Implicitly constituted materials with fading memoryprusv/ncmm/conference/... · 2012-06-01 ·...
Transcript of Implicitly constituted materials with fading memoryprusv/ncmm/conference/... · 2012-06-01 ·...
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Implicitly constituted materials with fading
memory
Mathematical Institute, Charles University
31 March 2012
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Incompressible simple fluid
Truesdell and Noll (1965):T = −pI+ F+∞s=0(Ct (t − s))
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Differential type models
General form, Rivlin and Ericksen (1955):T = −pI+ f(A1,A2,A3, . . . )
where A1 = 2DAn =dAn−1
dt+ An−1L+ L⊤An−1
Coleman and Noll (1960): These models can be understood assuccessive approximations of the history functionalT = −pI+ F+∞
s=0(Ct (t − s))
with “fading memory”.
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Pressure dependent viscosity
T = −pI+ 2µ(p)D
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Stress dependent viscosityT = −pI+ µ(T)DSeely (1964):
µ(T) = µ∞ + (µ0 − µ∞) e−|Tδ|τ0
Blatter (1995):
µ(T) = A(
|Tδ|2 + τ20
) n−12
Matsuhisa and Bird (1965):
µ(T) = µ0
1 + α |Tδ|n−1
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Implicit constitutive relation
Rajagopal (2003, 2006); Rajagopal and Srinivasa (2008):
f (T,D) = 0
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Rate type models T = −πI+ SOldroyd (1958):S+ λ1
▽S+λ3
2(DS+ SD) + λ5
2(Tr S)D+
λ6
2(S : D) I
= −µ
(D+ λ2
▽D+ λ4D2 +λ7
2(D : D) I)
Phan Thien (1978):
YS+ λ▽S+
λξ
2(DS+ SD) = −µD
Y = e−ελ
µTr S
Notation:▽b♭ =def
db♭
dt− [∇v]b♭ − b♭ [∇v]⊤
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Materials with fading memory
Implicit algebraic relation:
f (T,D) = 0
Implicit relation between the histories:
H+∞s=0 (T(t − s),Ct (t − s)) = 0
Questions:
◮ Are rate type and differential type models (and other knownmodels) special instances or approximations of the materialwith fading memory?
◮ Is something like the celebrated retardation theoremby Coleman and Noll (1960) available for implicit typematerials with fading memory?
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Independent variables
[. . . ] the properties of a material element may dependupon the previous rheological states through which thatelement has passed, but not in any way on the states ofneighbouring elements and not on the motion of theelement as a whole in the space.
[. . . ] only those tensor quantities need to be consideredwhich have a significance for the material elementindependent of its motion as a whole in space.
Oldroyd (1950)
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Convected coordinate system
eyξ3
ξ2
ξ1
τ = t− s
τ = t
χ
X
ez
ex
x = χ(X, t)
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Plan
◮ Formulate the constitutive relation in the convectedcoordinate system, Hencky (1925), Oldroyd (1950).
◮ Formulate the constitutive relation in an implicit form,Rajagopal (2003).
◮ Expand the functional using an analogue of the retardationtheorem, Coleman and Noll (1960).
◮ Use representation theorems for isotropic linear and bilinearfunctions, Truesdell and Noll (1965).
◮ Transform the constitutive relation to a fixed-in-spacecoordinate system, Oldroyd (1950).
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Constitutive assumptions
General relation:
H+∞s=0 ( (ξ, t − s), �(ξ, t − s)) = 0,
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Constitutive assumptions
General relation:
H+∞s=0 ( (ξ, t − s), �(ξ, t − s)) = 0,
Special form of the general constitutive relation:� = −πI+ �0 = G+∞s=0 ( (ξ, t − s)− I,�(ξ, t − s))
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Constitutive assumptions
General relation:
H+∞s=0 ( (ξ, t − s), �(ξ, t − s)) = 0,
Special form of the general constitutive relation:� = −πI+ �0 = G+∞s=0 ( (ξ, t − s)− I,�(ξ, t − s))
Constitutive assumption:
‖�(ξ, t − s)‖S = O (‖ (ξ, t − s)− I‖Γ) as ‖ (ξ, t − s)− I‖Γ → 0+,
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Norm
[...] the deformations that occurred in the distant pastshould have less influence in determining the presentstress than those that occurred in the recent past.
Truesdell and Noll (1965)
‖ ‖L2h=def
(∫ +∞
s=0| (s)|2 h(s)ds) 1
2
∥∥∥[ ,�]⊤∥∥∥
L2h×L2
h
=def
(
‖ ‖2L2h+ ‖�‖2L2
h
) 12
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Taylor series for the functional� = −πI+ �0 = G+∞s=0 ( (ξ, t − s)− I,�(ξ, t − s))
G+∞s=0
([ (ξ, t − s)− I�(ξ, t − s)
])
= A+B+C+o
(∥∥∥∥
[ (ξ, t − s)− I�(ξ, t − s)
]∥∥∥∥
2
L2h×L2
h
)
A = G+∞s=0
([00])B = δG+∞
s=0
([00])[ (ξ, t − s)− I�(ξ, t − s)
]
C =[ (ξ, t − s)− I,�(ξ, t − s)
]⊤δ2G+∞
s=0
([00]) [ (ξ, t − s)− I�(ξ, t − s)
]
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Slow history
t− s
t− αs
(x, t− s)
t
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Taylor series for the metric tensor–stress tensor history
Informal expansion:
[ (ξ, t − αs)− I�(ξ, t − αs)
]
=
[ (ξ, t)− I�(ξ, t) ]− αs
[d dt(ξ, t)
d�dt(ξ, t)
]
+1
2α2s2
[d2 dt2
(ξ, t)d2�dt2
(ξ, t)
]
+ o(α2)
=
[ 0�(ξ, t)]︸ ︷︷ ︸
(0)g
−α
[d dt(ξ, t)
d�dt(ξ, t)
]
︸ ︷︷ ︸
(1)g
s +1
2α2
[d2 dt2
(ξ, t)d2�dt2
(ξ, t)
]
︸ ︷︷ ︸
(2)g
s2 + o(α2)
Rigorous result:
limα→0+
1
α2
∥∥∥∥
[ (ξ, t − αs)− I�(ξ, t − αs)
]
−
((0)
g − α(1)
gs +1
2α2(2)
gs2)∥∥∥∥L2h×L2
h
= 0
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Approximation for slow histories
Use constitutive assumption
‖�(ξ, t − s)‖S = O (‖ (ξ, t − s)− I‖Γ) as ‖ (ξ, t − s)− I‖Γ → 0+,
and substitute to the Taylor formula for the functional.First order:
G+∞s=0
([ (ξ, t − αs)− I�(ξ, t − αs)− �(ξ, t)]) = f0
((0)
g
)
+ f1
((1)
g
)
+ o (α)
Second order:
G+∞s=0
([ (ξ, t − αs)− I�(ξ, t − αs)− �(ξ, t)]) = f0
((0)
g
)
+ f1
((1)
g
)
+ f2
((2)
g
)
+ g00
((0)
g,(0)
g
)
+ g10
((1)
g,(0)
g
)
+ g01
((0)
g,(1)
g
)
+ g11
((1)
g,(1)
g
)
+ o(α2)
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Linear and bilinear tensor functions
Representation for isotropic linear functions:
h(A) = a1 (Tr A) I+ a2ARepresentation for isotropic bilinear functions:
h (A,B) = (c1 Tr ATrB+ c2 Tr (AB)) I+ c3 (Tr A)B+ c4 (TrB)A+ c5 (AB+ BA)
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Time derivatives with respect to fixed-in-space coordinate
system
Oldroyd (1950):
dbkidt
=def
(∂bki∂t
+ vmbki |m
)
− vk |mb
mi + b
kmv
m|i ,
dbkidt
=def
(∂bki∂t
+ vmbki |m
)
+ vm|kbmi + bkmv
m|i ,
dbki
dt=def
(∂bki
∂t+ v
mbki |m
)
− vk |mb
mi − bkm
vi |m,
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Time derivatives with respect to fixed-in-space coordinate
system
dbdt
=dbdt
− [∇v]b+ b [∇v] ,
db♯
dt=
db♯
dt+ [∇v]⊤ b♯ + b♯ [∇v] ,
db♭
dt=
db♭
dt− [∇v]b♭ − b♭ [∇v]⊤ ,
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Identification of the derivatives
�(ξ, t) 7→ S(x, t)d dt
(ξ, t) 7→ D(x, t)d2
dt2(ξ, t) 7→
▽D(x, t)d�dt
(ξ, t) 7→▽S(x, t)
d2�dt2
(ξ, t) 7→▽▽S(x, t)
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Approximation formulae
First order:
G+∞s=0
([ (ξ, t − αs)− I�(ξ, t − αs)− �(ξ, t)])7→ b0 (Tr S) I+ b1S+ 2b3D+ b4
(
Tr▽S) I+ b5
▽S+ o (α)
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Approximation formulae
Second order:
G+∞s=0
([ (ξ, t − αs)− I�(ξ, t − αs)− �(ξ, t)])7→[
b0 (Tr S) + b4
(
Tr▽S)+ b6
(
Tr▽▽S)+ (b15 − 2b8) Tr (D)2
+(
b10 (Tr S)2 + b11 Tr (S)2)+
(
b18
(
Tr▽S)2 + b19 Tr
(▽S)2)
+b23 Tr(D▽S)+ (b27 Tr STr
▽S+ b28 Tr(S▽S))+ b33 Tr (SD)] I
+[
b1 + b12 (TrS) + b30
(
Tr▽S)]S+[b3 + b25
(
Tr▽S)+ b34 (Tr S)]D
+ b13 (S)2 + b17 (D)2 + b36 (SD+ DS)+ b9
▽D+[
b5 + b20
(
Tr▽S)+ b29 (Tr S)] ▽S+ b21
(▽S)2
+ b26
(D▽S+▽SD)+ b31
(S▽S+▽SS)+ b7
▽▽S+ o(α2)
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Rate type models T = −πI+ SOldroyd (1958):S+ λ1
▽S+λ3
2(DS+ SD) + λ5
2(Tr S)D+
λ6
2(S : D) I
= −µ
(D+ λ2
▽D+ λ4D2 +λ7
2(D : D) I)
Phan Thien (1978):
YS+ λ▽S+
λξ
2(DS+ SD) = −µD
Y = e−ελ
µTr S
Notation:▽b♭ =def
db♭
dt− [∇v]b♭ − b♭ [∇v]⊤
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Conclusion
◮ Implicit constitutive relations provide a general concept thatcan accommodate both differential and rate type models.Generalization of the concept of simple fluid.
◮ Rate type models for viscoelastic materials can be seen asspecial instances of a general material with fading memory.(After a rigorous approximation procedure.)
◮ This is only a proof of concept—there are better ways how toderive implicit type constitutive relations that are consistentwith the laws of thermodynamics.
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