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Defects Elasticity Theory

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    3.2 Elasticity theory of dislocations

    Basics of linear elasticity theory

    Stress field of a straight dislocation

    Strain energy

    Forces on dislocations

    Hartmut S. Leipner: Defects in crystals

    (Dislocation core structure)

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    hsl 2008 Defects in crystals 3.2 Elasticity theory

    Displacement vectoru = (ux, uy, uz)

    Nine components of the strain tensor

    ij

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    hsl 2008 Defects in crystals 3.2 Elasticity theory

    Considering a small cubic volume element in a solid, the total stress state

    can be described by the forces perpendicular and parallel to the faces ofthe cube.

    On each face, three stresses: 1 normal ii, 2 shearij(ij; i,j =x,y,z) All together nine components of the stress

    Stress in the solid

    3

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    hsl 2008 Defects in crystals 3.2 Elasticity theory

    Stress tensor

    Stress tensor is symmetrical, ij

    = ji

    (rotational equilibrium).

    Magnitude of the individual components depends on the orientation of

    the coordinate system.

    A special coordinate system can always be found, where there are only

    normal stresses,

    Positive normal stress as tension

    Hydrostatic pressure is the average normal stress,

    4

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    hsl 2008 Defects in crystals 3.2 Elasticity theory

    Strain

    Generally, the elastic deviation of the shape of the solid can beexpressed as astrain tensor,

    ii elongations, ij shear (ij)

    Strain tensor also symmetrical

    5

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    hsl 2008 Defects in crystals 3.2 Elasticity theory

    Stressstrain relationships

    Stress as force per unit area of surface; consider orientationof the surface and direction of the force Uniaxial tension =, shear = G Special cases ofHookes law

    Relation between stress and strain tensors

    Expression of 9 equation like

    Chas 34 = 81 components Cijkl(4th rank tensor)

    6

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    hsl 2008 Defects in crystals 3.2 Elasticity theory

    Elastic constants C

    In praxi, number of constants is reduced due to symmetry. For isotropic solids only two parameters (e.g.G and Lam constant )

    In cubic crystals, three constants are needed.

    ~

    7

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    hsl 2008 Defects in crystals 3.2 Elasticity theory

    Elastic moduls

    Other constants to be used: Youngs modulus, Poissons constant ,and bulk modulusK,

    Poissons constant

    Elongation inx-direction connected with reduction of cross section

    yy = zz=xx

    ~

    8

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    hsl 2008 Defects in crystals 3.2 Elasticity theory Strain field screw

    Volterra screw dislocation [Hull, Bacon 1992]

    Representation as a cylinderof elastic material

    Slit LMNO ||zaxis, surfacedisplaced by b

    Displacements:

    ux = uy = 0

    Strain field of a straight screw dislocation

    bb

    Cylinder with radius r0

    not taken into account:

    assumptions oflinearelasticity theory not valid

    9

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    hsl 2008 Defects in crystals 3.2 Elasticity theory

    Simpler form in cylindrical coordinates:

    Using rz=xzcos+ yzsin z= xzsin+ yzcos

    (the only non-zero

    components)

    Straight screw dislocation

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    hsl 2008 Defects in crystals 3.2 Elasticity theory

    Strain and stress 1/r, diverge withr 0

    Linear elasticity approach not valid at the center of the dislocation

    Dislocation core with atomistic model Theoretical stress limit reached atrb

    Reasonable core radius 1 nm

    Discussion of the strain and stress fields

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    hsl 2008 Defects in crystals 3.2 Elasticity theory Strain field edge

    Volterra edge dislocation[Hull, Bacon 1992]

    bb

    Stress field of a straight edge dislocation

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    hsl 2008 Defects in crystals 3.2 Elasticity theory Stress field edge dislocation

    Contours of equal stress

    about an edge dislocation[Hirth, Lothe 1992]

    Stress field contours of an edge dislocation

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    hsl 2008 Defects in crystals 3.2 Elasticity theory

    Deformation is basically a plane strain. Both dilatational and shear components exist.

    Largest normal stress xx || Burgers vector

    Max. compressive stress immediately abovey = 0 (slip plane)

    max. tensile stress immediately belowy = 0

    Pressure on a volume element

    Stress field of an edge dislocation

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    hsl 2008 Defects in crystals 3.2 Elasticity theory

    Elastic strain energy in theory of elasticity:

    Two parts of the total strain energy of a body containing a dislocation:E=Ecore +Eel

    Strain energy of a dislocation

    (Total elastic energy per unit length)

    Elastic energyper unit length of a screw:

    15

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    hsl 2008 Defects in crystals 3.2 Elasticity theory

    Strain energy of an edge more complicated to calculate(lower symmetry)

    Elastic energy of an edge dislocation higher by about 3/2 than that of a screw

    Eeldepends onr0andR(core radius and cut-off radius). Example:G = 41010 Nm2, r0 = 1 nm,R = 1 mm, b = 0.25 nm

    Eel 6 eV per unit length of a dislocation

    R corresponds to crystal dimensions.

    For many dislocations in a crystal,

    superposition of the long-range strain fields

    Discussion of the strain energy

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    hsl 2008 Defects in crystals 3.2 Elasticity theory Elastic energy screw

    Elastic energy of dislocations

    r

    Elastic energy in a ring cylinder of the thickness dr

    17

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    hsl 2008 Defects in crystals 3.2 Elasticity theory

    Superposition of edge and screw parts

    EelGb2, with 0.51.0

    Shortest lattice translation vectors

    preferred asEelis min.

    Splitting of a dislocation withb1 = 2ainto two dislocations,E1 4a

    2,E2 2a2

    [Bohm 1992]

    Dislocation splitting

    Energy of mixed dislocations

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    hsl 2008 Defects in crystals 3.2 Elasticity theory

    + =

    b1

    b2

    b3

    b1+ b

    2= b

    3

    Energy criterion for dislocation reaction

    Reaction favorable

    Condition with angle:! /2 < Reaction preferred0 < /2 Dissociation preferred

    Franks rule

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    hsl 2008 Defects in crystals 3.2 Elasticity theory

    Elementary process of plastic deformation

    The motion of dislocations is the elementary process of the plastic deformationof crystals. is here the shear stress.

    20

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    hsl 2008 Defects in crystals 3.2 Elasticity theory

    External forces on dislocations

    Dislocation separates slipped regionfrom unslipped one

    Deformation work may be done by

    external force shift of the dislocation

    Plastic deformation by motion of a dislocation[Kelly:2000]

    Screw motion

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    hsl 2008 Defects in crystals 3.2 Elasticity theory

    Dislocation of lengthL, swept distance on the slip planex

    Applied shear force on the crystal (per lengthL): F= x

    Work done by the crystal (per lengthL): W= x b

    L

    x

    b

    Definition of a force (per lengthL) to move the dislocation in

    x-direction: workW= force on dislocation x

    Fd = b

    Pure motion in the glide plane

    Fd = b (per unit lengthL)

    Definition of force

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    hsl 2008 Defects in crystals 3.2 Elasticity theory

    PeachKoehler force

    General case of a shear force on a crystal: F= n

    (n unit vector of the swept-out surface, n =u, with line vector, direction of motion u)

    Displacement by Burgers vectorb if dislocation moves

    Work done by the crystal:

    W= (n)b =(b)n

    W= (b)(u) = (b)u

    PeachKoehlerforce Fd = (b)

    Force acting on a plane perpendicular to b || dislocation: Fd always normal to the dislocation

    Force to move the dislocation in the direction u

    (All eq. are given per unit length of dislocationL.)

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    hsl 2008 Defects in crystals 3.2 Elasticity theory

    Strain energy proportional to the length,

    increase in length causes increase in energyExistence of a line tension trying to reduce the line

    lengthTo be defined via the increase in energy per unit

    length T= Gb2

    [Bohm 1992]

    Line tension

    Line tension

    Calculation of the shear stress 0 to maintaina certain radius of curvatureR

    Inward force:Ks = 2Tsin(/2),

    for small angles: dKs = Td

    Outward force on segment ds due to appliedstress is 0 bds

    Equilibrium: Td= 0 bds (ds =Rd)

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    hsl 2008 Defects in crystals 3.2 Elasticity theory

    Edge dislocations with the same slipplanerepulsive force ifbhas the same

    sign, attractive if opposite sign More complicated, if slip planes

    different Displacement in dislocation I is

    Burgers vectorb of dislocation II

    Interaction between edge dislocations

    Forces between dislocations

    y

    x

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    hsl 2008 Defects in crystals 3.2 Elasticity theory

    Calculation of the force

    Components of the force on dislocation II per unit length(bx = b, by = bz= 0):

    y

    Fx

    Fy

    x

    I

    II

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    F b ll l d di l i

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    hsl 2008 Defects in crystals 3.2 Elasticity theory Forces between edge dislocations

    Force between parallel edge dislocations. Unit of forceFx is Gb2y/[2(1 )].

    Curve A for like dislocations, curve B for unlike dislocations.[Hull, Bacon 1993/Cottrell 1953]

    Force between parallel edge dislocations

    27

    I t ti f b t d di l ti

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    hsl 2008 Defects in crystals 3.2 Elasticity theory Forces between edge dislocations

    Dislocations motion only in the slip plane

    most importantFx

    Forx > 0,Fx < 0 (attractive) ifx 0 (attractive) ifx


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