1.021 , 3.021, 10.333, 22.00 I ntroduc tion to Modeling and Simulation
Spring 2011
Part I – C ontinuum and partic le me thods
How to model chemical interactions II
Lecture 6
Markus J. Buehler
1
Laboratory for Atomistic and Molecular Mechanics Department of Civil and Environmental Engineering Massachusetts Institute of Technology
Content overview
I. Particle and continuum me thods
1. Atoms, molecul e s, chemistry
2. Continuum modeling approac hes and solution approaches
3. Statistical mechanics
4. Molecular dynamics, Monte Carlo
5. Visualization and data analysis
6. Mechanical proper ties – applic ation: how things fail (and how to prevent it)
7. Multi-scale modeling par adigm
8. Biological systems (simulation in biophysics) – h ow proteins work and how to model them
II. Quantum mechanical methods
1. It’s A Q uantum World: T he Theory of Quantum Mechanics
2. Quantum Mechanics: Practice Makes Perfect
3. The Many-Body Problem: Fr om Many-Body to Single- Particle
4. Quantum modeling of materials
5. From Atoms to Solids
6. Basic pr operties of mater i als
7. Advanced proper ties of materials
8. What else can we do?
Lectures 2-13
Lectures 14-26
2
Overview: Material covered so far…
Lecture 1: Broad introduction to IM/S
Lecture 2 : Introduction to atomistic and continuum modeling (multi-scale modeling paradigm, difference between continuum and atomistic approach, case study: diffusion)
Lecture 3 : Basic statistical mechanics – p roperty calculation I (property calculation: microscopic states vs. macroscopic properties, ensembles, probability density and partition function)
Lecture 4 : Property calculation II (Monte Carlo, advanced property calculation, introduction to chemical interactions)
Lecture 5: How to model chemical interactions I (example: movie of copper deformation/dislocations, etc.)
Lecture 6: How to model chemical interactions II 3
Lecture 6: How to model chemical interactions II
Outline:
1. Cas e study: Deformation of copper wire (cont’d)
2. How to model metals: Multi-body potentials
3. Brittle versus ductile materials
4. Basic deformation mechanism in brittle materials - c rack extension
Goal of today’s lecture:
Complete example of copper deformation
Learn how to build a model to describ e brittle fracture (from scratch)
Learn bas ics in fracture of brittle materials
Apply our tools to model a particu lar material phenomena – b rittle fracture ( useful for pset #2 )
1. Case study: Deformation of copper wire (cont’d)
A simulation with 1,000,000,000 particles Lennard-Jones - copper
Fi g. 1 c from Bu eh ler, M . , et al . "T he Dynami cal Complexity of Work - H arden i n g: A Large-Scale Molecu l a r Dynami cs Simu l a t i on." Ac ta Mech Sinica 21 (2 005): 103-11.
© S prin g e r- V e rlag. A ll r i gh t s r e s e rv ed. T h is c on t en t is ex cl u d e d f r om ou r C r ea t ive C o mm on s 6
lic e n s e. For more infor m at ion, s ee http:/ /ocw. m it.edu/fai ruse .
??
Image by MIT OpenCou r seWare.
Strengthening caused by hindering dis l ocation motion
If too difficult, ductile modes break down and material becomes brittle 7
Fig. 1 c from B u e h l e r, M. e t al. "The D y na mica l Co mp le xity o f Wo rk - H a rdening: A La rge- Sca l e Mo le cu la r D y na mics Simu la tion." Ac ta Me ch Sin i ca 21 (2005) : 10 3 - 111.
© S p r inge r - V e r lag . All r i ghts rese r v ed . Th is content is e x c l uded from ou r 8
C r eative Co mmons license . F o r mo re in fo r m a t ion , see h ttp ://ocw . mit.edu/fa iruse .
Parameters for Morse potential
(for reference)
Morse potential parameters for various metals
Morse Potential Parameters for 16 Metals
Metal |
a 0 |
|
L x 10 -22 (eV) |
|
r 0 |
D (eV) |
Pb |
2.921 |
83.02 |
7.073 |
1.1836 |
3.733 |
0.2348 |
Ag |
2.788 |
71.17 |
10.012 |
1.3690 |
3.1 15 |
0.3323 |
Ni |
2.500 |
51.78 |
12.667 |
1.4199 |
2.780 |
0.4205 |
Cu |
2.450 |
49.1 1 |
10.330 |
1.3588 |
2.866 |
0.3429 |
Al |
2.347 |
44.17 |
8.144 |
1.1646 |
3.253 |
0.2703 |
Ca |
2.238 |
39.63 |
4.888 |
0.80535 |
4.569 |
0.1623 |
Sr |
2.238 |
39.63 |
4.557 |
0.73776 |
4.988 |
0.1513 |
Mo |
2.368 |
88.91 |
24.197 |
1.5079 |
2.976 |
0.8032 |
W |
2.225 |
72.19 |
29.843 |
1.41 16 |
3.032 |
0.9906 |
Cr |
2.260 |
75.92 |
13.297 |
1.5721 |
2.754 |
0.4414 |
Fe |
1.988 |
51.97 |
12.573 |
1.3885 |
2.845 |
0.4174 |
Ba |
1.650 |
34.12 |
4.266 |
0.65698 |
5.373 |
0.1416 |
K |
1.293 |
23.80 |
1.634 |
0.49767 |
6.369 |
0.05424 |
Na |
1.267 |
23.28 |
1.908 |
0.58993 |
5.336 |
0.06334 |
Cs |
1.260 |
23.14 |
1.351 |
0.41569 |
7.557 |
0.04485 |
Rb |
1.206 |
22.15 |
1.399 |
0.42981 |
7.207 |
0.04644 |
Adapted from Table I in Girifalco, L. A., and V. G. Weizer. "Application of the Morse Potential Function to Cubic Metals." Physical Review 114 (May 1, 1959): 687- 690 .
Image by MIT OpenCou r seWare.
( r ij )
D exp 2 ( r ij
r 0 ) 2 D exp ( r ij r 0 )
Morse potential: application example (nanowire)
See: Komanduri , R., et al . " M o l ecu lar D y n a mic s (M D) Sim u la t i on of U n i a xi al Tension of Some Si ngle-Cr ystal Cubi c Metals at Nanolevel ." Int e rn ati o nal Journal of Mech anical Sci e n c es 43, no. 10 (2001): 2237-60.
Further Morse potential parameters:
Courte sy of El se vie r, Inc., h t t p ://www. scien c e dir ec t . c o m . Used wi th permission.
Cutoff-radius: saving time
Cutoff radius
U i
( r ij )
N
j 1
6
…
5
j=1
i
4
2
3
r cut
U i
r cut
LJ 12:6
potential
~
( r ij )
j 1 .. N neigh
r
Cutoff radius = considering interact ions only to a certain distance Basis: Force contribution negligible (slope) 13
-d /dr (eV/A)
r cut
Derivative of LJ potential ~ force
0.2
0.1
F = _ d ( r )
d r
0
P otential shift
-0.1
-0.2
2
r 0
3
4
5
r (A)
o
Image by MIT OpenCou r seWare.
14
Beyond cutoff: Changes in energy (and thus forces) small
Putting it all together…
15
MD updating scheme: Complete
(1) Updating method (integration scheme)
r i ( t 0 t ) r i ( t 0 t ) 2 r i ( t 0 ) t a i
( t 0
) t 2
...
Positions at t 0 - t
Positions at t 0
Accelerations at t 0
(2) Obtain accelerations from forces
f i ma i
a i f i / m
(3) Obtain forces from potential
(4) Crystal (initial conditions)
Positions at t 0
F
d ( r )
d r
f i F i
x
r
4
Potential
12
6
( r )
16
r
r
2.2 How to model metals: Multi-body
potentials
Pair potential : Total energy sum of all pairs of bonds
Individual bond contribution does not depend on other atoms
“ all b onds are the same ”
N N
Court e sy of the Cent er for Pol y mer St ud ies at Bost on Un iversity. Used with permis sion.
Is this a good assumption?
U total 1
( r ij )
2
i 1 , i j j 1
17
Are all bonds the same? - v alency in hydrocarbons
Ethane C 2 H 6
(stable configuration)
H
All bonds are not the same! Adding another H is not favored
18
Are all bonds the same? – metallic systems
Surface
Bulk
stronger
+ different bond EQ distance
Pair potentials: All bonds are equal!
Reality: Have environment effects; it matter that there is a free sur f ace!
Bonds depend on the environment! 19
Are all bonds the same?
Bonding energy of red atom in is six times bonding energy in
This is in contradiction with bot h experiments and more accurate quantum mechanic al calc ulations on many materials
Bonding energy of atom i
U i
( r ij )
U i ( r ij )
j 1
6
U i ( r ij )
N
j 1
Are all bonds the same?
Bonding energy of red atom in is six times bonding energy in
This is in contradiction with bot h experiments and more accurate quantum mechanic al calc ulations on many materials
For pair potentials ~ Z
Z
For m e tals ~
Z : Coordination = how many immediate neighbors an atom has
Bond s get “weaker” as more atoms are added to central atom
Bond strength depends on coordination
energy per bond
~ Z
pair
potential
Z
~
Nickel
Z
2 4 6 8 10 12 coordination
22
Da w, Foile s, Baskes, Mat. Science Reports , 1993
Transferability of pair potentials
Pair potentials have limited transferability:
Parameters determined for molecules can not be used for crystals, parameters for specific types of crystals can not be used to describe range of crystal structures
E.g. difference between FCC and BCC can not be captured using a pair potential
Metallic bonding: multi-body effects
Need to consider more details of chemical bonding to understand environmental effects
+
+ |
+ |
+ |
+ |
+ |
+ |
+ |
+ |
+ |
+ |
+ |
+ |
+ |
+ |
+ |
+ |
+ |
+ |
Electron (q=-1) Ion core (q=+N)
Delocalized valence electrons moving between nuclei generate a binding force to hold the atoms together: Electron gas model ( positive ions in a sea of electrons )
Mostly non-directional bonding, but the bond strength indeed depends on the environment of an atom, precisely the electron density imposed by other atoms
Concept: include electron density effects
, j
Each atom features a particular distribution of electron density
Concept: include electron density effects
Electron density at atom i
i , j ( r ij )
r ij
j 1 .. N neigh
r ij
x j
x i
j i
, j ( r ij )
Atomic electron density contribution of atom j to atom i
Contribution to electron density at site i due to electron density of atom j evaluated at distance r ij 26
Concept: include electron density effects
1
i 2
( r ij )
F ( i )
j 1 .. N neigh
embedding term F (how local electron density contributes to potential energy)
Electron density at atom i
, j
( r ij )
i , j ( r ij )
Atomic electron density contribution of atom j to atom i
j 1 .. N neigh
r ij
x j
x i
27
j i
x j x i
Embedded-atom method (EAM)
Atomic energy
1
new
Total energy
N
i ( r ij )
F ( i )
U total
i
2 j 1 .. N
neigh
i 1
Pair potential energy Embedding ener gy
as a function of electron density
i Electron density at atom i
based on a “pair potential”:
i
, j ( r ij )
j 1 .. N neigh
First proposed by Finnis, Sinclair, Daw, Baskes et al. (1980s) 28
Embedding term: example
0
-5
-10
0
0.01
0.02
0.03
( A o -3 )
0.04
0.05
0.06
G (eV)
Embedding energy
1 ( r ) F ( )
Image by MIT OpenCou r seWare.
Electron density
2
i ij i
j 1 .. N neigh
Pair potential energy
Embedding energy
as a function of electron dens ity 29
2
1.5
1
0.5
0
2
3
4
R (A)
o
Pair potential term: example
U (eV)
Pair contribution
( r ij )
Image by MIT OpenCou r seWare.
1 ( r ) F ( )
Distance
r ij
2
i ij i
j 1 .. N neigh
Pair potential energy
Embedding ener gy
as a function of electron density 30
Effective pair interactions
r
+ + + + + +
+ + + + + +
+ + + + + +
r
+ + + + + +
+ + + + +
+ + + + +
+
+
1
0.5
Bulk
Surface
0
-0.5
2
3
4
r (A)
o
Ef fective pair potential (eV )
Image by MIT OpenCou r seWare.
Can describe differences between bulk and surface
31
See also: Daw, Foi l e s , Ba ske s, Mat. Science Reports , 1993
Comparison with experiment
Diffusion: Activation energies
(in eV)
Courte sy of El se vie r, Inc., h t t p ://www. scien c e dir ec t . c o m . Used wi th permission.
Comparison EAM model vs. experiment
Melting temperature (in K)
Summary: EAM method
State of the art approach to model metals
Very good potentials available for Ni, Cu, Al since late 1990s, 2000s
Numerically efficient, can treat billions of particles
Not much more expensive than pair potential (approximately three times), but describes physics much better
Strongly recommended for use!
3. Brittle versus ductile materials
Brittle
Ductile
Strain
Tensile test of a wire
Necking
Brittle
Ductile
Stress
Image by MIT OpenCou r seWare. Image by MIT OpenCou r seWare.
Ductile versus brittle materials
BRITTLE
DUCTILE
Glass Polymers Ice...
Copper , Gold
Shear load
Difficult to deform,
breaks easily
Image by MIT OpenCou r seWare.
Easy to deform hard to break
43
Deformation of materials:
Nothing is perfect, and flaws or cracks matter
Failure of materials initiates at cracks
Griffith, Irwine and others: Failure initiates at defects, such as cracks, or
grain boundaries with reduced tracti on, nano-voids, other imperfections 39
SEM picture of material: nothing is perfect
40
Significance of material flaws
“global”
“local”
Fig. 1.3 in Buehler, Ma r k us J. Atom istic Modeling of Materials Failure . Spring er, 2008. © S pringer. All rig h ts r e s e rved. This
c o n t ent is e x clud ed from our C r ea t i ve C o mmons li cense. For more i n format ion, see ht tp:/ /ocw.mi t.edu/f ai ruse . 41
Stress concentrators: local stress >> global stress
Deformation of materials:
Nothing is perfect, and flaws or cracks matter
“Macro, global”
( r )
“M icro (nano), local”
r
Failure of materials initiates at cracks
Griffith, Irwine and others: Failure initiates at defects, such as cracks, or
grain boundaries with reduced tracti on, nano-voids, other imperfections 42
Cracks feature a singular stress field, with singularity at the tip of the crack
stress tensor
r
( r ) ~ 1
y
yy
xx
xy
rr
r
r
x
K I :
Stress intensity factor (function of geometry)
Image by MIT OpenCou r seWare.
43
Crack extension: brittle response
( r )
r
Large stresses lead to rupture of chemical bonds between atoms
Thus, crack extends
44
Image by MIT OpenCou r seWare.
Lattice shearing: ductile response
Instead of crack extension, induce shearing of atomic lattice
Due to large shear stresses at crack t ip
Lecture 5
Image by MIT OpenCou r seWare.
Image by MIT OpenCou r seWare.
Brittle vs. ductile material behavior
Whether a material is ductile or brittle depends on the material’s propensity to undergo shear at the crack tip , or to break atomic bonds that l e ads to crack extension
Intimately link ed to the atomic structure and atomic bon d ing
Related to temperature (activated process) ; some mechanism are eas ier accessible under higher/lower temperature
Many materials show a propensity towards brittleness at low temperature
Molecular dynamics is a quite suitable tool to study these mechanisms, that is, to find out what makes materials brittle or ductile
Historical example: significance of brittle vs. ductile fracture
Liberty ships : cargo ships built in the U.S. during World War II (during 1930s and 40s)
Eighteen U.S. shipy a rds built 2, 751 Liberties between 1941 and 1945
Early Liberty ships suffered hull and de ck cracks, and several were lost to such structural defects
Twelv e ships, including three of the 2710 Liberties built, broke in half without warning, including the SS John P. Gaines (sank 24 November 1943)
Constance Tipper of Cambridge University demonstrated that the fractures were initiated by the grade of steel used whic h suffered from embrittlement .
She discovered that the ships in t he North Atlantic were exposed to temperatures that could fall below a critical point when the mechanism of failure changed from ductile to brittle , and thus the hull could fracture relatively easily.
Liberty ships: brittle failure
48
Court e sy of the U.S. N a v y .
4. Basic deformation mechanism in brittle materials - crack extension
Introduction: brittle fracture
Materials: glass, silicon, many ceramics, rocks
At large loads, rather than accommodating a shape change, materials break
Science of fracture: model geometry
Typically consider a single crack in a crystal
Remotely applied mechanic al load
Follow ing dis c ussion focused on single cracks and their behav ior
remote load
a
remote load
51
Image by MIT OpenCou r seWare.
Brittle fracture loading conditions
Commonly cons ider a single crack in a material geometry, under three types of loading: mode I, mode II and mode III
Mode I
Mode II
Mode III
T ensile load, focus of this lectur e
Image by MIT OpenCou r seWare.
Tens ile load, focus
of this lecture 52
Brittle fracture mechanisms: fracture is a multi- scale phenomenon, from nano to macro
Imag e removed du e t o copyrigh t re str i c t ion s . S e e Fig. 6.2 in Bu eh ler, Markus J.
At omistic M o deling of Materials Fa ilure . Sprin ger, 2008.
Focus of this part
Basic fracture process : diss ipation of elastic energy
Fracture initiation , that is, at what applied load to fractures initiate
Fracture dynamics , that is, how fast can fracture propagate in material
Basic fracture process: dissipation of elastic energy
a
Undeformed Stretching=store elastic energy Release elastic energy
dissipated into breaking
chemical bonds 55
Elasticity = reversible deformation
Stress?
cross-sectional
area
A
Force per unit area
Elasticity = reversible deformation
Stress?
cross-sectional area
A
F / A
Force per unit area
Elasticity = reversible deformation
cross-sectional area
F / A
A
area under curve: stored energy
E
Young’s modulus
u / L
58
Continuum description of fracture
Fracture is a diss ipative process in which elastic energy is dissipated to break bonds (and to heat at large crack speeds)
Energy to break bonds = surface energy s (energy necessary to create new surface, dimens ions: energy/area, Nm/m 2 )
"Relaxed" element
"Strained" element
a ~
a
a ~
a
(2)
(1)
Image by MIT OpenCou r seWare.
59
Continuum description of fracture
Fracture is a diss ipative process in which elastic energy is dissipated to break bonds (and to heat at large crack speeds)
Energy to break bonds = surface energy s (energy necessary to create new surface, dimens ions: energy/area, Nm/m 2 )
"Relaxed" element
a ~
a
"Strained" element
a a ~
1
2
2 E
1 2
(2)
1 2 ~
(1)
Image by MIT OpenCou r seWare.
B out-of-plane thickness
W P ( 1 ) 2
V
E 2 E
a B
W P ( 2 ) 0 60
Continuum description of fracture
Fracture is a diss ipative process in which elastic energy is dissipated to break bonds (and to heat at large crack speeds)
Energy to break bonds = surface energy s (energy necessary to create new surface, dimens ions: energy/area, Nm/m 2 )
1
2
~
a B
"Relaxed" element
"Strained" element
a ~
a
a ~
2 E
1 2
(1)
Image by MIT OpenCou r seWare.
V
1 2
a ~ B
a
(2)
1
2
2 E
W P ( 1 ) 2 E 2 E
W P ( 2 ) W P ( 1 )
W P ( 2 ) 0 61
Continuum description of fracture
Fracture is a diss ipative process in which elastic energy is dissipated to break bonds (and to heat at large crack speeds)
Energy to break bonds = surface energy s (energy necessary to create new surface, dimens ions: energy/area, Nm/m 2 )
"Relaxed" element
a ~
a
"Strained" element
a a ~
1
2
2 E
1 2
(2)
1 2 ~
(1)
Image by MIT OpenCou r seWare.
energy to create surfaces
W P ( 1 ) 2
V
E 2 E
a B
1 2 ~ ! ~
W P ( 2 ) 0
W P ( 2 ) W P ( 1 ) 2
a B
E
2 s a B
62
Continuum description of fracture
Fracture is a diss ipative process in which elastic energy is dissipated to break bonds (and to heat at large crack speeds)
Energy to break bonds = surface energy s (energy necessary to create new surface, dimens ions: energy/area, Nm/m 2 )
"Relaxed" element
a ~
1 2
(2)
a
a
1 2 ~
"Strained" element
a ~
(1)
1
2
2 E
Image by MIT OpenCou r seWare.
energy to create surfaces
W P ( 1 ) 2
V
E 2 E
a B
1 2 ~ ! ~
63
4 s E
W P ( 2 ) 0
W P ( 2 ) W P ( 1 ) 2
a B
E
2 s a B
Continuum description of fracture
Fracture is a diss ipative process in which elastic energy is dissipated to break bonds (and to heat at large crack speeds)
Energy to break bonds = surface energy s (energy necessary to create new surface, dimens ions: energy/area, Nm/m 2 )
1 2
"Relaxed" element
"Strained" element
a ~
a
a ~
a
(2)
(1)
Image by MIT OpenCou r seWare.
2 E
4 s E
1 2 ~ ! ~
a B
2 E
2 s B a
change of elastic (potential) energy = G
energy to create 64
surfaces
Griffith condition for fracture initiation
Energy release rate G , that is, the elastic energy released per unit crack advance must be equal or lar ger than the energy necessary to create new surfaces
G :
1 2
2 E
2 y s
Provides criterion to predict fail ure initiation
Calculation of G can be complex, but straight forward for thin st rips as shown above
Approach to calculate G based on “ stress intensity factor ” ( s e e further literature, e.g. Br oberg, Anderson, Freund, Tada)
Brittle fracture mechanisms
Once nuc leated, cracks in brittle materials spread rapidly, on the order of sound speeds
Sound speeds in materials (=wave speeds):
Ray leigh-wave speed c R (speed of surface waves)
shear wave speed c s (speed of shear waves)
longitudinal wave speed c l (speed of longitudinal waves )
Maximum speeds of cracks is given by sound speeds, depending on mode of loading (mode I, II, II I )
Linear elastic continuum theory
Sound speeds in materials: overview
Wave speeds are calc ulated based on elastic properties of material
= shear modulus
E 8 / 3
3 / 8 E 67
Limiting speeds of cracks: linear elastic
continuum theory
Mother-daughter mechanism
Super- Sub-Rayleigh Rayleigh
Mode II
Intersonic
Supersonic
Mode I
C r C s
C l
Limiting speed v
Subsonic
Supersonic
Mode III
C s
C l
Limiting speed v
Linear Nonlinear
Image b y MIT OpenCo u rseW are.
• C racks can not exceed the limiting speed given by the corresponding wave speeds unless materia l behavior is nonlinear
• C racks that exceed limiting s peed would produce energy (physically impos sible - linear elastic continuum theory )
Physical reason for crack limiting speed
Phys ical (mathematical) reason for th e limiting speed is that it becomes increasingly difficult to increase the speed of the crack by adding a larger load
When the crack approaches the limiting speed, the resistance to fracture diverges to infinity (= dynamic fracture toughness )
Imag e removed du e t o co pyrigh t restric t ion s.
Pleas e s e e: Fig. 6.15 in Bu eh ler, Markus J. Atomistic Modeling of Materials Failure . Spring er, 2008.
Stress
Stiffening
Linea r theory
Softening
Linear versus nonlinear elasticity=hyperelasticity
Hyperela sticity
Strain
Image by MIT OpenCou r seWare.
Linear elasticity: Young’s modulus (stiffness) does not change with deformation
Nonlinear elasticity = hyperelasticity : Young’s m odulus (stiffn e ss) changes with deformation 70
Subsonic and supersonic fracture
Under certain conditions, materi al nonlinearities (that is, the behavior of materials under large deformation = hyperelasticity) becomes important
This can lead to different limiting speeds
than described by the model introduced above
( r ) ~ 1
r
Strain
S tress
Linea r elastic
classical theories
Deformation field near a crack
large deform ati o n nonlinear zone “si ngulari ty”
Nonlinear re al
ma ter ials
small deformation
Image by MIT OpenCou r seWare. 71
Limiting speeds of cracks
Image by MIT OpenCou r seWare.
• U nder presence of hyperelastic effects, cracks can exceed the conventional barrier given by the wave speeds
72
• T his is a “local” e ffect due to enhancement of energy flux
• Subsonic fracture due to loc a l soft ening, that is, reduction of energy flux
Stiffening
Linea r theory
Stiffening vs. softening behavior
Stress
real materials
Hyperela sticity
Strain
“linear elasticity”
1 2
Softening
2 E
73
Increased/decreased wav e speed
Image by MIT OpenCou r seWare.
Energy flux reduction/enhancement
K dominance zone
Chara cteristic energy length
Hyperelastic zone
Fra cture process zone
Classical
New
Energy Flux Related to Wave Speed: High local w a v e speed, high energy flux, cr ack can mo v e faster (and rev erse f or low local w a v e speed).
Image by MIT OpenCou r seWare.
Energy flux related to wave speed: high local wave speed, high energy flux, crack can move faster (and re verse for low local wave speed)
74
Physical basis for subsonic/supersonic fracture
Changes in energy flow at the crac k tip due to changes in local wave speed (energy flux higher in materials with higher wave speed)
Controlled by a characteristic length scale
R e print e d by permis sio n from Ma cmill an Publish e rs L t d: Nature.
S o urc e : Bueh ler, M., F. Abraham, and H. Gao. "H ypere l a s t i c i ty Governs Dynamic
Fractur e at a Critica l L e ngth S ca l e." Nature 42 6 (2003): 1 41-6. © 20 03. 75
Summary: atomistic mechanisms of brittle fracture
Brittle fracture – rapid spreading of a small initial crack
Cracks initiate based on Griffith con dition G = 2 s
Cracks spread on the order of s ound speeds (km/sec for many brittle materials)
Cracks have a maximum speed , which is giv en by characteristic sound speeds for different loading conditions)
Maximum speed can be altered if material is strongly nonlinear, leading to s upersonic or subsonic fracture
76
Supersonic fracture: mode II (shear)
77
Pleas e s e e: Bu eh ler, Markus J., Farid F. Abraham, and Hua j i a n Gao. "Hyperel ast i cit y Governs Dynamic Fractur e at a Crit ica l L e n g th Scale. "
Nature 426 (Novemb e r 13, 2003): 141-146.
Appendix: Notes for pset #1
78
Notes regarding pset #1 (question 1.)
E b
ln( D )
D D 0
exp
k B T
ln( D 0 )
ln( D )
ln( D 0 )
E b k B T
1
high temperature low temperature T
slope
~ E b
k B
Plot data extracted from RMSD graph, then fit equation
above and identify parameters 79
Mechanism and energy barrier
E b
D D 0
exp
k B T
D 0 : Rate of
attempt
80
“transition state”
E b
Court e sy of Runn i n gamok19 . Lic e n s e: CC-BY.