The governing equations for a continuum (apart from the kinematic relations
and the constitutive laws) are
- Balance of mass
- Balance of linear momentum
- Balance of angular momentum
- Balance of energy
- Entropy inequality
Two important results from calculus
There are two important results from calculus that are useful when we
use or derive these governing equations. These are
- The Gauss divergence theorem.
- The Reynolds transport theorem
These are useful enough to bear repeating at this point in the context of
second order tensors.
Reynold's transport theorem
The transport theorem shows you how to
calculate the material time derivative of an integral. It is a
generalization of the Leibniz formula.
Let
be a body in its current configuration and let
be
its surface. Also, let
.
If
is a scalar valued function of
and
then
![{\displaystyle {\cfrac {D}{Dt}}\left[\int _{\Omega }\phi (\mathbf {x} ,t)~{\text{dV}}\right]=\int _{\Omega }{\frac {\partial \phi }{\partial t}}~{\text{dV}}+\int _{\partial \Omega }(\mathbf {v} \cdot \mathbf {n} )~\phi ~{\text{dA}}=\int _{\Omega }\left[{\frac {\partial \phi }{\partial t}}+{\boldsymbol {\nabla }}\cdot \left(\phi ~\mathbf {v} \right)\right]~{\text{dV}}}](../35cd963065429119f0700f041eab886d9a9f5e00.svg)
If
is a vector valued function of
and
.
Then
![{\displaystyle {\cfrac {D}{Dt}}\left[\int _{\Omega }\mathbf {f} (\mathbf {x} ,t)~{\text{dV}}\right]=\int _{\Omega }{\frac {\partial \mathbf {f} }{\partial t}}~{\text{dV}}+\int _{\partial \Omega }(\mathbf {v} \cdot \mathbf {n} )~\mathbf {f} ~{\text{dA}}=\int _{\Omega }\left[{\frac {\partial \mathbf {f} }{\partial t}}+{\boldsymbol {\nabla }}\cdot (\mathbf {f} \otimes \mathbf {v} )\right]~{\text{dV}}}](../f8566fdb7d4f55f71dfee50514bfd3e0d34faa7b.svg)
To refresh your memory, recall that the material time derivative is given by

Conservation of mass
For the situation where a body does not gain or lose mass, the balance of mass
is written as

Sometimes, this equation is also written in conservative form as

If the material is incompressible then the density does not change with
time and we get

For Lagrangian descriptions we can show that

where
is the initial density.
Conservation of linear momentum
The balance of linear momentum is essentially Newton's second applied to
continua. Newton's second law can be written as

where the linear momentum
is given by

and the total force
is given by

where
is the density,
is the spatial velocity,
is
the body force and
is the surface traction. Therefore, the balance
of linear momentum can be written as
![{\displaystyle {\cfrac {D}{Dt}}\left[\int _{\Omega }\rho (\mathbf {x} ,t)~\mathbf {v} (\mathbf {x} ,t)~{\text{dV}}\right]=\int _{\Omega }\rho (\mathbf {x} ,t)~\mathbf {b} (\mathbf {x} ,t)~{\text{dV}}+\int _{\partial \Omega }\mathbf {t} (\mathbf {x} ,t)~{\text{dA}}}](../6ddf066b6e0f7d9219b7932e471999605921e4d0.svg)
Now using the transport theorem, we have
![{\displaystyle {\cfrac {D}{Dt}}\left[\int _{\Omega }\rho ~\mathbf {v} ~{\text{dV}}\right]=\int _{\Omega }\left[\rho ~{\cfrac {D\mathbf {v} }{Dt}}+\left({\cfrac {D\rho }{Dt}}+\rho ~{\boldsymbol {\nabla }}\cdot \mathbf {v} \right)\right]~{\text{dV}}}](../131dea0c7fba66e13faf01d86e322ff91ecab562.svg)
From the conservation of mass, the second term on the right hand side is zero
and we are left with
![{\displaystyle {\cfrac {D}{Dt}}\left[\int _{\Omega }\rho (\mathbf {x} ,t)~\mathbf {v} (\mathbf {x} ,t)~{\text{dV}}\right]=\int _{\Omega }\rho ~{\cfrac {D\mathbf {v} }{Dt}}~{\text{dV}}}](../e52f7274f30965ba21bc8a4c1d6f06d80ec28d9d.svg)
Therefore, the balance of linear momentum can be written as

Using Cauchy's theorem (
) and the divergence theorem we
can show that the balance of linear momentum can be written as

In index notation,

Conservation of angular momentum
We also have to make sure that the moments are balanced. This requirement takes
the form of the conservation of angular momentum and can be written as
![{\displaystyle {\cfrac {D}{Dt}}\left[\int _{\Omega }\mathbf {x} \times (\rho ~\mathbf {v} )~{\text{dV}}\right]=\int _{\Omega }\mathbf {x} \times (\rho ~\mathbf {b} )~{\text{dV}}+\int _{\partial \Omega }\mathbf {x} \times \mathbf {t} ~{\text{dA}}}](../4dfdee84abe9b4eac418db82f3c99fea7398da58.svg)
We can show that this equation reduces down to the requirement that the
Cauchy stress is symmetric, i.e.,

Entropy inequality
The entropy inequality is useful in determining which forms of the constitutive
equations are admissible. This inequality is also called the dissipation
inequality. In its Clausius-Duhem form, the inequality may written as

where
is the specific entropy (entropy per unit mass) and
is the
temperature.
In differential form the Clausius-Duhem inequality can be written as

In terms of the specific internal energy, the entropy inequality can be
expressed as

If we define the Helmholtz free energy (the energy that is available to do
mechanical work) as

we can also write,

Governing equations in the reference configuration
The Lagrangian form of the governing equations can be obtained using the
relations between the various measures in the deformed and reference
configurations.
Balance of mass
The Lagrangian form of the balance of mass is

Balance of angular momentum
The balance of angular momentum in Lagrangian form is

In terms of the first Piola-Kirchhoff stress

In terms of the second Piola-Kirchhoff stress

Balance of energy
In the material frame, the balance of energy takes the form

where
is the heat flux per unit reference area.
In terms of the first Piola-Kirchhoff stress tensor we have

Entropy inequality
The entropy inequality in Lagrangian form is

In terms of the first P-K stress we have

Conjugate work measures
Whatever measures we choose to use to represent stress and strain (or a rate
of strain), their product should give us a measure of the work done (or the
power spent). This measure should not depend on the chosen measures.
Therefore, the correct combination of stress and strain should be
work conjugate or power conjugate. Three commonly used power
conjugate stress and rate of strain measures are
- The Cauchy stress (
) and the rate of deformation (
).
- The nominal stress (
) and the rate of the deformation gradient (
).
- The second P-K stress (
) and the rate of the Green strain (
).
We can show that, in the absence of heat fluxes and sources,
- :{\dot {\boldsymbol {F}}}={\cfrac {1}{\rho _{0}}}~\mathbf {P} ^{T}:{\dot {\boldsymbol {F}}}={\cfrac {1}{\rho }}~{\boldsymbol {S}}:{\dot {\boldsymbol {E}}}}

Many more work/power conjugate measures can be found in the literature.