Chapter 6
Equations of Motion, Momentum and Energy
for Deformable Solids
6.1 Linear and angular momentum balance equations for
a deformable solid
Deformable
solids are governed by the same physical laws (Newton’s laws) as a system of
particles. You will hopefully recall
that, for a particle system in which particles can only interact by exerting
forces on one another (and cannot exert moments on one another):
1.
The net external
force acting on the system is equal to the time derivative of the total linear
momentum of the system
2.
The total
external moment acting on the system is equal to the rate of change of its
total angular momentum
3.
The rate of work
done by external forces is equal to the sum of the rate of change of kinetic
energy of the system and the rate of work done by internal forces.
A
deformable solid can be thought of as an infinite number of infinitesimal
particles. For a system of this kind,
the balance laws can be re-written as a set of partial differential equations,
as outlined in the sections to follow.
6.1.1 Linear
momentum balance in terms of Cauchy stress
Let denote the Cauchy stress distribution within a
deformed solid. Assume that the solid is
subjected to a body force ,
and let and denote the displacement, velocity and
acceleration of a material particle at position in
the deformed solid.
Newton’s third law of motion (F=ma) can be expressed
as
Written out in full
Note that the derivative is taken with respect to position in
the actual, deformed solid. For the special (but rather common) case of a solid
in static equilibrium in the absence of body forces
Derivation: Recall that the resultant force
acting on an arbitrary volume of material V
within a solid is
where
T(n) is the internal traction acting on the surface A with normal n that bounds V.
The linear momentum of the
volume V is
where
v is the velocity vector of a
material particle in the deformed solid. Express T in terms of and set
Apply
the divergence theorem to convert the first integral into a volume integral,
and note that one can show (see Appendix D) that
so
Since this must hold for
every volume of material within a solid, it follows that
as stated.
6.1.2 Angular momentum balance in
terms of Cauchy stress
Conservation
of angular momentum for a continuum requires that the Cauchy stress satisfy
i.e. the
stress tensor must be symmetric.
Derivation: write down the equation for balance
of angular momentum for the region V within
the deformed solid
Here, the left hand side is the resultant moment (about the
origin) exerted by tractions and body forces acting on a general region within
a solid. The right hand side is the total
angular momentum of the solid about the origin.
We can
write the same expression using index notation
Express T in terms of and re-write the first integral as a volume
integral using the divergence theorem
We may
also show (see Appendix D) that
Substitute
the last two results into the angular momentum balance equation to see that
The
integral on the right hand side of this expression is zero, because the
stresses must satisfy the linear momentum balance equation. Since this holds for any volume V, we conclude that
which is the result we
wanted.
6.1.3 Equations of motion in terms of
other stress measures
In terms
of nominal and material stress the balance of linear momentum is
Note that
the derivatives are taken with respect to position in the undeformed solid.
The
angular momentum balance equation is
To derive
these results, you can start with the integral form of the linear momentum
balance in terms of Cauchy stress
Recall (or
see Appendix D for a reminder) that area elements in the deformed and
undeformed solids are related through
In
addition, volume elements are related by . We can use these results to re-write the
integrals as integrals over a volume in the undeformed
solid as
Finally,
recall that and that to see that
Apply the
divergence theorem to the first term and rearrange
Once
again, since this must hold for any material volume, we conclude that
The linear
momentum balance equation in terms of material stress follows directly, by
substituting into this equation for in terms of
The angular momentum
balance equation can be derived simply by substituting into the momentum
balance equation in terms of Cauchy stress
6.1.4 Equations of motion and
equilibrium equations for small deformations
The general equations of motion for a deformable solid
are hard to solve, because the shape of the solid must be calculated as part of
the solution. In many engineering
applications, the deformation is small enough to be neglected. If this is the case, we can simplify the
calculations as follows
- We neglect the differences between the various
stress measures described in Section 6.1.3.
- We neglect the difference between the density of
the deformed and undeformed solid
- We satisfy the equations of motion (or
equilibrium) on the undeformed solid, instead of the deformed solid.
Accordingly,
let denote the position of a material particle in
the undeformed solid, and let denote the mass density of the undeformed
material. Assume that the solid is
subjected to a body force b per unit
mass. Newton’s third law of motion (F=ma)
can be expressed as
Written out in full
For the special (but rather common) case of a solid in static
equilibrium in the absence of body forces
Example: The
stress field
represents
the stress in an infinite, incompressible linear elastic solid that is
subjected to a point force with components acting at the origin (you can visualize a
point force as a very large body force which is concentrated in a very small
region around the origin).
(a) Verify that the stress field is in static equilibrium
This
is a tedious exercise in index notation
(b)
Consider a
spherical region of material centered at the origin. This region is subjected to (1) the body
force acting at the origin; and (2) a force exerted by the stress field on the
outer surface of the sphere. Calculate
the resultant force exerted on the outer surface of the sphere by the stress,
and show that it is equal in magnitude and opposite in direction to the body
force.
The
traction acting on the exterior surface is and a unit vector normal vector to a sphere
radius R centered at the origin is . The resultant force is thus
The
integral clearly vanishes for by symmetry.
Choosing k=j=3 without loss of
generality we can evaluate the remaining integral in spherical-polar
coordinates as
Example Let be a twice differentiable, scalar function of
position. Derive a plane stress field
from by setting
Show that this stress field satisfies the equations of
stress equilibrium with zero body force.
The
equilibrium formulas (with zero body force) are
The
third equation is satisfied trivially.
The others can be verified by substitution

Example: A prismatic concrete column of mass density supports its own weight, as shown below. (Assume that the solid is subjected to a
uniform gravitational body force of magnitude g per unit mass). Show that the stress distribution
satisfies the equations of static equilibrium
and also satisfies the boundary conditions
on all free boundaries.
The
body force (per unit mass) is . For
this case, the equilibrium equations (written out in full) are
The first and last equatinos are satisfied automatically, and
substituting for the stress into the second and evaluating the derivative shows
that that, too, is satisfied.
On the sides of the column, the normal vectors point in the directions.
Since it follows that on the sides. The stress is zero at , so the tractions on the top face are also
zero.
6.2 Work done by stresses
In this section, we derive formulas that enable you to
calculate the work done by stresses acting on a solid.
6.2.1 Work done by Cauchy stresses
Consider a solid with mass density in its initial configuration, and density in the deformed solid. Let denote the Cauchy stress distribution within
the solid. Assume that the solid is
subjected to a body force (per unit mass), and let and denote the displacement, velocity and
acceleration of a material particle at position in
the deformed solid. In addition, let
denote the
stretch rate in the solid.
The rate of work done
by Cauchy stresses per unit deformed volume is then . This energy is either dissipated as heat or
stored as internal energy in the solid, depending on the material behavior.
We
shall show that the rate of work done by internal forces acting on any
sub-volume V bounded by a surface A in the deformed solid can be
calculated from
Here,
the two terms on the left hand side represent the rate of work done by
tractions and body forces acting on the solid (work done = force
x velocity). The first term on the right-hand side can be
interpreted as the work done by Cauchy stresses; the second term is the rate of
change of kinetic energy.
Derivation: Substitute
for in terms of Cauchy stress to see that
Now, apply the divergence
theorem to the first term on the right hand side
Evaluate
the derivative and collect together the terms involving body force and stress
divergence
Recall
the equation of motion
and note
that since the stress is symmetric
to see
that
Finally,
note that
Finally, substitution leads to
as
required.
6.2.2 Rate of mechanical work in
terms of other stress measures
The rate
of work done per unit undeformed volume by Kirchhoff stress is
The rate
of work done per unit undeformed volume by Nominal stress is
The rate
of work done per unit undeformed volume by Material stress is
This shows
that nominal stress and deformation gradient are work conjugate, as are material stress and Lagrange strain.
In addition, the rate of work done on a volume of the undeformed solid can be expressed as
Derivations: The proof of the first result (and the stress power of
Kirchhoff stress) is straightforward and is left as an exercise. To show the second result, note that and to re-write the integrals over the undeformed
solid; then and apply the divergence theorem to see that
Evaluate the derivative,
recall that and use the equation of motion
to see that
Finally,
note that and re-write the second integral as a kinetic
energy term as before to obtain the required result.
The
third result follows by straightforward algebraic manipulations note that by definition
Since is symmetric it follows that
6.2.3 Rate of mechanical work for
infinitesimal deformations
For infintesimal motions all stress measures are equal; and
all strain rate measures can be approximated by the infinitesimal strain tensor
. The rate of work done by stresses per unit
volume of either deformed or undeformed solid (the difference is neglected) can
be expressed as ,
and the work done on a volume of the solid is
6.3 The principle of Virtual Work
The
principle of virtual work is an alternative way of expressing the equations of
motion and equilibrium derived in Section 6.1.
At first sight it appears to be fairly useless, but it turns out to be
an extremely useful way of deriving equilibrium equations or equations of
motion for a solid in which the deformation is approximated in some way for example, in a beam, plate or shell. In addition, the principle of virtual work is
also used as the starting point for finite element analysis for nonlinear
solids, and so is a particularly important result.

Some
definitions are needed before the principle can be stated. Suppose that a deformable solid is subjected
to loading that induces a displacement field ,
and a velocity field . The loading consists of a prescribed
displacement on part of the boundary (denoted by ), together with a traction t (which may be zero in places) applied
to the rest of the boundary (denoted by ). The
loading induces a Cauchy stress . The stress field satisfies the angular
momentum balance equation .
The
principle of virtual work is a different way of re-writing partial differential
equation for linear moment balance
in an
equivalent integral form, which is
much better suited for computer solution.
To
express the principle, we define a kinematically
admissible virtual velocity field ,
satisfying on . You can visualize this field as a small
change in the velocity of the solid, if you like, but it is really just an
arbitrary differentiable vector field.
The term `kinematically admissible’ is just a complicated way of saying
that the field is continuous, differentiable, and satisfies on - that is to say, if you perturb the velocity by
,
the boundary conditions on displacement are still satisfied.
In
addition, we define an associated virtual
velocity gradient, and virtual stretch rate as
The
principal of virtual work may be stated in two ways.
6.3.1 First version of the principle of
virtual work
The
first is not very interesting, but we will state it anyway. Suppose that the Cauchy stress satisfies:
1. The boundary condition on
2. The linear momentum balance equation
Then the virtual
work equation
Or equivalently, with index
notation
is satisfied for all virtual
velocity fields.
Proof: Observe that since the Cauchy stress is
symmetric
Next, note that
Finally,
substituting the latter identity into the virtual work equation, applying the
divergence theorem, using the linear momentum balance equation and boundary
conditions on and we obtain the required result.
6.3.2 Second version of the principle of virtual work
The converse of this
statement is much more interesting and useful.
Suppose that satisfies the virtual work equation
Or, using index notation
for all virtual velocity fields . Then the stress field must satisfy
3. The boundary condition on
4. The linear momentum balance equation
The
significance of this result is that it gives us an alternative way to solve for
a stress field that satisfies the linear momentum balance equation, which avoids having to differentiate the
stress. It is not easy to
differentiate functions accurately in the computer, but it is easy to integrate
them. The virtual work statement is the
starting point for any finite element solution involving deformable solids.
Proof: Follow
the same preliminary steps as before, i..e.
and substitute into the
virtual work equation
Apply the divergence
theorem to the first term in the first integral, and recall that on ,
we see that
Since this must hold for
all virtual velocity fields we could choose
where
is an arbitrary function that is positive
everywhere inside the solid, but is equal to zero on . For this choice, the virtual work equation
reduces to
and since the integrand is
positive everywhere the only way the equation can be satisfied is if
Given
this, we can next choose a virtual velocity field that satisfies
on . For this choice (and noting that the volume
integral is zero) the virtual work equation reduces to
Again, the integrand is
positive everywhere (it is a perfect square) and so can vanish only if
as stated.
6.3.3 The Virtual Work equation in
terms of other stress measures.
It is often convenient to
implement the virtual work equation in a finite element code using different
stress measures.
To do so, we define
1.
The actual
deformation gradient in the solid
2.
The virtual rate
of change of deformation gradient
3.
The virtual rate
of change of Lagrange strain
In addition, we define (in
the usual way)
1. Kirchhoff
stress
2.
Nominal (First
Piola-Kirchhoff) stress
3.
Material (Second Piola-Kirchhoff) stress
In terms of these
quantities, the virtual work equation may be expressed as
Note
that all the volume integrals are now taken over the undeformed solid this is convenient for computer applications,
because the shape of the undeformed solid is known. The area integral is evaluated over the deformed solid, unfortunately. It can be expressed as an equivalent integral
over the undeformed solid, but the result is messy and will be deferred until
we actually need to do it.
6.3.4 The Virtual Work equation for
infinitesimal deformations.
For infintesimal motions, the Cauchy, Nominal, and Material
stress tensors are equal; and the virtual stretch rate can be replaced by the
virtual infinitesimal strain rate
There is no need to distinguish between the volume or surface
area of the deformed and undeformed solid.
The virtual work equation can thus be expressed as
for all kinematically
admissible velocity fields.
As
a special case, this expression can be applied to a quasi-static state with .
Then, for a stress state satisfying the static equilibrium equation and boundary conditions on ,
the virtual work equation reduces to
In which are kinematically admissible displacements components
on S2)
and .
Conversely,
if the stress state satisfies for every set of kinematically admissible
virtual displacements, then the stress state satisfies the static equilibrium equation and boundary conditions on .

Example: The shell shown in the figure is subjected to a radial
body force ,
and a radial pressure acting on the surfaces at and .
The loading induces a spherically symmetric state of stress in the shell, which
can be expressed in terms of its components in a spherical-polar coordinate
system as (or if you prefer matrix notation
(a)
By considering a virtual velocity of the form ,
(i.e. all points in the sphere can only move in the radial direction, but they
can move by an arbitrary displacement) show that the stress state is in static
equilibrium if
for
all w(R).
(b) Hence,
show that the stress state must satisfy
The principle of virtual work will usually magically
give you a simplified form of the general equilibrium equation for any
simplified kind of deformation. There
is a standard process to follow, which involves two steps: (i) substitute a
virtual displacement field that has the same form as the simplified kind of
motion; and then (usually) (ii) integrate the virtual work equation by parts to
remove any derivatives of the displacement field.
We will use this method here. To evaluate the virtual work equation, we
must first calculate the virtual stretch rate .
By definition . We
can use the formula from Section 3.5.8 to calculate the gradient in spherical
polar coordinates
This is symmetric already, so in this case.
It follows that
The remaining terms in the virtual work equation are
standard dot products, and the volume integral can be re-written as an integral
with respect to the radial coordinate R,
so the virtual work principle therefore reduces to
In this form, the equation does not tell us anything
interesting. However, if we integrate
the first term by parts, we can re-write the virtual work equation as
This must vanish for all w. Since this includes any w with w=0 at R=a,R=B,
it follows that
This
must vanish even if we happen to pick
which
requires that
The
integrand is now positive or zero everywhere, so the integral can only be zero
if the integrand is zero. Therefore
Since
the integrand vanishes, we now are left with
Again,
this condition must be satisfied for all
w, which is only possible if