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    CHAPTER 3: BASIC CONCEPTS AND DEFINITIONS

    3.1Basic Definitions:3.1.1 Deformation Gradient: Consider a body as shown in Fig. 1 which undergoes some

    deformations. Let R and R*be the undeformed and deformed states of the body respectively. Let

    x be the position vector of a point P of the body in R. Position of point P in the deformed

    configuration is p and its position vector is y. Let dxrepresents a

    Figure 1: Body in undeformed and deformed configurationssmall length element in undeformed configuration and it is changed to dy in the deformed

    configuration . Then dy and dx are related to each other by

    where F is given by

    [

    ]

    This F and is called the deformation gradient. Here are the components of displacementu in directions respectively.

    (1)

    (2)

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    3.1.2 Principle Invariants of a Tensor:For any tensor A we can define three terms called as

    principle invariants which are denoted by I1, I2, I3and are given by

    *,- + where tr denotes trace of tensor and det denotes determinant of tensor.

    3.1.3 Indicial notations:The indicial notations we have used can be understood by taking an

    example. Let f is a function of then

    3.1.4 CauchyGreen Deformation Tensors:

    3.1.4.1 Right Cauchy Green deformation tensor:It is defined as

    Here T denotes the transpose.

    3.1.4.2 Left CauchyGreen deformation tensor:It is defined as

    3.1.5 Traction Vector: If dF is the force acting on an area ds of the surface of a body then

    traction vector is defined as

    3.1.6 Stress At A Point:At any point of the body the state of stress is defined by following stress

    tensor

    Here represent that the stress is acting in j

    th

    direction on a plane which is perpendicular to theith

    direction.

    (3)

    (4)

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    calculate tr and det of any tensor. Other

    incomplete information. Thissub-section

    after indicial notation.

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    3.1.7 Relation between t and : If the normal vector to the surface of the body is nthen at thatpoint

    and t are related by

    3.1.8 Types Of Stress Tensor: When a body undergoes large deformations then we have tomake distinction between undeformed and deformed configuration.Let us assume that traction T

    is applied on a small surface element dS in R .N is the normal vector on dS. Whilet and nare

    the traction vector and normal vector to the surface element ds in R*. Let force acting on the

    body is df. Then we can define following three types of stress tensors

    Figure 2: Body with PK-I and Cauchy traction vectors

    3.1.9 Cauchy Stress Tensor : In this tensor the area of deformed configuration is used for stress

    calculation. It is denoted byand is given by

    Here tis the Cauchy traction vector. Cauchy stress tensor is symmetric.

    3.1.10 First Piola-Kirchhoff (PK-I) stress Tensor: In this tensor the area of undeformed

    configuration is used for stress calculation. It is denoted by

    and is given by

    Here T is the first Piola-Kirchhoff (PK-I) traction vector. First Piola-Kirchhoff (PK-I) stress

    Tensor is generally not symmetric.

    3.1.11 Second Piola-Kirchhoff (PK-II) stress Tensor:We define a pseudo force vector suchthat

    then second Piola-Kirchhoff stress tensor denoted by S is given by

    3.1.12 Relation Between Three Stress Tensors:By equations (6) and (7) we obtain

    (5)

    (6)

    (7)

    (8)

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    We shall use the Nansons relationwhich relates the normal vector in undeformed and deformed

    co-ordinates,

    Now

    This is the relation between and . J is the third invariant of and its value is 1 forincompressible materials. Again from (7) and (8)

    and putting from (9) This is the relation between and S.3.2 Hyper elastic materials and basic governing equations:

    3.2.1 Hyperelastic materials:Linear elastic material model assumes that the deformations are

    small in the material. There exists some materials which are elastic but exhibits large

    deformations upon loading so that linear elastic model is not suitable for such materials.

    Hyperelastic model is used to characterize such material behavior. Rubber, vualcaunized

    elastomers, unfilled elastomers and biological tissues are some examples whose behaviour can be

    best characterized by hyperelastic model. These materials are a special case of Cauchy elastic

    materials which means that the stress state depends only on the current state of deformation and

    not on the path or history of deformation. For these materials stress-strain relationships are

    derived from strain energy density function W and given by

    For general hyperelastic material model W is a function of three principle invariants of the left

    (or right) Cauchy-Green tensor

    The values of are given by

    (9)

    (10)

    (11)

    (12)

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    I is the unit tensor. Putting values in S

    Using (11)

    Following are the names ofsome of the widely used hyperelastic material laws:

    a. Neo-Hookean

    b.Mooney-Rivlin

    c. Polynomial form of order 2

    d.Reduced Polynomial form of order 2

    e. Arruda-Boyce

    These all differ in the way that they assume different expressions for W. In this seminar material

    is chosen to be Neo Hookean because it gives the simplest expression for W. In addition the

    Neo-Hookean material is assumeds the material to be incompressible. So to ensure that

    deformation is locally volume preserving (incompressible) we shall assume that an arbitrary

    hydrostatic pressure p is acting at all points of the body such that equation (13) converts to

    For Neo-Hookean material W is a function ofonly so the derivatives of W with respect to and will be zero hence from equation (14)

    and from equation (9)

    (13)

    (14)

    (15)

    (16)

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    Chapter 4 Problem Considered And Its Solution

    Figure 3: Crack with coordinate system

    4.1 Solution of the crack problem: Consider a region R which represents the open cross

    section of an infinite slab containing a crack of length 2c. The slab is to be deformed in finite anti

    plane shear. Such a deformation is characterized by

    Our goal is to find which will satisfy the boundary conditions and equilibrium equations andconsistent with the constitutive relation (15) and (16). Now with the above displacementcomponents the values of and from EQs. (???) and (???) will be

    [

    () ()]

    So from the state of stress in the slab in terms of PK-I stress tensor from equation (16) is

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    [

    ]

    And in terms of Cauchy stress tensor from equation (15) is

    [

    () ()]

    () () The equilibrium equations in terms of and are

    Since the surface of the crack is a free surface i.e. there is no load at that surface so traction will

    be zero along the crack faces in both deformed and undeformed configuration. We can not

    determine the stress boundary conditions in terms of Cauchy stresses because body has

    undergone large deformation so in the deformed configuration we do not know the no rmal vector

    in the plane of crack. We can determine the boundary conditions only in terms of PK-I stresses so

    we shall solve equation and determine the state of stress . Then from the relation between and we shall determine which we are finally interested in. From (17) and (20)0 1 (21)

    (17)

    (18)

    (19)

    (20)

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    Comment [w6]: Both places we cant

    meaning is different in undeformed and

    cases.

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    Here and have the range 1, 2. Since left side expression of this equation is a function of and only so p should be linear in . And first two equation requires that should beindependent of so let us assume p to be of the following form Where is an arbitrary constant. Puttingpinto equations (21) and (22)

    Solving equation (24) we get

    Load along the crack faces is zero so the traction vector along the crack line is

    Normal vector of the crack faces in R is

    So by the relation between and we get boundary conditions is already zero. By the second boundary condition we get

    This equation should be true for all values of so we get From third boundary condition we get

    (22)

    (23)

    (24)

    (25)

    (26)

    (27)

    (28)

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    So we get the condition

    After putting the value of p in equation (22) we get the condition

    There is one additional boundary condition

    should correspond to simple shear at large

    distances from the crack tip i. e.

    Here krepresents the amount of shear. Now the problem is to find such that it satisfies (29),(30) and (31). Oone more condition on is that it should be bounded near the crack tips. For the

    Neo-Hookean material the value of W is given by

    Using this value the equation (30) converts to

    And the value of stresses areis,

    () ()The global solution of this problem is given by

    So the values of stresses are

    ( )

    (29)

    (30)

    (31)

    (32)

    (33)

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    (

    )

    Resultant shear stress is

    The near tip approximation of near the right crack tip isdenoted by and is given as,

    ( ) If the problem is solved using the linear theory than near tip approximation of is found to besame as that obtaind above. So we shall use this value (37) to compare with exact value of (36)to get a measure of non linearity of the problem.

    4.2 Condition for the nonlinearity to be small scale:

    4.2.1 level nonlinear zone (: If represents the specified error tolerance than for thiscrack problem the inequality

    represents the set of all points (for which the elastic field is approximately non linear at level (because is non linear and is linear). Putting values from equations (35) and (36) weget Figures below show level nonlinear zone (for different values of k. It can be seen that

    (34)

    (35)

    (36)

    (37)

    (38)

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    different

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    Figure 4: level nonlinear zone (, k=0.9

    Figure 5: level nonlinear zone (, k=

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    Figure 6: level nonlinear zone (, k=For k , contains two bounded, connected subsets and such that +while contains right (left) crack tip. In this case we say that nonlinear effect iscontained. And for is unbounded.4.2.2 level near tip linear zone for right crack tip (:This represents set of all points forwhich relative error commitedcommittedby near tip approximation to the resultant shear stressis in magnitude at most i. e. set of all points for which| | Putting values

    ./ Figures ??????? below show the

    level near tip linear zone

    for

    and

    . The

    region between the outer and inner curve is , the middle curve is the locus of all points whereand are exactly equal. The matlab code for the curves of sections 4.2.1 and 4.2.2 havesbeenincluded in the appendix.

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    Figure 7: Near tip linear zone ,

    Figure 8: Near tip linear zone , We say that the nonlinear effect is small scale if it is contained and

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    Since the problem is symmetric about the

    axis so if we satisfy either of the condition of

    equation (40) the other will be satisfied automatically so we take first condition

    If and represents the intersection of the and with the axis respectively then

    by equation (41)

    Now we shall determine and explicitly. A point ( belongs to if and only if and equation (38) holds with | | i. e. if and only if

    | | | |

    And So coincides with the interval

    A point ( belongs to if and only if and equation (39) holds with || | |i. e. if and only if

    ./ | |||

    (40)

    (41)

    (42)

    (43)

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    .

    / | |||

    ./ | |||

    ./ 0 , -1

    ./ | |||

    ./ | ||| 0 , -1 So coincides with the interval

    0 , -1

    0 ,

    -1

    We can verify that

    From equation (42), (43) and (45) it follows that

    (44)

    (45)

    (46)

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    So from above two equations we can write

    { } We can show that for all values of between 0 and 1 first entry is smaller than second soequation (47) may be written as

    Now we have shown that if the nonlinear effect is small scale at level

    then k must satisfy the

    condition (48). It can also be shown that equation (48) is sufficient as well as necessary forequation (42) and also that equation (42) implies equation (41). So it follows that equation (48)

    supplies necessary as well as sufficient condition to be satisfied by the amount of shear at infinity

    k if the nonlinear effect in the crack problem considered to be small scale at level .

    (47)

    (48)

    (49)

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    FINITE STRAIN DEFORMATION NEAR THE TIP OF CRACK IN

    HYPERELASTIC SOLIDS

    Abstract:

    Analysis of cracked bodies is a very important subject from the point of view of

    fracture. Linear elastic fracture mechanics is used for the analysis of most cracked

    bodies. This theory is valid for the elastic bodies undergoing small deformations.

    Here in this report, by relaxing the assumption of small strains the crack problem

    has been analyzed for hyperelastic material which shows large deformations. The

    body has been assumed to be deforming in anti plane shear. A condition has also

    been derived under which the error committed by linear approximation of finite

    deformation problem will be less than a specified value.

    Keywords:Large deformation, Cauchy stresses,Hyperelastic,Neo-hookean

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    CHAPTER 1 INTRODUCTION

    Finite deformation problems always give a nonlinear solution which is complex to

    analyze and in case of cracked bodies it is even more complex. So our motivation is

    always to solve such problems by linear theories which are simpler but they may

    lead to errors and in some cases they may give ambiguous results. If we have a

    condition under which non linearity will be small in the crack problem then we can

    apply linear theories without exceeding a specified error level. In this report we

    derive such condition for finite anti plane shear of an infinite body containing a

    crack of finite length.

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    CHAPTER 5 CONCLUSION

    From equation (48) it can be inferred if the value of

    is higher then the upper limit

    on k will also be higher for the nonlinear effect to be of small scale for that level of, it is expected because if the deformation is large then nonlinearity will also belarge and the error due to linaer approximation will be large.

    If the crack is not symmetric about axis then two conditions of equation (40) arenot equivalent to each other and the nonlinear effect might be small scale at one

    crack tip and not at the other. If the material used is not Neo-hookean then

    expression for W will be different and the results derived will not be valid. This

    remark also holds if the crack is deformed in mode I or mode II rather than in mode

    III (anti plane shear).

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    CHAPTER 2 REVIEW OF LITERATURE

    Recently much work has been done on the study of deformations and stresses near the tip of

    crack for hyperelastic materials.

    [4] did asymptotic analysis of deformations and stresses in traction free crack in infinite slab

    under plane strain. They assumed uniform axial tension at infinity at right angles to the faces of

    crack.

    [2] Did analysis of crack in finite anti-plane shear in an infinite slab. He took the material to be

    Neo-hookean.

    [5] Did the asymptotic analysis of traction plane crack under plane strain condition. He took the

    power law materials (which in a special case converts to Mooney-Rivlin material.

    [6] Did the asymptotic analysis of traction free interface crack between two dissimilar semi

    infinite Neo-hookean sheets.

    [1] Did the analysis of anti-plane shear problem in crack and derived the condition for the

    nonlineasr effect to be small scale.

    [7] Did the asymptotic analysis of traction free crack at interface of two semi infinite slabs

    bonded under the conditions of plane strain.

    [8] Did the asymptotic analysis of stress and strain near the tip of a crack with generalised Neo-

    hookean material. He assumed the crack to be deforming in mode I and mixed mode.

    [9] Did analysis of interface crack between, (1) two generalised Neo-hookean sheets having same

    hardening characteristics and (2) a generalised Neo-hookean sheet and a rigid substrate.

    [10] Did the analysis of motion field surrounding a rapidly propagating crack which is loadedsymmetrically in mode I conditions.

    In this seminar anti-plane shear problem for Neo-hookean material has been studied because this

    is the simplest problem to solve.

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    Appendix I Matlab Code For Section 4.2.1 and 4.2.2

    %create the following function files

    functioncrak=sem(x,y)syms xycrak=1.5^4*(x.^4+y.^4+2*x.^2*y.^2)-(x.^2+1-2*x+y.^2)*(x.^2+1+2*x+y.^2)

    functioncrac2=sem2(x,y)syms xye=0.67crac2=2*(x.^2+y.^2)*(1+e.^2-2*e)-(x.^2+1+2*x+y.^2)^0.5

    functioncrac2=sem4(x,y)syms xye=0.67crac2=2*(x.^2+y.^2)-(x.^2+1+2*x+y.^2)^0.5

    functioncrac2=sem3(x,y)syms xye=0.67

    crac2=2*(x.^2+y.^2)*(1+e.^2+2*e)-(x.^2+1+2*x+y.^2)^0.5%give the following commands

    ezplot (sem,[-4,4])

    %and separatelyezplot (sem2,[-10,10]);hold on

    ezplot (sem3,[-10,10]);hold on

    ezplot (sem4,[-10,10])

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    REFERENCES

    [1] J. K. Knowles, A. J. Rosakis (1986), On the scale of nonlinear effect in a

    crack problem, Journal of Applied Mechanics, 53, 545-549.

    [2] J. K. Knowles (1977), The finite anti plane shear field near the tip of a crack

    for a class of incompressible elastic solids, Journal of Elasticity, 13, 611-639.[3] C. S. Jog (2007) Foundations and applications of mechanics, volume 1:

    continuum mechanics, 2E, Narosa Publication House.

    [4] Knowles, Sternberg (1973), An asymptotic finite deformation analysis of the

    elastostatic field near the tip of a crack, Journal of Elasticity, 3, 67-107.[5] Rodney A. Stephenson (1982), The equilibrium field near the tip of a crack

    for finite plane strain of incompressible elastic materials, Journal of

    Elasticity, 12, 65-99.

    [6] Knowles, Sternberg (1983), Large deformation near a tip of an intrerfacecrack between the Neo-Hookean sheets, Journal of Elasticity, 13, 257-293.

    [7] J.M.Herrmann (1989), An asymptotic analysis of finite deformations near thetip of an interface crack, Journal of Elasticity, 21, 227-269.

    [8] Philippe H. Geubelle (1994), Finite strains at the tip of a crack in a sheet ofhyperelastic material: I. homogeneous case, Journal of Elasticity, 35, 61-98.

    [9] Philippe H. Geubelle (1994), Finite strains atthe tip of a crack in a sheet ofhyperelastic material: II. Special biomaterial case, Journal of Elasticity, 35,

    99-137.[10] Angelo Marcello (1999), Large deformation near a tip of an intrerface crack

    between the Neo-Hookean sheets, Journal of Elasticity, 57, 85-103.

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