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.

Deformation patterns of brittle and ductile materials.

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.

xup-39

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

Imag e court e sy of quin n.anya . Li ce nse : CC - B Y .

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

Graphic showing the limiting speeds of cracks according to linear elastic continuum theory.

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

Diagram showing the classical and new conceptions of the characteristic energy length as well as the fracture process, hyperelastic, and K dominance zones. Diagram showing the classical and new conceptions of the characteristic energy length as well as the fracture process, hyperelastic, and K dominance zones. Diagram showing the classical and new conceptions of the characteristic energy length as well as the fracture process, hyperelastic, and K dominance zones. Diagram showing the classical and new conceptions of the characteristic energy length as well as the fracture process, hyperelastic, and K dominance zones. Diagram showing the classical and new conceptions of the characteristic energy length as well as the fracture process, hyperelastic, and K dominance zones.

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

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Sp r i ng 2012

F o r in fo r m a t ion about c i ting these ma te ria l s o r our Ter m s o f use , vis i t htt p :// oc w. mit.edu/ t e rms .