4.2 Spherically
symmetric solution to quasi-static large strain elasticity problems
This section shows
how to calculate the deformation and stresses in a thick-walled spherical
shell, made from a hyperelastic material.
The results generalize the solutions in Section 4.1 by accounting for
large changes in shape and the effects of a nonlinear stress-stretch
relation. To simplify calculations, the
material is assumed to be incompressible (a reasonable assumption for most
elastomers).
4.2.1 Summary of governing equations of finite elasticity in Cartesian
components
We begin by reviewing the general equations that govern
static deformation of hyperelastic solids. A representative problem is sketched
in the figure below.

We are given the following information
1. The geometry of the solid
2. A constitutive law for the material
(i.e. the hyperelastic strain energy potential)
3. The body force density (per unit mass) (if any)
4. Prescribed boundary tractions and/or boundary displacements
To simplify the problem we will assume
· The solid is stress free in its
undeformed configuration;
· Temperature changes during
deformation are neglected
· The solid is incompressible
With these assumptions, we wish to calculate
the displacement field , the left Cauchy-Green deformation
tensor and the stress field satisfying the following equations:
· Displacementstrain relation
· Incompressibility condition
· Stressstrain relation
where is the Cauchy stress tensor, is the strain energy potential for the elastic
solid, p is the hydrostatic part of
the stress (which must be determined as part of the solution) and .
·
Equilibrium Equation
·
Traction boundary
conditions on parts of the boundary where tractions are
known.
·
Displacement
boundary conditions on parts of the
boundary where displacements are known.
4.2.2 Simplified equations for incompressible spherically
symmetric solids
A representative
spherically symmetric problem is illustrated in the figure. We consider a hollow, spherical solid, which
is subjected to spherically symmetric loading (i.e. internal body forces, as
well as tractions or displacements applied to the surface, are independent of and , and act in the
radial direction only).
The solution is most
conveniently expressed using a spherical-polar coordinate system, illustrated
in Fig. 4.11. For a finite deformation
problem, we need a way to characterize the position of material particles in
both the undeformed and deformed solid.
To do this, we let identify a material particle in the undeformed
solid. The coordinates of the same point in the deformed solid is identified by
a new set of spherical-polar co-ordinates . One way to describe the deformation would be
to specify each of the deformed coordinates in terms of the reference coordinates . For a spherically
symmetric deformation, points only move radially, so that
In finite
deformation problems vectors and tensors can be expressed as components in a basis
associated with the position of material
points in the undeformed solid, or, if more convenient, in a basis associated with material points in the
deformed solid. For spherically
symmetric deformations the two bases are identical consequently, we can write
· Position vector in the undeformed solid
· Position vector in the deformed solid
· Displacement vector
The stress, deformation gradient and deformation tensors
(written as components in ) have the form
and furthermore must satisfy .
For spherical symmetry, the governing
equations reduce to
· Strain Displacement Relations
· Incompressibility condition
· StressStrain relations
·
Equilibrium Equations
·
Boundary Conditions
Prescribed Displacements
Prescribed Tractions
4.2.3 Pressurized hollow sphere made from an
incompressible rubber
As an example,
consider a pressurized hollow rubber shell, as shown in the figure. Assume that
· Before deformation,
the sphere has inner radius A and
outer radius B
· After deformation,
the sphere has inner radius a and
outer radius b
· The solid is made from
an incompressible Mooney-Rivlin solid, with strain energy potential
·
No body forces act on the sphere
·
The inner surface r=a
is subjected to pressure
·
The outer surface r=b
is subjected to pressure
The deformed radii a,b of the inner and outer surfaces of the spherical shell are
related to the pressure by
where , , and are related by
Provided the
pressure is not too large (see below), the preceding two equations can be
solved for and given the pressure and properties of the shell
(for graphing purposes, it is better to assume a value for , calculate the
corresponding , and then determine
the pressure).
The position
r of a material particle after
deformation is related to its position R before
deformation by
The deformation tensor distribution in the
sphere is
The Cauchy stress in the sphere is
The variation of the
internal radius of the spherical shell with applied pressure is plotted in Fig.
4.13, <Fig. 4.13 near here> for (a representative value for a typical
rubber). For comparison, the linear
elastic solution (obtained by setting and in the formulas given in section 4.1.4) is
also shown.

Note that:
1. The small strain solution is accurate for
2. The relationship
between pressure and displacement is nonlinear in the large deformation regime.
3. As the internal radius of the sphere
increases, the pressure reaches a maximum, and thereafter decreases (this will
be familiar behavior to anyone who has inflated a balloon). This is
because the wall thickness of the shell decreases as the sphere expands.
The stress
distribution for various displacements in the shell is plotted in Figure 4.14, <Fig.
4.14 near here> for , and B/A=3. The radial stress remains
close to the linear elastic solution even in the large deformation regime. The hoop stress distribution is significantly
altered as the deformation increases, however.

Derivation
1. Integrate the
incompressibility condition from the inner radius of the sphere to some
arbitrary point R
2. Note that by definition, and since the point at R=A moves to r=a after deformation. This gives the relationship between the
position r of a point in the deformed
solid and its position R before
deformation
3. The components of the Cauchy-Green
tensor follow as
4. The stresses follow from the
stress-strain equation as
5. Substituting these stresses into the
equilibrium equation leads to the following differential equation for
6. After substituting
for and , and expressing R in terms of r, this equation can be integrated and simplified to see that
7. The boundary
conditions require that on (r=a,R=A),
while on (r=b,R=B),
which requires
where and . The expression that relates and to the pressure follows by subtracting the
first equation from the second. Adding
the two equations gives the expression for C.
8. Finally, the hoop stress follows by noting
that, from (4)