Finite strain theory
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In continuum mechanics, the finite strain theory also called large strain theory, or large deformation theory, deals with deformations in which both rotations and strains are arbitrarily large, i.e. invalidate the assumptions inherent in infinitesimal strain theory. In this case, the undeformed and deformed configurations of the continuum are significantly different and a clear distinction has to be made between them. This is commonly the case with elastomers, plastically-deforming materials and other fluids and biological soft tissue.
[edit] Displacement
A change in the configuration of a continuum body results in a displacement. The displacement of a body has two components: a rigid-body displacement and a deformation. A rigid-body displacement consist of a simultaneous translation and rotation of the body without changing its shape or size. Deformation implies the change in shape and/or size of the body from an initial or undeformed configuration
to a current or deformed configuration
(Figure 1).
If after a displacement of the continuum there is a relative displacement between particles, a deformation has occurred. On the other hand, if after displacement of the continuum the relative displacement between particles in the current configuration is zero i.e. the distance between particles remains unchanged, then there is no deformation and a rigid-body displacement is said to have occurred.
The vector joining the positions of a particle
in the undeformed configuration and deformed configuration is called the displacement vector
, in the Lagrangian description, or
, in the Eulerian description.
A displacement field is a vector field of all displacement vectors for all particles in the body, which relates the deformed configuration with the undeformed configuration. It is convenient to do the analysis of deformation or motion of a continuum body in terms of the displacement field, In general, the displacement field is expressed in terms of the material coordinates as
or in terms of the spatial coordinates as
where
are the direction cosines between the material and spatial coordinate systems with unit vectors
and
, respectively. Thus
and the relationship between
and
is then given by
Knowing that
then
It is common to superimpose the coordinate systems for the undeformed and deformed configurations, which results in
, and the direction cosines become Kronecker deltas, i.e.
Thus, we have
or in terms of the spatial coordinates as
[edit] Displacement gradient tensor
The partial differentiation of the displacement vector with respect to the material coordinates yields the material displacement gradient tensor
. Thus we have,
where
is the deformation gradient tensor.
Similarly, the partial differentiation of the displacement vector with respect to the spatial coordinates yields the spatial displacement gradient tensor
. Thus we have,
[edit] Deformation gradient tensor
Consider a particle or material point
with position vector
in the undeformed configuration (Figure 2). After a displacement of the body, the new position of the particle indicated by
in the new configuration is given by the vector position
. The coordinate systems for the undeformed and deformed configuration can be superimposed for convenience.
Consider now a material point
neighboring
, with position vector
. In the deformed configuration this particle has a new position
given by the position vector
. Assuming that the line segments
and
joining the particles
and
in both the undeformed and deformed configuration, respectively, to be very small, then we can expressed them as
and
. Thus from Figure 2 we have
where
is the relative displacement vector, which represents the relative displacement of
with respect to
in the deformed configuration.
For an infinitesimal element
, and assuming continuity on the displacement field, it is possible to use a Taylor series expansion around point
, neglecting higher-order terms, to approximate the components of the relative displacement vector for the neighboring particle
as
Thus, the previous equation
can be written as
The material deformation gradient tensor
is a second-order tensor that represents the gradient of the mapping function or functional relation
, which describes the motion of a continuum. The material deformation gradient tensor characterizes the local deformation at a material point with position vector
, i.e. deformation at neighbouring points, by transforming (linear transformation) a material line element emanating from that point from the reference configuration to the current or deformed configuration, assuming continuity in the mapping function
, i.e differentiable function of
and time
, which implies that cracks and voids do not open or close during the deformation. Thus we have,
The deformation gradient tensor
is related to both the reference and current configuration, as seen by the unit vectors
and
, therefore it is a two-point tensor.
Due to the assumption of continuity of
,
has the inverse
, where
is the spatial deformation gradient tensor. Then, by the implicit function theorem (Lubliner), the Jacobian determinant
must be nonsingular, i.e. 
[edit] Transformation of a surface and volume element
To transform quantities that are defined with respect to areas in a deformed configuration to those relative to areas in a reference configuration, and vice versa, we use the Nanson's relation, expressed as
where
is an area of a region in the deformed configuration,
is the same area in the reference configuration, and
is the outward normal to the area element in the current configuration while
is the outward normal in the reference configuration,
is the deformation gradient, and
.
-
Derivation of Nanson's relation To see how this formula is derived, we start with the oriented area elements in the reference and current configurations:
The reference and current volumes of an element are
where
.Therefore,
or,
or,
So we get
or,
[edit] Polar decomposition of the deformation gradient tensor
The deformation gradient
, like any second-order tensor, can be decomposed, using the polar decomposition theorem, into a product of two second-order tensors (Truesdell and Noll, 1965): an orthogonal tensor and a positive definite symmetric tensor, i.e.
where the tensor
is a proper orthogonal tensor, i.e.
and
, representing a rotation; the tensor
is the right stretch tensor; and
the left stretch tensor. The terms right and left means that they are to the right and left of the rotation tensor
, respectively.
and
are both positive definite, i.e.
and
, and symmetric tensors, i.e.
and
, of second order.
This decomposition implies that the deformation of a line element
in the undeformed configuration onto
in the deformed configuration, i.e.
, may be obtained either by first stretching the element by
, i.e.
, followed by a rotation
, i.e.
; or equivalently, by applying a rigid rotation
first, i.e.
, followed later by a stretching
, i.e.
(See Figure 3).
It can be shown that,
so that
and
have the same eigenvalues or principal stretches, but different eigenvectors or principal directions
and
, respectively. The principal directions are related by
This polar decomposition is unique as
is non-symmetric.
[edit] Deformation tensors
Several rotation-independent deformation tensors are used in mechanics. In solid mechanics, the most popular of these are the right and left Cauchy-Green deformation tensors. The Finger deformation tensor is mainly used in describing the motion of nonlinear fluids.[citation needed]
Since a pure rotation should not induce any stresses in a deformable body, it is often convenient to use rotation-independent measures of deformation in continuum mechanics. As a rotation followed by its inverse rotation leads to no change (
) we can exclude the rotation by multiplying
by its transpose.
[edit] The Right Cauchy-Green deformation tensor
In 1839, George Green introduced a deformation tensor known as the right Cauchy-Green deformation tensor or Green's deformation tensor, defined as:
Physically, the Cauchy-Green tensor gives us the square of local change in distances due to deformation, i.e. 
Invariants of
are often used in the expressions for strain energy density functions. The most commonly used invariants are
[edit] The Left Cauchy-Green deformation tensor
Reversing the order of multiplication in the formula for the right Green-Cauchy deformation tensor leads to the left Cauchy-Green deformation tensor which is defined as:
Invariants of
are also used in the expressions for strain energy density functions. The conventional invariants are defined as
where
is the determinant of the deformation gradient.
For nearly incompressible materials, a slightly different set of invariants is used:
[edit] The Cauchy or Finger deformation tensor
Earlier in 1828 [1], Augustin Louis Cauchy introduced a deformation tensor defined as the inverse of the left Cauchy-Green deformation tensor,
, which is often called the Cauchy deformation tensor or Finger deformation tensor, named after Josef Finger (1894).
[edit] Spectral representation
If there are three distinct principal stretches
, the spectral decompositions of
and
is given by
Furthermore,
Observe that
Therefore the uniqueness of the spectral decomposition also implies that
. The left stretch (
) is also called the spatial stretch tensor while the right stretch (
) is called the material stretch tensor.
The effect of
acting on
is to stretch the vector by
and to rotate it to the new orientation
, i.e,
In a similar vein,
-
Examples Uniaxial extension of an incompressible material This is the case where a specimen is stretched in 1-direction with a stretch ratio of
. If the volume remains constant, the contraction in the other two directions is such that
or
. Then:Simple shear



Rigid body rotation


[edit] Derivatives of stretch
Derivatives of the stretch with respect to the right Cauchy-Green deformation tensor are used to derive the stress-strain relations of many solids, particularly hyperelastic materials. These derivatives are
and follow from the observations that
[edit] Finite strain tensors
The concept of strain is used to evaluate how much a given displacement differs locally from a rigid body displacement (Ref. Lubliner). One of such strains for large deformations is the Lagrangian finite strain tensor, also called the Green-Lagrangian strain tensor or Green - St-Venant strain tensor, defined as
or as a function of the displacement gradient tensor
or
The Green-Lagrangian strain tensor is a measure of how much
differs from
. It can be shown that this tensor is a special case of a general formula for Lagrangian strain tensors (Hill 1968):
For different values of
we have:
The Eulerian-Almansi finite strain tensor, referenced to the deformed configuration, i.e. Eulerian description, is defined as
or as a function of the displacement gradients we have
-
Derivation of the Lagrangian and Eulerain finite strain tensors A measure of deformation is the difference between the squares of the differential line element
, in the undeformed configuration, and
, in the deformed configuration (Figure 2). Deformation has occurred if the difference is non zero, otherwise a rigid-body displacement has occurred. Thus we have,
In the Lagrangian description, using the material coordinates as the frame of reference, the linear transformation between the differential lines is
Then we have,
where
are the components of the right Cauchy-Green deformation tensor,
. Then, replacing this equation into the first equation we have,or
where
, are the components of a second-order tensor called the Green - St-Venant strain tensor or the Lagrangian finite strain tensor,In the Eulerian description, using the spatial coordinates as the frame of reference, the linear transformation between the differential lines is
where
are the components of the spatial deformation gradient tensor,
. Thus we havewhere the second order tensor
is called Cauchy's deformation tensor,
. Then we have,or
where
, are the components of a second-order tensor called the Eulerian-Almansi finite strain tensor,Both the Lagrangian and Eulerian finite strain tensors can be conveniently expressed in terms of the displacement gradient tensor. For the Lagrangian strain tensor, first we differentiate the displacement vector
with respect to the material coordinates
to obtain the material displacement gradient tensor, 
Replacing this equation into the expression for the Lagrangian finite strain tensor we have
or
Similarly, the Eulerian-Almansi finite strain tensor can be expressed as
[edit] Stretch ratio
The stretch ratio is a measure of the extensional or normal strain of a differential line element, which can be defined at either the undeformed configuration or the deformed configuration.
The stretch ratio for the differential element
(Figure) in the direction of the unit vector
at the material point
, in the undeformed configuration, is defined as
where
is the deformed magnitude of the differential element
.
Similarly, the stretch ratio for the differential element
(Figure), in the direction of the unit vector
at the material point
, in the deformed configuration, is defined as
The normal strain
in any direction
can be expressed as a function of the stretch ratio,
This equation implies that the normal strain is zero, i.e. no deformation, when the stretch is equal to unity. Some materials, such as elastometers can sustain stretch ratios of 3 or 4 before they fail, whereas traditional engineering materials, such as concrete or steel, fail at much lower stretch ratios, perhaps of the order of 1.001 (reference?)
[edit] Physical interpretation of the finite strain tensor
The diagonal components
of the Lagrangian finite strain tensor are related to the normal strain, e.g.
where
is the normal strain or engineering strain in the direction
.
The off-diagonal components
of the Lagrangian finite strain tensor are related to shear strain, e.g.
where
is the change in the angle between two line elements that were originally perpendicular with directions
and
, respectively.
Under certain circumstances, i.e. small displacements and small displacement rates, the components of the Lagrangian finite strain tensor may be approximated by the components of the infinitesimal strain tensor
-
Derivation of the physical interpretation of the Lagrangian and Eulerian finite strain tensors The stretch ratio for the differential element
(Figure) in the direction of the unit vector
at the material point
, in the undeformed configuration, is defined as
where
is the deformed magnitude of the differential element
.Similarly, the stretch ratio for the differential element
(Figure), in the direction of the unit vector
at the material point
, in the deformed configuration, is defined asThe square of the stretch ratio is defined as
Knowing that
we have
where
and
are unit vectors.The normal strain or engineering strain
in any direction
can be expressed as a function of the stretch ratio,Thus, the normal strain in the direction
at the material point
may be expressed in terms of the stretch ratio assolving for
we have
The shear strain, or change in angle between two line elements
and
initially perpendicular, and oriented in the principal directions
and
, respectivelly, can also be expressed as a function of the stretch ratio. From the dot product between the deformed lines
and
we havewhere
is the angle between the lines
and
in the deformed configuration. Defining
as the shear strain or reduction in the angle between two line elements that were originally perpendicular, we havethus,
then
or
[edit] See also
- Piola-Kirchhoff stress tensor, the stress tensor for finite deformations.
[edit] Notes
- ^ Jirásek,Milan; Bažant, Z. P. Inelastic analysis of structures, Waley, p 463
[edit] References
- Dill, Ellis Harold (2006). Continuum Mechanics: Elasticity, Plasticity, Viscoelasticity. Germany: CRC Press. ISBN 0849397790. http://books.google.ca/books?id=Nn4kztfbR3AC&rview=1.
- Hutter, Kolumban; Klaus Jöhnk (2004). Continuum Methods of Physical Modeling. Germany: Springer. ISBN 3540206191. http://books.google.ca/books?id=B-dxx724YD4C.
- Lubarda, Vlado A. (2001). Elastoplasticity Theory. CRC Press. ISBN 0849311381. http://books.google.ca/books?id=1P0LybL4oAgC.
- Lubliner, Jacob (2008). Plasticity Theory (Revised Edition). Dover Publications. ISBN 0486462900. http://www.ce.berkeley.edu/~coby/plas/pdf/book.pdf.
- Macosko, C. W. (1994). Rheology: principles, measurement and applications. VCH Publishers. ISBN 1-56081-579-5.
- Mase, George E. (1970). Continuum Mechanics. McGraw-Hill Professional. ISBN 0070406634. http://books.google.ca/books?id=bAdg6yxC0xUC&rview=1.
- Mase, G. Thomas; George E. Mase (1999). Continuum Mechanics for Engineers (Second ed.). CRC Press. ISBN 0-8493-1855-6. http://books.google.ca/books?id=uI1ll0A8B_UC&rview=1.
- Nemat-Nasser, Sia (2006). Plasticity: A Treatise on Finite Deformation of Heterogeneous Inelastic Materials. Cambridge: Cambridge University Press. ISBN 0521839793. http://books.google.ca/books?id=5nO78Rt0BtMC.
- Rees, David (2006), Basic Engineering Plasticity - An Introduction with Engineering and Manufacturing Applications, Butterworth-Heinemann, ISBN 0750680253, http://books.google.ca/books?id=4KWbmn_1hcYC



























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I_1^C & := \text{tr}(\mathbf{C}) = C_{II} = \lambda_1^2 + \lambda_2^2 + \lambda_3^2 \\
I_2^C & := \tfrac{1}{2}\left[\text{tr}(\mathbf{C}^2) - (\text{tr}~\mathbf{C})^2 \right]
= \tfrac{1}{2}\left[C_{IK}C_{KI} - C_{JJ}^2\right] = \lambda_1^2\lambda_2^2 + \lambda_2^2\lambda_3^2 + \lambda_3^2\lambda_1^2 \\
I_3^C & := \det(\mathbf{C}) = \lambda_1^2\lambda_2^2\lambda_3^2.
\end{align}
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![\begin{align}
I_1 & := \text{tr}(\mathbf{B}) = B_{ii} = \lambda_1^2 + \lambda_2^2 + \lambda_3^2\\
I_2 & := \tfrac{1}{2}\left[(\text{tr}~\mathbf{B})^2 - \text{tr}(\mathbf{B}^2)\right]
= \tfrac{1}{2}\left(B_{ii}^2 - B_{jk}B_{kj}\right) = \lambda_1^2\lambda_2^2 + \lambda_2^2\lambda_3^2 + \lambda_3^2\lambda_1^2 \\
I_3 & := \det\mathbf{B} = J^2 = \lambda_1^2\lambda_2^2\lambda_3^2
\end{align}
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![\begin{align}
\mathbf E &= \frac{1}{2}\left(\mathbf F^T\mathbf F-\mathbf I\right) \\
&=\frac{1}{2}\left[ \left( \mathbf u\nabla_{\mathbf X}^T+\mathbf I\right)\left( \mathbf u\nabla_{\mathbf X}+\mathbf I\right)-\mathbf I\right] \\
&=\frac{1}{2}\left( \mathbf u\nabla_{\mathbf X}^T + \mathbf u\nabla_{\mathbf X} + \mathbf u\nabla_{\mathbf X}^T \mathbf u\nabla_{\mathbf X}\right) \\
\end{align}\,\!](http://upload.wikimedia.org/math/a/6/e/a6ed833c2cadad24871a58089945858e.png)
![\begin{align}
E_{KL}&=\frac{1}{2}\left( \frac{\partial x_j}{\partial X_K}\frac{\partial x_j}{\partial X_L}-\delta_{KL}\right) \\
&=\frac{1}{2}\left[\delta_{jM}\left(\frac{\partial U_M}{\partial X_K}+\delta_{MK}\right)\delta_{jN}\left(\frac{\partial U_N}{\partial X_L}+\delta_{NL}\right)-\delta_{KL}\right] \\
&=\frac{1}{2}\left[\delta_{MN}\left(\frac{\partial U_M}{\partial X_K}+\delta_{MK}\right)\left(\frac{\partial U_N}{\partial X_L}+\delta_{NL}\right)-\delta_{KL}\right] \\
&=\frac{1}{2}\left[\left(\frac{\partial U_M}{\partial X_K}+\delta_{MK}\right)\left(\frac{\partial U_M}{\partial X_L}+\delta_{ML}\right)-\delta_{KL}\right] \\
&=\frac{1}{2}\left(\frac{\partial U_K}{\partial X_L}+\frac{\partial U_L}{\partial X_K}+\frac{\partial U_M}{\partial X_K}\frac{\partial U_M}{\partial X_L}\right)
\end{align}\,\!](http://upload.wikimedia.org/math/3/d/b/3db58870d5484e0e6b8fdca530e0ff78.png)

















