The previous page on small strains demonstrated
that their actual limitation is not small strains at all, but rather small
rotations. It was demonstrated that as the amount of rotation grows, so does
the inaccuracies in the small strain tensor.
It was also demonstrated that the stretch tensor, specifically
\({\bf U} - {\bf I}\), fulfills all the desired properties of a
strain tensor and is not limited to small rotations.
However, \({\bf U}\) is very difficult to compute
(see this page on polar decompositions),
so an alternative strain definition is needed that is easy to
calculate and is not corrupted by rigid body rotations.
The answer to this dilemma is the Green strain tensor.
Green Strain Definition
The Green strain tensor, \({\bf E}\), is based on the deformation gradient as follows.
\[
{\bf E} = {1 \over 2} \left( {\bf F}^T \cdot {\bf F} - {\bf I} \right)
\]
Recall that \({\bf F}^T \cdot {\bf F}\) completely eliminates the
rigid body rotation, \({\bf R}\), from the problem because
\[
{\bf F}^T \! \cdot {\bf F} \quad = \quad
\left( {\bf R} \cdot {\bf U} \right)^T \cdot \left( {\bf R} \cdot {\bf U} \right) \quad = \quad
{\bf U}^T \! \cdot {\bf R}^T \cdot {\bf R} \cdot {\bf U} \quad = \quad
{\bf U}^T \! \cdot {\bf U}
\]
And this leaves only the stretch tensor, \({\bf U}\), in the calculation,
confirming that the result is indeed independent of any rotations
(you will get the same computed strain regardless of the amount of rotation).
The Green strain tensor, in tensor notation, is
\[
E_{ij} = {1 \over 2} \left( F_{ki} F_{kj} - \delta_{ij} \right)
\]
and since \(F_{ij} = \delta_{ij} + u_{i,j}\), then
\[
{\bf E} = \left[ \matrix{
E_{xx} & E_{xy} & E_{xz} \\
\\
E_{xy} & E_{yy} & E_{yz} \\
\\
E_{xz} & E_{yz} & E_{zz}
} \right]
\]
The specific expressions for each
component of the Green strain tensor are listed here.
Keep in mind that \({\bf u} = (u,v,w)\).
\[
\begin{eqnarray}
E_{xx} & = & {\partial \, u \over \partial X} + {1 \over 2} \left[ \left( {\partial \, u \over \partial X} \right)^2 + \left( {\partial \, v \over \partial X} \right)^2 + \left( {\partial \, w \over \partial X} \right)^2 \right] \\
\\
\\
E_{yy} & = & {\partial \, v \over \partial Y} + {1 \over 2} \left[ \left( {\partial \, u \over \partial Y} \right)^2 + \left( {\partial \, v \over \partial Y} \right)^2 + \left( {\partial \, w \over \partial Y} \right)^2 \right] \\
\\
\\
E_{zz} & = & {\partial \, w \over \partial Z} + {1 \over 2} \left[ \left( {\partial \, u \over \partial Z} \right)^2 + \left( {\partial \, v \over \partial Z} \right)^2 + \left( {\partial \, w \over \partial Z} \right)^2 \right] \\
\\
\\
E_{xy} & = & {1 \over 2} \left( {\partial \, u \over \partial Y} + {\partial \, v \over \partial X} \right) + {1 \over 2} \left[ {\partial \, u \over \partial X} {\partial \, u \over \partial Y} + {\partial \, v \over \partial X} {\partial \, v \over \partial Y} + {\partial \, w \over \partial X} {\partial \, w \over \partial Y} \right] \\
\\
\\
E_{xz} & = & {1 \over 2} \left( {\partial \, u \over \partial Z} + {\partial \, w \over \partial X} \right) + {1 \over 2} \left[ {\partial \, u \over \partial X} {\partial \, u \over \partial Z} + {\partial \, v \over \partial X} {\partial \, v \over \partial Z} + {\partial \, w \over \partial X} {\partial \, w \over \partial Z} \right] \\
\\
\\
E_{yz} & = & {1 \over 2} \left( {\partial \, v \over \partial Z} + {\partial \, w \over \partial Y} \right) + {1 \over 2} \left[ {\partial \, u \over \partial Y} {\partial \, u \over \partial Z} + {\partial \, v \over \partial Y} {\partial \, v \over \partial Z} + {\partial \, w \over \partial Y} {\partial \, w \over \partial Z} \right] \\
\end{eqnarray}
\]
The equations are certainly too complex to provide much intuitive insight
into their properties, other than the fact that it is known that they
are independent of rotations. Perhaps the best insight is that
they can be grouped into...
\[
\text{Green Strain = Small Strain Terms + Quadratic Terms}
\]
The small strain terms are the same, possessing all the desirable properties
of engineering strain behavior. The quadratic terms are what gives
the Green strain tensor its rotation independence. But this does come
at a price, the \(\epsilon = \Delta L / L_o\) and
\(\gamma = D / T\) behaviors are affected
by the quadratic terms when the strains are large. (Not just rotations
this time, but actual strains.)
This is discussed in more detail shortly.
Shear Term Alert
Do not forget that the shear terms are one half of the engineering shear values because
they are components in a strain tensor!
U - I, Small Strain, Green Strain
Recall this example from the small strain
page. The deformation gradient, \({\bf F}\), is written below. And recall that it
corresponds to a 25° rigid body rotation
about \({\bf p} = (-0.0404,-0.3539,-0.8859)\).
\[
{\bf E} =
\left[ \matrix{
0.515 & 0.081 & 1.010 \\
0.081 & 0.123 & 0.000 \\
1.010 & 0.000 & 0.781
} \right]
\]
which is different still from both the small strain tensor,
\(\boldsymbol{\epsilon}\), and \({\bf U} - {\bf I}\).
But while \(\boldsymbol{\epsilon}\) will change with
rotation, at least \({\bf E}\) does not. This is due to the
quadratic terms in \({\bf E}\). They eliminate the rotations,
but at the expense of altering the strain components
from the desired \(\Delta L / L_o\) values when
\(\Delta L / L_o\) is large.
A Smaller Strain Example
Let's do this again for a case where the strain levels are smaller, although the
rotations are still large. In fact, we'll use the same rotation matrix as
before. Start with...
\[
{\bf F} =
\left[ \matrix{
\;\;\;1.0098 & 0.4758 & -0.0445 \\
-0.3601 & 1.1001 & \;\;\;0.1652 \\
\;\;\;0.2705 & 0.1687 & \;\;\;1.3012
} \right]
\]
The rotation matrix, \({\bf R}\), still corresponds to a 25°
rotation, and the stretch tensor, \({\bf U}\), is
\[
{\bf E} =
\left[ \matrix{
0.102 & 0.064 & 0.122 \\
0.064 & 0.221 & 0.187 \\
0.122 & 0.187 & 0.347
} \right]
\]
This time the Green strain tensor and \({\bf U} - {\bf I}\) are much
closer to each other than is \(\boldsymbol{\epsilon}\), especially the
\( \epsilon_{11} \) and \( \epsilon_{22} \) components. This is because
the strains are more moderate levels, even though the rotations are
still present. For smaller strains still,
the Green strain tensor and \({\bf U} - {\bf I}\) will become
very close to each other, regardless of the level of rotation, while
\(\boldsymbol{\epsilon}\) will not.
Uniaxial Tension
This time, let's do uniaxial tension.
Recall that \(u = \frac{X}{L_o} (L_F - L_o)\) and therefore
\[
\epsilon_x = {\partial \, u \over \partial X} = {\Delta L \over L_o} = \epsilon_{eng}
\]
In this case, the only nonzero component of the Green strain tensor is \(E_{11}\).
All partial derivatives are zero except \({\partial u \over \partial X}\). This gives
\[
E_{11} = {\partial \, u \over \partial X} + {1 \over 2} \left( {\partial \, u \over \partial X} \right)^2
\]
So for uniaxial tension, one could write
\[
E_{11} = {\Delta L \over L_o} + {1 \over 2} \left( {\Delta L \over L_o} \right)^2
\]
So again, the compromise in a Green strain tensor is the quadratic terms which, while
negligible when the strains are small, will cause \({\bf E}\) to be different from
engineering strain values when the strains are moderate or large.
Shear Strain
And finally, shear strains. In this case, \(v = \frac{X D}{T}\),
so all derivatives are zero except
\[
{\partial \, v \over \partial X} = {D \over T}
\]
So the engineering and small strain values are
\[
\gamma_{xy} = {\partial \, u \over \partial Y} + {\partial \, v \over \partial X} = {D \over T}
\]
The Green strain components are
\[
\begin{eqnarray}
E_{xx} & = & {1 \over 2} \left( {\partial \, v \over \partial X} \right)^2 = {1 \over 2} \left( {D \over T} \right)^2
\\
\\
E_{yy} & = & 0
\\
\\
E_{zz} & = & 0
\\
\\
E_{xy} & = & {1 \over 2} {\partial \, v \over \partial X} = {1 \over 2} {D \over T}
\\
\\
E_{xz} & = & 0
\\
\\
E_{yz} & = & 0
\end{eqnarray}
\]
So the Green strain tensor for this shear case is
And the shear terms are exactly the desired results. The \(E_{11}\) term is initially
a surprising nonzero result. But there is in fact an advantage to this.
The initial length of the horizontal leg of the square is simply \(T\).
But its final length in the sheared state is \(\sqrt{T^2 + D^2}\).
So \(\Delta L \over L_o\) amounts to
\[
\begin{eqnarray}
\Delta L \over L_o & = & { \sqrt{T^2 + D^2} - T \over T} \\
\\
& = & \sqrt{1 + \left( {D \over T} \right)^2} - 1
\\
\\
& = & 1 + {1 \over 2} \left( {D \over T} \right)^2 -
{1 \over 8} \left( {D \over T} \right)^4 + \;\; ... \;\; - 1 \\
\end{eqnarray}
\]
where the last line is a Taylor series expansion of the line above it.
This makes it clear that the \(E_{11}\) term is actually the second order
effect of stretching of a horizontal line segment due to shear.
This effect is not reflected by \({\bf U} - {\bf I}\).
The examples above make it clear that the Green strain tensor has several
interesting properties that are usually considered desirable: independence
from rotations, normal stretching due to shear, etc. But the compromise is
that simple uniaxial tension is not exactly equal to \(\Delta L / L_o\) at large
strains.
An Alternative Derivation
The Green strain is often presented in textbooks in a way that does not
highlight its rotational independence, but instead in a way that I
feel is more coincidental than physical.
Since \({\bf F}\) is defined as
\[
{\bf F} = {\partial \, {\bf x} \over \partial {\bf X}}
\]
This means that it can be used to relate an initial undeformed differential
length, \({\bf dX}\), to its deformed result, \({\bf dx}\), as follows.
\[
{\bf dx} = {\bf F} \cdot {\bf dX} \qquad \text{because} \qquad
{\bf dx} = {\partial \, {\bf x} \over \partial {\bf X}} \cdot {\bf dX}
\]
The above relationship is exploited in the following story leading to a
derivation of the Green strain tensor. It goes like this...
Since \({\bf dx} = {\bf F} \cdot {\bf dX}\), then
\[
{\bf dx} \cdot {\bf dx} = {\bf F} \cdot {\bf dX} \cdot {\bf F} \cdot {\bf dX}
\]
Tensor notation is needed here to figure out how to manipulate this result.
So in tensor notation, it is
\[
\begin{eqnarray}
dx_i dx_i & = & F_{ij} dX_j F_{ik} dX_k \\
\\
& = & dX_j F_{ij} F_{ik} dX_k \\
\end{eqnarray}
\]
Which can be recognized as containing a \({\bf F}^T \! \cdot {\bf F}\) term.
So this means
\[
{\bf dx} \cdot {\bf dx} - {\bf dX} \cdot {\bf dX} =
{\bf dX} \cdot ( 2 {\bf E} ) \cdot {\bf dX}
\]
This is used to justify that
\[
E = {ds^2 - dS^2 \over 2 \, dS^2 }
\]
where \(ds^2\) is the deformed length squared, and
\(dS^2\) is the undeformed length squared.
This is often presented as if it is somehow a better definition of strain
than the "boring old" \(\Delta L / L_o\) relationship.
But I consider this to only be a coincidence. It is not better at all.
It can be checked by substituting \(L_o\) for \(dS\), and
\(L_o + \Delta L\) for \(ds\). It will lead to the now familiar relationship
This is an example of computing strains at the belt edge of a tire
under high speed axisymmetric centrifugal loading
in cylindrical coordinates.
The important points to note are...
As always, the first step is to calculate the deformation gradient.
The only curve ball is that the partial derivatives
in \({\bf F}\) in cylindrical coordinates are more complex than
in rectangular coordinates. This is reviewed below.
However, once \({\bf F}\) is obtained, the remaining steps
are identical to those in rectangular coordinates, i.e.,
\({\bf E} = \frac{1}{2} ({\bf F}^T \! \cdot {\bf F} - {\bf I})\).
The deformation gradient in cylindrical coordinates is
where \(u_r, u_\theta\), and \(u_z\) are the \(R, \theta,\) and \(Z\)
components of the displacement vector.
Suppose that the displacements at the belt edge are
(I've chosen arbitrary values here, in fact.)
\[
\begin{eqnarray}
u_r & = & 0.05 R \\
\\
u_\theta & = & -0.2 (R - R_o)
\end{eqnarray}
\]
Plugging these displacements, at \(R_o\), into the deformation gradient gives
\[
{\bf F} =
\left[ \matrix {
\;\;\;1.05 & 0 & 0 \\
-0.20 & 1.05 & 0 \\
\;\;0 & 0 & 1
} \right]
\]
And the Green strain is
\[
{\bf E} =
\left[ \matrix {
\;\;\;0.071 & -0.105 & 0 \\
-0.105 & \;\;\;0.051 & 0 \\
\;\;0 & \;\;0 & 0
} \right]
\]
Cylindrical coordinates are often nonintuitive, and that seems to
apply here as well. There is a substantial amount of
circumferential strain, \(E_{\theta \theta}\), in this case even
though the displacements are not a function of \(\theta\) at all.
This circumferential strain comes from the \(u_r / R\) term in
the \(F_{\theta \theta}\) component of \({\bf F}\).
The \(u_r / R\) term captures the fact that the deformed circumference,
\(2 \pi R_{deformed}\), is different from the initial circumference,
\(2 \pi R_o\).
But here's something way more important than the above observation.
It is... that once numerical values are calculated from the partial
derivatives in \({\bf F}\), the fact that the problem is in
cylindrical coordinates goes away. From that point on, the process,
interpretation, etc, is identical to that for rectangular coordinates,
or any other system for that matter.
This is because a strain is a strain is a strain, independent of how
you got it (the same is true for stress as well). All the rules
for transformations, principal values, hydrostatic and deviatoric
components, etc, are the same in rectangular coordinates as in
cylindrical coordinates.
Almansi Strain
The Almansi strain tensor, \({\bf e}\), is yet another measure of strain.
It always gets covered in discussions of continuum mechanics,
but I've never seen it actually used anywhere.
So I won't spend much time on it.
Its derivation begins similar to the one just above for Green strain. Start with
the quantity:
\[
{\bf dx} \cdot {\bf dx} - {\bf dX} \cdot {\bf dX}
\]
But this time, substitute the following the identity:
\({\bf dX} = {\bf F}^{-1} \! \cdot {\bf dx}\)
(Note that \({\bf F}^{-1} = {\partial {\bf X} \over \partial {\bf x}}\))
\[
{\bf e} = \frac{1}{2} ({\bf I} - {\bf F}^{-T} \! \cdot {\bf F}^{-1})
\]
This can also be written as
\[
{\bf e} = \frac{1}{2} ({\bf I} - ({\bf F} \cdot {\bf F}^T)^{-1})
\]
And we already know that \({\bf F} \cdot {\bf F}^T = {\bf V} \cdot {\bf V}^T\).
The rotation matrix, \({\bf R}\) has been eliminated from the problem again.
So the Almansi strain tensor is independent of rigid body rotations just
like the Green strain tensor is.
In terms of the displacement field, it is written as
\[
e_{ij} = {1 \over 2} \left( {\partial \, u_i \over \partial x_j} + {\partial \, u_j \over \partial x_i} -
{\partial \, u_k \over \partial x_i} {\partial \, u_k \over \partial x_j} \right)
\]
The key here is that the derivatives are with respect to the deformed positions, \({\bf x}\).
Uniaxial Tension with Almansi Strain
Let's do uniaxial tension with the Almansi strain tensor.
Recall that \(u = \frac{X}{L_o} (L_F - L_o)\). However, we need \(u\) as a
function of \(x\) instead of as a function of \(X\). Replacing \(X\) with \(x - u\)
gives
\[
u = {x - u \over L_o} (L_F - L_o)
\]
and solving for \(u\) gives
\[
u = {x \over L_F} (L_F - L_o)
\]
So
\[
{\partial \, u \over \partial \, x} = {\Delta L \over L_F}
\]
The \(e_{11}\) component is
\[
e_{11} = {\partial \, u \over \partial x} -
{1 \over 2} \left( {\partial \, u \over \partial x} \right)^2
\]
and substituting \(\Delta L / L_F\) gives
\[
e_{11} = {\Delta L \over L_F} - {1 \over 2} \left( {\Delta L \over L_F} \right)^2
\]
Textbooks
Thank You
Thank you for visiting this webpage. Feel free to
email me if you have questions.
Also, please consider visiting an advertiser above.
Doing so helps to cover website hosting fees.