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viscoelasticity.pdf

Viscoelasticity

Rate

Strain rate

Units [time]-1

Similar definitions for every

x

v

dt

dx

x 

1 

ij 

Viscoelastic behavior

σ

t

Reversible BUT after some time

ε0 = elastic instantaneous

τ = characteristic time to reach ε(t0)/e

(e=2.718)

Time dependent (creep) modulus

at constant stress

Time dependent (relaxation)

modulus at constant strain

Moduli are functions of time

E(t), G(t), K(t)

and the corresponding

compliances

C(t), J(t), D(t)

e.g.,

Relaxation shear modulus:

G(t)=σ(t)/0

Creep compliance:

J(t)= ε(t)/s0

Notation gets messy

Basic assumptions (many times not valid ☺)

1. Linear viscoelasticity

2. Boltzman’s superposition principle

3. Correspondence principle

(elasticity-viscoelasticity)

4. Time-temperature equivalance

Linear viscoelasticity

)()()()(

)()(

)()(

2121

22

11

tttt

THEN

tt

tt

IF

ss

s

s



Boltzman’s superposition principle

Based on linear-viscoelasticity assumption

It is the basis of the beautiful math

behind viscoelasticity

transformFourierindicates

Gi

dtGGt

t

*

)(*)(*)(*)()(*

)()()0()0()( 0

s

s



 

G

Viscoelastic Characterization

Based on frequency:

1) Low: Creep or relaxation test ( < 1Hz )

2) Medium: DMA (0.1 – 100 Hz)

3) High: Wave propagation (Split Hopkinson Bar) (100 Hz and higher)

• Dynamic Mechanical Analysis (DMA) ▫ Applied strain:  = o cos(t) ▫ Response with lag: σ = σo cos(t + )

• Complex Modulus ▫ Storage and Loss components

E*() = E() + iE()

• Dissipation (Loss) Factor tan = E / E

Stress Relaxation Creep

DMA result for viscoelastic material

A practical approximation

• If the viscoelastic moduli (and compliances) change slowly with time then:

)(

1 )(

tJ tG 

• In general moduli and compliances are inverse to each other only for their

Fourier transforms

Correspondence principle

)( 3)(3

)( 33

tC I

FL

ItE

FL t 

EI

FL

3

3

Elastic solution for deflection

Approximate viscoelastic solution

for deflection

)( 3)(3

)(* 33

 

 C Ε I

FL

I

FL 

Viscoelastic solution

for deflection

Same but with

Fourier transforms

Time temperature equivalance

Typical thermal activation based

temperature dependence

Assumes a single activation – i.e. single relaxation mechanism (NOT TRUE)

More practical is to use WLF

Williams-Landel-Ferry

equation

Shift factor

Plot αΤ vs ΔΤ

and fit to get

C1 and C2

Time – temperature

superposition

For amorphous plastics

From experimental data to models

Oops … not linear 

Isochronous

stress-strain curve

FIG 21

Intermittent stresses

Viscoelastic solutions

• It is OK to use raw data for creep strain for our

problem (pipe under pressure)

• But this is NOT possible if we want a solution to a

more general problem i.e.

• If pressure varies with time (what about our case?)

• If stress varies with location (what about a bending

problem?)

• In those cases we need a full model for the moduli

and compliances

From experimental data to models

Example: Voigt model

τ = retardation time

Simple Voigt model can not model relaxation

Voigt model

Generalized Voigt

τ = retardation time

Can not model relaxation

The Relaxation Spectrum

If n is sufficiently large the summation can be approximated by the

integral over a continuous distribution of relaxation times.This is called

the “Relaxation Spectrum”. It provides a continuous function of the

relaxation time rather than a discrete set.

 

 0

d)]/t)[exp((F)t(G

Using a logarithmic scale, and a continuous spectrum H(), where

H=F and H dln()=Fd, the relaxation modulus can be related to

H():

 

  )(lnd)]/t)[exp((H)t(G

where H() is the RELAXATION SPECTRUM

Generalized Voigt-Kelvin Model

Similar arguments can be applied for a generalized Voigt-Kelvin model.







 

 





n

1i

/t

i

o

n

1i

/t

io

/t

ioi

)e1(J )t(

)t(J

)e1(J)t(

)e1(J)t(

i

i

i

Effect of soil above the pipe

D

q

3

223.0  

  

 

t

D

E

q 

q

3

03.0  

  

 

t

D

E

q 

D+d

 

gravel duncompacte

and clay,sandy compacted

clay,sandy for kN/m 20 and9, 2,

pressure soil horizontal

pressure soil vertical

091.0

15.0

2

3





 

H

V

H

V

P

P

d

DP E

EDtE

DP d

modulus elastic

lengthunit per load

Ε

q

C

When a pipe is loaded by two opposite forces F, the

points A, B, C and D are subjected to the maximum

moments which are all equal to:

The stresses due to this loading are:

1) If every point in the cross section is elastically loaded

(stress distribution is linear)

2) If every point in the cross section has plastically

yielded (all points are subjected to the yield stress)

FRM 

2 0 

lengthpipe, 12

where

2 ,

2

3

0 maxmax





L Lt

I

I

tM

t

y sss

F

F

A

B

D

R

t

2

max

0 4

Lt

M Y s

t M0

smax

t M0

sY

When F is large the pipe

deforms by yielding

at points A, B, C and D

Yielding