Mooney–Rivlin solid

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Template:Short description Script error: No such module "sidebar". 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¯1−3)+C2(I¯2−3),

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

I¯1=J−2/3I1,I1=λ12+λ22+λ32,I¯2=J−4/3I2,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¯1−3)p(I¯2−3)q+∑m=1M1Dm(J−1)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¯2−3)+C10(I¯1−3)+1D1(J−1)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(∂W∂I¯1+I¯1∂W∂I¯2)𝑩−1J4/3∂W∂I¯2𝑩⋅𝑩]+[∂W∂J−23J(I¯1∂W∂I¯1+2I¯2∂W∂I¯2)]𝑰

For a compressible Mooney–Rivlin material,

∂W∂I¯1=C1;∂W∂I¯2=C2;∂W∂J=2D1(J−1)

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

𝝈=2J[1J2/3(C1+I¯1C2)𝑩−1J4/3C2𝑩⋅𝑩]+[2D1(J−1)−23J(C1I¯1+2C2I¯2)]𝑰

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

p:=−13tr(𝝈)=−∂W∂J=−2D1(J−1).

The stress can then be expressed in the form

𝝈=−p𝑰+1J[2J2/3(C1+I¯1C2)𝑩−2J4/3C2𝑩⋅𝑩−23(C1I¯1+2C2I¯2)𝑰].

The above equation is often written using the unimodular tensor 𝑩¯=J−2/3𝑩 :

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)𝑩−2C2𝑩⋅𝑩−23(C1I1+2C2I2)𝑰.

Since det⁡J=1 the Cayley–Hamilton theorem implies

𝑩−1=𝑩⋅𝑩−I1𝑩+I2𝑰.

Hence, the Cauchy stress can be expressed as

𝝈=−p∗𝑰+2C1𝑩−2C2𝑩−1

where p∗:=23(C1I1−C2I2).

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

σ11−σ33=λ1∂W∂λ1−λ3∂W∂λ3;σ22−σ33=λ2∂W∂λ2−λ3∂W∂λ3

For an incompressible Mooney-Rivlin material,

W=C1(λ12+λ22+λ32−3)+C2(λ12λ22+λ22λ32+λ32λ12−3);λ1λ2λ3=1

Therefore,

λ1∂W∂λ1=2C1λ12+2C2λ12(λ22+λ32);λ2∂W∂λ2=2C1λ22+2C2λ22(λ12+λ32);λ3∂W∂λ3=2C1λ32+2C2λ32(λ12+λ22)

Since λ1λ2λ3=1. we can write

λ1∂W∂λ1=2C1λ12+2C2(1λ32+1λ22);λ2∂W∂λ2=2C1λ22+2C2(1λ32+1λ12)λ3∂W∂λ3=2C1λ32+2C2(1λ22+1λ12)

Then the expressions for the Cauchy stress differences become

σ11−σ33=2C1(λ12−λ32)−2C2(1λ12−1λ32);σ22−σ33=2C1(λ22−λ32)−2C2(1λ22−1λ32)

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:

σ11−σ33=2C1(λ2−1λ)−2C2(1λ2−λ)σ22−σ33=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)(λ2−1λ)

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

T11=(2C1+2C2α)(α2−α−1)

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)(α−α−2)

If we define

T11∗:=T11engα−α−2;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

σ11−σ33=σ22−σ33=2C1(λ2−1λ4)−2C2(1λ2−λ4)

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

σ11−σ33=2C1(λ2−1)−2C2(1λ2−1);σ22−σ33=2C1(1λ2−1)−2C2(λ2−1)

Therefore

σ11−σ22=2(C1+C2)(λ2−1λ2)

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+γ𝐞1⊗𝐞2

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

γ=λ−1λ;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=𝑭⋅𝑭T=[1+γ2γ0γ10001]

Therefore,

𝑩−1=[1−γ0−γ1+γ20001]

The Cauchy stress is given by

𝝈=[−p∗+2(C1−C2)+2C1γ22(C1+C2)γ02(C1+C2)γ−p∗+2(C1−C2)−2C2γ2000−p∗+2(C1−C2)]

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, Template:ISBN.
  5. ↑ Unimodularity in this context means det⁡𝑩¯=1.
  6. ↑ Template:Cite book
  7. ↑ 7.0 7.1 Ogden, R. W., 1984, Nonlinear elastic deformations, Dover
  8. ↑ Template:Cite journal

See also