Physics:Mooney–Rivlin solid

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Short description: Hyperelastic material model

In continuum mechanics, a Mooney–Rivlin solid[1][2] is a hyperelastic material model where the strain energy density function W is a linear combination of two invariants of the left Cauchy–Green deformation tensor B. The model was proposed by Melvin Mooney in 1940 and expressed in terms of invariants by Ronald Rivlin in 1948.

The strain energy density function for an incompressible Mooney–Rivlin material is[3][4]

W=C1(I¯13)+C2(I¯23),

where C1 and C2 are empirically determined material constants, and I¯1 and I¯2 are the first and the second invariant of B¯=(detB)1/3B (the unimodular component of B[5]):

I¯1=J2/3I1,I1=λ12+λ22+λ32,I¯2=J4/3I2,I2=λ12λ22+λ22λ32+λ32λ12

where F is the deformation gradient and J=det(F)=λ1λ2λ3. For an incompressible material, J=1.

Derivation

The Mooney–Rivlin model is a special case of the generalized Rivlin model (also called polynomial hyperelastic model[6]) which has the form

W=p,q=0NCpq(I¯13)p(I¯23)q+m=1M1Dm(J1)2m

with C00=0 where Cpq are material constants related to the distortional response and Dm are material constants related to the volumetric response. For a compressible Mooney–Rivlin material N=1,C01=C2,C11=0,C10=C1,M=1 and we have

W=C01(I¯23)+C10(I¯13)+1D1(J1)2

If C01=0 we obtain a neo-Hookean solid, a special case of a Mooney–Rivlin solid.

For consistency with linear elasticity in the limit of small strains, it is necessary that

κ=2/D1;μ=2(C01+C10)

where κ is the bulk modulus and μ is the shear modulus.

Cauchy stress in terms of strain invariants and deformation tensors

The Cauchy stress in a compressible hyperelastic material with a stress free reference configuration is given by

σ=2J[1J2/3(WI¯1+I¯1WI¯2)B1J4/3WI¯2BB]+[WJ23J(I¯1WI¯1+2I¯2WI¯2)]I

For a compressible Mooney–Rivlin material,

WI¯1=C1;WI¯2=C2;WJ=2D1(J1)

Therefore, the Cauchy stress in a compressible Mooney–Rivlin material is given by

σ=2J[1J2/3(C1+I¯1C2)B1J4/3C2BB]+[2D1(J1)23J(C1I¯1+2C2I¯2)]I

It can be shown, after some algebra, that the pressure is given by

p:=13tr(σ)=WJ=2D1(J1).

The stress can then be expressed in the form

σ=pI+1J[2J2/3(C1+I¯1C2)B2J4/3C2BB23(C1I¯1+2C2I¯2)I].

The above equation is often written using the unimodular tensor B¯=J2/3B :

σ=pI+1J[2(C1+I¯1C2)B¯2C2B¯B¯23(C1I¯1+2C2I¯2)I].

For an incompressible Mooney–Rivlin material with J=1 there holds p=0 and B¯=B . Thus

σ=2(C1+I1C2)B2C2BB23(C1I1+2C2I2)I.

Since detJ=1 the Cayley–Hamilton theorem implies

B1=BBI1B+I2I.

Hence, the Cauchy stress can be expressed as

σ=p*I+2C1B2C2B1

where p*:=23(C1I1C2I2).

Cauchy stress in terms of principal stretches

In terms of the principal stretches, the Cauchy stress differences for an incompressible hyperelastic material are given by

σ11σ33=λ1Wλ1λ3Wλ3;σ22σ33=λ2Wλ2λ3Wλ3

For an incompressible Mooney-Rivlin material,

W=C1(λ12+λ22+λ323)+C2(λ12λ22+λ22λ32+λ32λ123);λ1λ2λ3=1

Therefore,

λ1Wλ1=2C1λ12+2C2λ12(λ22+λ32);λ2Wλ2=2C1λ22+2C2λ22(λ12+λ32);λ3Wλ3=2C1λ32+2C2λ32(λ12+λ22)

Since λ1λ2λ3=1. we can write

λ1Wλ1=2C1λ12+2C2(1λ32+1λ22);λ2Wλ2=2C1λ22+2C2(1λ32+1λ12)λ3Wλ3=2C1λ32+2C2(1λ22+1λ12)

Then the expressions for the Cauchy stress differences become

σ11σ33=2C1(λ12λ32)2C2(1λ121λ32);σ22σ33=2C1(λ22λ32)2C2(1λ221λ32)

Uniaxial extension

For the case of an incompressible Mooney–Rivlin material under uniaxial elongation, λ1=λ and λ2=λ3=1/λ. Then the true stress (Cauchy stress) differences can be calculated as:

σ11σ33=2C1(λ21λ)2C2(1λ2λ)σ22σ33=0

Simple tension

Comparison of experimental results (dots) and predictions for Hooke's law(1, blue line), neo-Hookean solid(2, red line) and Mooney–Rivlin solid models(3, green line)

In the case of simple tension, σ22=σ33=0. Then we can write

σ11=(2C1+2C2λ)(λ21λ)

In alternative notation, where the Cauchy stress is written as T and the stretch as α, we can write

T11=(2C1+2C2α)(α2α1)

and the engineering stress (force per unit reference area) for an incompressible Mooney–Rivlin material under simple tension can be calculated using T11eng=T11α2α3=T11α. Hence

T11eng=(2C1+2C2α)(αα2)

If we define

T11*:=T11engαα2;β:=1α

then

T11*=2C1+2C2β.

The slope of the T11* versus β line gives the value of C2 while the intercept with the T11* axis gives the value of C1. The Mooney–Rivlin solid model usually fits experimental data better than Neo-Hookean solid does, but requires an additional empirical constant.

Equibiaxial tension

In the case of equibiaxial tension, the principal stretches are λ1=λ2=λ. If, in addition, the material is incompressible then λ3=1/λ2. The Cauchy stress differences may therefore be expressed as

σ11σ33=σ22σ33=2C1(λ21λ4)2C2(1λ2λ4)

The equations for equibiaxial tension are equivalent to those governing uniaxial compression.

Pure shear

A pure shear deformation can be achieved by applying stretches of the form [7]

λ1=λ;λ2=1λ;λ3=1

The Cauchy stress differences for pure shear may therefore be expressed as

σ11σ33=2C1(λ21)2C2(1λ21);σ22σ33=2C1(1λ21)2C2(λ21)

Therefore

σ11σ22=2(C1+C2)(λ21λ2)

For a pure shear deformation

I1=λ12+λ22+λ32=λ2+1λ2+1;I2=1λ12+1λ22+1λ32=1λ2+λ2+1

Therefore I1=I2.

Simple shear

The deformation gradient for a simple shear deformation has the form[7]

F=1+γ𝐞1𝐞2

where 𝐞1,𝐞2 are reference orthonormal basis vectors in the plane of deformation and the shear deformation is given by

γ=λ1λ;λ1=λ;λ2=1λ;λ3=1

In matrix form, the deformation gradient and the left Cauchy-Green deformation tensor may then be expressed as

F=[1γ0010001];B=FFT=[1+γ2γ0γ10001]

Therefore,

B1=[1γ0γ1+γ20001]

The Cauchy stress is given by

σ=[p*+2(C1C2)+2C1γ22(C1+C2)γ02(C1+C2)γp*+2(C1C2)2C2γ2000p*+2(C1C2)]

For consistency with linear elasticity, clearly μ=2(C1+C2) where μ is the shear modulus.

Rubber

Elastic response of rubber-like materials are often modeled based on the Mooney–Rivlin model. The constants C1,C2 are determined by fitting the predicted stress from the above equations to the experimental data. The recommended tests are uniaxial tension, equibiaxial compression, equibiaxial tension, uniaxial compression, and for shear, planar tension and planar compression. The two parameter Mooney–Rivlin model is usually valid for strains less than 100%.

[8]

Notes and references

  1. Mooney, M., 1940, A theory of large elastic deformation, Journal of Applied Physics, 11(9), pp. 582–592.
  2. Rivlin, R. S., 1948, Large elastic deformations of isotropic materials. IV. Further developments of the general theory, Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 241(835), pp. 379–397.
  3. Boulanger, P. and Hayes, M. A., 2001, "Finite amplitude waves in Mooney–Rivlin and Hadamard materials", in Topics in Finite Elasticity, ed. M. A Hayes and G. Soccomandi, International Center for Mechanical Sciences.
  4. C. W. Macosko, 1994, Rheology: principles, measurement and applications, VCH Publishers, ISBN:1-56081-579-5.
  5. Unimodularity in this context means detB¯=1.
  6. Bower, Allan (2009). Applied Mechanics of Solids. CRC Press. ISBN 1-4398-0247-5. http://solidmechanics.org/. Retrieved 2018-04-19. 
  7. 7.0 7.1 Ogden, R. W., 1984, Nonlinear elastic deformations, Dover
  8. Hamza, Muhsin; Alwan, Hassan (2010). "Hyperelastic Constitutive Modeling of Rubber and Rubber-Like Materials under Finite Strain". Eng.& Tech. Journal 28 (13): 2560-2575. https://www.iasj.net/iasj?func=fulltext&aId=27732. 

See also