Defects VIII - Dislocation Motion and Generation

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  • 8/9/2019 Defects VIII - Dislocation Motion and Generation

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    3.4 Dislocation motionand generation

    Hartmut S. Leipner: Defects in crystals

    ! Slip of crystals

    ! Velocity of dislocations

    ! Peierls energy

    ! Frank–Read source

    ! Cross slip of screw dislocations

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    hsl 2009 – Defects in crystals – 3.4 Dislocation motion

    Concept of slip

    !   Glide – conservative motion of dislocation in the surface which contains both its line and Burgers vector 

    !   Climb – nonconservative motion out of the glide surface normal to the

    Burgers vector ! Glide of many dislocations results in slip, the manifestation of plastic

    deformation of crystals! Slip planes are normally the planes with highest density of atoms,

    direction of slip the direction of closest spacing

    ! Slip plane + slip direction: slip system

     Examples:

    hcp (0001) basal planes, directions1210

    fcc {111}110 – 

     – 

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    hsl 2009 – Defects in crystals – 3.4 Dislocation motion

    Resolved shear stress

    Geometry of slip

    Shear stress resolved on the slipplane in the slip direction:

    Schmid factor m = cos ! cos  !

    Min. stress required for the onset of slip:

    critical resolved shear stress

    [Hull, Bacon 1992] SlipSalami

     F

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    hsl 2009 – Defects in crystals – 3.4 Dislocation motion

    !

    Dislocations of opposite sense glidein opposite directions! For dislocation glide, a shear stress

    must act on the slip plane in the

    direction of the Burgers vector

    !

    The direction of the motion isgiven by the Peach–Koehler

    formula, F d = (! ·b)"# 

    Direction of dislocation glide

    [Hull, Bacon 1992] Glide direction

    b

    b

    b

    b

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    hsl 2009 – Defects in crystals – 3.4 Dislocation motion

    Measurement of the dislocation glide velocity 

    Etch pits LiF modified

    Dislocation etch pits on a LiF crystal. The crystal has been etched threetimes. The movement of dislocation B under two subsequent stress pulsesis indicated by the pits. Dislocations A did not move.

    [Gilman, Johnston 1957/Hull, Bacon 1992]

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    hsl 2009 – Defects in crystals – 3.4 Dislocation motion

    In situ observation of dislocation glide

    Disloc_TEMmpgMisfit loop

    Thermal activation of dislocation glide by heating of the specimeninside the transmission electron microscope to a temperature of 680 °C

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    hsl 2009 – Defects in crystals – 3.4 Dislocation motion

    Velocity of dislocations

    ! Different velocities for different types of dislocations

    ! Critical stress for the onset of glide (CRSS)

    ! Strongly material dependent

    ! Strong dependence on purity of materials (doping)

    ! Speed of sound upper limit for dislocation velocity

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    hsl 2009 – Defects in crystals – 3.4 Dislocation motion

    Velocity of dislocations

    Stress dependence of dislocation velocity in LiF[Gilman, Johnston 1959/Hull, Bacon 1992]

    Dislocation velocity LiF

    Stress (MPa)

       D   i

      s   l  o  c  a   t   i  o  n  v  e   l  o  c   i   t  y   (  c  m   /  s   ) Velocity of  (110)[110] shear waves

     –

    3·105 cm/s

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    hsl 2009 – Defects in crystals – 3.4 Dislocation motion

    Dislocation velocity in III–V compounds

    Dislocation velocities in undopedGaAs and InP

    [Sumino 1992]

    Dislocation velocity GaAs InP

    m Q/eV

    GaAs 1.6…1.8 1.3…1.4

    InP 1.4…1.8 1.6…1.7

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    hsl 2009 – Defects in crystals – 3.4 Dislocation motion

    Peierls model of the dislocation core

    Displacement of atoms u at an edgedislocation. The lower panel shows thedisplacement difference !u across theslip plane (disregistry).

    [Hull, Bacon 1992]

    !u = u(B)!

     u(A)dislocation width w: disregistrygreater than one half of itsmaximum value

    Peierls model

    ub

    !u/b

     x

     x

     y

    w

    u

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    hsl 2009 – Defects in crystals – 3.4 Dislocation motion

    Peierls barrier

    ! Disregistry core energy, resistance to dislocation movement

    ! Simple approach (Peierls–Nabarro model): sinusoidal force relationbetween planes A, B

    ! Calculation of the dislocation core energy per unit length as a functionof the dislocation position

    !

    Maximum: Peierls energy

    ! Peierls stress: resolved shear stress required to move a dislocation in theperfect crystal

    ! Direct consequence of the lattice periodicity

    !   ! P depends on the core structure

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    hsl 2009 – Defects in crystals – 3.4 Dislocation motion

    Peierls potential

     E 

     x

    Peierls valleys

    (dislocation equilibriumposition at 0 K)

    Closed packeddirection

    h

     E P

    Dislocation positionat finite temperature

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    hsl 2009 – Defects in crystals – 3.4 Dislocation motion

    Double-kink nucleation

    S 11-91 double kink

    ! Thermally activated process of double-kink nucleation at T  > 0

    ! Minimum spacing XY required, typically 20b

    Kink jump frequency

    Kink diffusivity

    Kink velocity Dislocation velocity

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    hsl 2009 – Defects in crystals – 3.4 Dislocation motion

    Frank–Read source

    S18-90 Frank Read source

    ! Radius of curvature depends on resolved shear

    ! Critical bow out for  R =  L/2 ( L = AB)  !  ! Gb/ L

    ! Further steps are the formation of a kidney-shaped loop and the annihilation of

    dislocation segments with the same Burgers vector but opposite line sense.

     A

    B

     A

    B

     A

    B

     A

    B B

     A A

    B

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    hsl 2009 – Defects in crystals – 3.4 Dislocation motion

    Dislocation source in deformed silicon

    TEM weak-beam image of dislocations in deformed silicon. The lengthof the Frank–Read source amounts to 2 µm.

    [George, Rabier 1987]

    Frank Read source in Si

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    hsl 2009 – Defects in crystals – 3.4 Dislocation motion

    Cross slip

    ! In principle, screws can glide on any slip plane! In praxi, closed packed planes preferred

    ! Screw can switch from one plane to another: cross slip

    [Hull, Bacon 1992] Xslip1

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    hsl 2009 – Defects in crystals – 3.4 Dislocation motionJogs

    Jogs and kinks

    [Hull, Bacon 1992]

    Kinks and jogs

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    hsl 2009 – Defects in crystals – 3.4 Dislocation motion

    Intersection of edge dislocations

    [Read 1953/Hull, Bacon 1992] Jog1

    The formation of the jog after the

    cutting of edge dislocations with b1 ! b2 

    can be envisaged by considering the

    displacement of the plane PAB  produced

    by the dislocation XY.

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    hsl 2009 – Defects in crystals – 3.4 Dislocation motion

    Formation of kinks by dislocation intersection

    Intersection of edge dislocations with b1 || b2

    [Hull, Bacon 1992] Jog2

    " Jogs (kinks) in pure edge dislocationsdo not affect the glide motion.

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    hsl 2009 – Defects in crystals – 3.4 Dislocation motion

    Intersection of screw dislocations

    Generation of jogs by the intersection of an edge dislocation with a right-handed screw

    (left) and by the intersection of two screw dislocations (right).

    (a) (b)

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    hsl 2009 – Defects in crystals – 3.4 Dislocation motion Jog5

    The jog PP’ is a short edge segment and can only glide in the

    PP’R’R plane. The movement of the screw to A’B’ requires the

    climb of the jog along PQ.

    [Hull, Bacon 1992]

    Motion of a jog on a screw dislocation

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    hsl 2009 – Defects in crystals – 3.4 Dislocation motion

    Influence of jog height – Superjogs

    ! Elementary jogs produce

     point defects pd (vacancy

     jogs/interstitial jog)

    !   Superjogs: Dislocation

    segments XM, NY can

    move independently

    ! Intermediate jog: Segments

    NP and MO cannot pass,

    formation of a stable

    dislocation dipole

    [Gilman, Johnston 1962/Hull, Bacon 1992] Jog7

    pd

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    hsl 2009 – Defects in crystals – 3.4 Dislocation motion

    Glide of a jogged screw dislocation producing trails of point defects

    Jog6

     Jog dragging