Mooney–Rivlin solid


In continuum mechanics, a Mooney–Rivlin solid is a hyperelastic material model where the strain energy density function is a linear combination of two invariants of the left Cauchy–Green deformation tensor. 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
where and are empirically determined material constants, and and are the first and the second invariant of :
where is the deformation gradient and. For an incompressible material,.

Derivation

The Mooney–Rivlin model is a special case of the generalized Rivlin model which has the form
with where are material constants related to the distortional response and are material constants related to the volumetric response. For a compressible Mooney–Rivlin material and we have
If 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
where is the bulk modulus and 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
For a compressible Mooney–Rivlin material,
Therefore, the Cauchy stress in a compressible Mooney–Rivlin material is given by
It can be shown, after some algebra, that the pressure is given by
The stress can then be expressed in the form
The above equation is often written using the unimodular tensor :
For an incompressible Mooney–Rivlin material with there holds and . Thus
Since the Cayley–Hamilton theorem implies
Hence, the Cauchy stress can be expressed as
where

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
For an incompressible Mooney-Rivlin material,
Therefore,
Since. we can write
Then the expressions for the Cauchy stress differences become

Uniaxial extension

For the case of an incompressible Mooney–Rivlin material under uniaxial elongation, and. Then the true stress differences can be calculated as:

Simple tension

In the case of simple tension,. Then we can write
In alternative notation, where the Cauchy stress is written as and the stretch as, we can write
and the engineering stress for an incompressible Mooney–Rivlin material under simple tension can be calculated using
. Hence
If we define
then
The slope of the versus line gives the value of while the intercept with the axis gives the value of. 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. If, in addition, the material is incompressible then. The Cauchy stress differences may therefore be expressed as
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
The Cauchy stress differences for pure shear may therefore be expressed as
Therefore
For a pure shear deformation
Therefore.

Simple shear

The deformation gradient for a simple shear deformation has the form
where are reference orthonormal basis vectors in the plane of deformation and the shear deformation is given by
In matrix form, the deformation gradient and the left Cauchy-Green deformation tensor may then be expressed as
Therefore,
The Cauchy stress is given by
For consistency with linear elasticity, clearly where is the shear modulus.

Rubber

Elastic response of rubber-like materials are often modeled based on the Mooney–Rivlin model. The constants 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%.