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Tutorial I: Mechanics of Ductile Crystalline Solids

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Title: Tutorial I: Mechanics of Ductile Crystalline Solids


1
Tutorial IMechanics of Ductile Crystalline
Solids
  • Alberto M. Cuitiño
  • Mechanical and Aerospace Engineering
  • Rutgers University
  • Piscataway, New Jersey
  • cuitino_at_jove.rutgers.edu

IHPC-IMS Program on Advances Mathematical
Issues in Large Scale Simulation (Dec 2002 - Mar
2003 Oct - Nov 2003)
Institute of High Performance Computing
Institute for Mathematical Sciences, NUS
2
Hierarchy of Scales
SCS test
ms
Grains
Single crystals
time
µs
Microstructures
ns
Force Field
nm
µm
mm
length
3
The Role of Dislocations
ELASTICITY
Initial
PLASTICITY
area swept by dislocation
Dislocation Motion
Dislocation Generation
4
Anatomy of a Dislocation Loop
Edge
Mixed
Screw
Mixed Segment
Edge Segment
b burgers vector
Glide Plane
Screw Segment
Area swept by dislocation loop
Animations from http//uet.edu.pk/dmems/
5
Dislocation Motion and Arrest
6
Tracking Dislocation in ONE Plane
(Ortiz, 1999)
7
Overview
Effective Dislocation Energy
  • Core Energy
  • Dislocation Interaction
  • Irreversible Obstacle Interaction

Equilibrium configurations
  • Closed form solution at zero temperature.
  • Metropolis Monte Carlo algorithm and mean field
    approximation at finite temperatures.

Macroscopic Averages
8
Effective Energy
Elastic interaction
Core energy
External field
where
with
m
Displacement jump across S
Slip Surface S
9
Elastic interaction
  • Displacement field
  • Elastic distortion
  • Elastic interaction
  • Green function for an isotropic crystal

10
Elastic Interaction
with
A1
R
A2
(Hirth and Lothe,1969)
11
External Field
with
applied shear stress
forest dislocations
12
Core Energy
d inter-planar distance
Ortiz and Phillips, 1999
13
Phase-Field Energy
Minimization with respect to ? gives
core regularization factor
elastic energy
14
Phase-Field Energy
Elastic energy
Core regularization
Core regularization factor
15
Energy minimizing phase-field
Unconstrained minimization problem
if
with
16
Irreversible Process and Kinetics
  • Irreversible dislocation-obstacle interaction
    may be built into a variational framework, we
    introduce the incremental work function

incremental work dissipated at the obstacles
  • Primary and forest dislocations react to form a
    jog
  • Updated phase-field follows from
  • Short range obstacles

17
Irreversible Process and Kinetics
Kuhn-Tucker optimality conditions
Equilibrium condition
18
Solution Procedure
and compute the reactions
  • Stick predictor. Set
  • Reaction projection
  • Phase-field evaluation

19
Closed-form solution
Calculations are gridless and scale with the
number of obstacles
Dislocation loops
20
Macroscopic averages
  • Slip
  • Dislocation density
  • Obstacle concentration
  • Shear stress

21
Forest Hardening
  • Obstacle distribution

Parameters
BOUNDARY CONDITIONS Periodic OBSTACLE STRENGTH
Uniform, f 10 G b2 PEIERLS STRESS tp 0
22
Monotonic loading
Evolution of dislocation density with strain.
Stress-strain curve.
23
Dislocation Patterns
Evolution of dislocation pattern as a function of
slip strain
24
Interaction with Obstacles
Detail of the evolution of the dislocation
pattern showing dislocations bypassing a pair of
obstacles
25
Fading memory
a
b
d
c
Stress-strain curve.
e
f
Three dimensional view of the evolution of the
phase-field, showing the the switching of the
cusps.
26
Cyclic loading
a
b
c
Stress-strain curve.
d
e
f
Evolution of dislocation density with strain.
i
g
h
27
Irreversibility/Cyclic Loading
28
Poisson ratio effects
Evolution of dislocation density with strain.
Stress-strain curve.
Stress-strain curve
Dislocation density vs.strain
b
29
Obstacle density
30
Multiple Glide
31
Some Concluding Remarks
  • The aim of this study is to develop a phase-field
    theory of dislocation dynamics, strain hardening
    and hysteresis in ductile single crystals.
  • This representation enables to identify
    individual dislocation lines and arbitrary
    dislocation geometries, including tracking
    intricate topological transitions such as loop
    nucleation, pinching and the formation of Orowan
    loops.
  • This theory permits the coupling between slip
    systems, consideration of obstacles of varying
    strength, anisotropy, thermal and strain rate
    effects.

Ortiz,1999
32
Summary
  • Phase-field model.
  • Closed form solution at zero temperature.
  • Temperature effects.
  • Strain rate effects.
  • Dislocation structures in grain boundaries.
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