D. from IIT Roorkee, India. He has more than 20 years of experience in teaching and research. His

    current area of research includes Fluid mechanics and System Dynamics.