Lecture Micromechanics texture SFB 761
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Transcript of Lecture Micromechanics texture SFB 761
Why does a crystal rotate ?Why does a crystal rotate ?Dierk Raabe
Düsseldorf, Germany
SFB Class 2012
OverviewOverview
Roters et al. Acta Materi.58 (2010) 1
2
Some dislocation kinematics and kinetics: phenomenaSome dislocation kinematics and kinetics: phenomena
true strain
stress
3
Plastic deformation of a single crystal by dislocation slipPlastic deformation of a single crystal by dislocation slip
4
Plastic deformation of a single crystal by dislocation slipPlastic deformation of a single crystal by dislocation slip
5
Plastic deformation of a single crystal by dislocation slipPlastic deformation of a single crystal by dislocation slip
6
Plastic deformation of a single crystal by dislocation slipPlastic deformation of a single crystal by dislocation slip
bvtZ
bXxn
t md1d
dd
7
Plastic deformation of a single crystal by dislocation slipPlastic deformation of a single crystal by dislocation slip
S h id f tSchmid factor(orientation factor for that slip system)
8
Plastic deformation of a single crystal by dislocation slipPlastic deformation of a single crystal by dislocation slip
Plastic deformation of a single crystal by dislocation slipPlastic deformation of a single crystal by dislocation slip
Boundary condition: determines lab frame constraintsBoundary condition: determines lab frame constraints
11
Single crystal plasticity: crystal shear and crystal rotationSingle crystal plasticity: crystal shear and crystal rotation
12
Plastic deformation of a single crystal by dislocation slipPlastic deformation of a single crystal by dislocation slip
bvtZ
bXxn
t md1d
dd
13
u=u(x y z)
Kinematics, displacementKinematics, displacement
u u(x,y,z)
1 2
(x(1),y,z) (x(2),y,z)
1 2
u(1)(x,y,z) u(2)(x,y,z)u (x y z)=u (x y z)
1 2
u(1)(x,y,z)=u(2)(x,y,z)
1 2
14
u=u(x y z)
Kinematics, displacementKinematics, displacement
u u(x,y,z)
1 2
(x(1),y,z) (x(2),y,z)
1 2
u(1)(x,y,z) u(2)(x,y,z)u (x y z)≠u (x y z)
1 2
u(1)(x,y,z)≠u(2)(x,y,z)
1 2
15
1 2
Kinematics, displacement, displacement gradient: generalKinematics, displacement, displacement gradient: general
16
Kinematics: Micro-to-macro-transitionKinematics: Micro-to-macro-transition
17
Geometrical interpretationGeometrical interpretation
?
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Geometrical interpretationGeometrical interpretation
19
Complex boundary conditionsComplex boundary conditions
one dislocationmesoscopic boundary conditions(grain / orientation neighborhood)one dislocation
parallel loops
(grain / orientation neighborhood)
parallel loops
reactions
20
orientation change
Simplify boundary conditionsSimplify boundary conditions
Boundary conditions:
1) Upper bound treatment: iso-stress
2) Lower bound treatment: iso-strain2) Lower bound treatment: iso strain
21
sym sym sym sym
Iso-stress: single slip systemIso-stress: single slip system
a a
krit
b b
krit
d d
krit
c c
kritc b d a
m m m msym sym sym sym
1
D
33
T D33
T
a D
b
cD
kritaktiv
c
11
d
22
Single crystal plasticity: multiple slip (or twinning) systemSingle crystal plasticity: multiple slip (or twinning) system
mit
/
/mit
23
Single crystal yield surfaceSingle crystal yield surface
critijljlkik bana
1 crystal, 1 slip system: 33
slip system 1
same strain
jj
active)(1crits
..
33
differentstresses
11
slip system 2
active)(2crits
activecrit
critss bana
1 crystal, 2 slip systems:
11
ijljlkik bana
Ds=1
Iso-stress: multiple slip (or twinning) systemIso-stress: multiple slip (or twinning) system
33
Ds=2D
krit (+)aktiv)s1 (
..Vers
krit,(+) TBH
S
11
krit,(+)aktiv)s2 (
.
krit,(-)s2
krit,(-)aktiv)s1 (
.
VersDs=2
bcc fcc Bcc: 24 systems
Single crystal plasticitySingle crystal plasticity
kr
itbcc, fcc,
Section in stress space
Bcc: 24 systems
krit
krit krit
BCC, 48 systems
kr
it
krit
26
Simplify boundary conditionsSimplify boundary conditions
Boundary conditions:
1) Upper bound treatment: iso-stress
2) Lower bound treatment: iso-strain2) Lower bound treatment: iso strain
27
The Taylor ModelThe Taylor Model
28
Crystal yield surface, Taylor Bishop-HillCrystal yield surface, Taylor Bishop-Hill
29
Crystal yield surface, Taylor Bishop-HillCrystal yield surface, Taylor Bishop-Hill
Many crystals many slip systems:
33grain 1
Many crystals, many slip systems:
grain 2
grain 3g
grain 4
imposed strain
11
3% 8%
Homogeneity and boundary conditions – meso-scaleHomogeneity and boundary conditions – meso-scale
3% 8%
15%
Simplify boundary conditionsSimplify boundary conditions
Boundary conditions:
1) Upper bound treatment: iso-stress (strain not compatible)
2) Lower bound treatment: iso-strain (forces not in equilibrium)2) Lower bound treatment: iso-strain (forces not in equilibrium)
32
Multiscale crystal plasticity FEM or FFTMultiscale crystal plasticity FEM or FFT
33Raabe, Zhao, Park, Roters: Acta Mater. 50 (2002) 421
Crystal Mechanics FEM, grain scale mechanics (2D)Crystal Mechanics FEM, grain scale mechanics (2D)
Experiment (DIC, EBSD)v Mises strain
Simulation (C )(CP-FEM)
v Mises strain
SachtleberSachtleber, , Zhao, Raabe: MaterZhao, Raabe: Mater. . Sc. Sc. EnginEngin. A 336 (2002) 81. A 336 (2002) 81 34