In continuum mechanics, the finite strain theory—also called large strain theory, or large deformation theory—deals with deformations in which strains and/or rotations are large enough to invalidate assumptions inherent in infinitesimal strain theory. In this case, the undeformed and deformed configurations of the continuum are significantly different, requiring a clear distinction between them. This is commonly the case with elastomers, plastically deforming materials and other fluids and biological soft tissue.

Displacement field

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Figure 1. Motion of a continuum body.

The displacement of a body has two components: a rigid-body displacement and a deformation.

  • A rigid-body displacement consists 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).
A change in the configuration of a continuum body can be described by a displacement field. 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. The distance between any two particles changes if and only if deformation has occurred. If displacement occurs without deformation, then it is a rigid-body displacement.

Deformation gradient tensor

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Figure 2. Deformation of a continuum body.

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. Two types of deformation gradient tensor may be defined.

Due to the assumption of continuity of  ,   has the inverse  , where   is the spatial deformation gradient tensor. Then, by the implicit function theorem,[1] the Jacobian determinant   must be nonsingular, i.e.  

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,  

Relative displacement vector

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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 express 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.

Taylor approximation

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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  

Time-derivative of the deformation gradient

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Calculations that involve the time-dependent deformation of a body often require a time derivative of the deformation gradient to be calculated. A geometrically consistent definition of such a derivative requires an excursion into differential geometry[2] but we avoid those issues in this article.

The time derivative of   is   where   is the (material) velocity. The derivative on the right hand side represents a material velocity gradient. It is common to convert that into a spatial gradient by applying the chain rule for derivatives, i.e.,   where   is the spatial velocity gradient and where   is the spatial (Eulerian) velocity at  . If the spatial velocity gradient is constant in time, the above equation can be solved exactly to give   assuming   at  . There are several methods of computing the exponential above.

Related quantities often used in continuum mechanics are the rate of deformation tensor and the spin tensor defined, respectively, as:   The rate of deformation tensor gives the rate of stretching of line elements while the spin tensor indicates the rate of rotation or vorticity of the motion.

The material time derivative of the inverse of the deformation gradient (keeping the reference configuration fixed) is often required in analyses that involve finite strains. This derivative is   The above relation can be verified by taking the material time derivative of   and noting that  .

Polar decomposition of the deformation gradient tensor

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Figure 3. Representation of the polar decomposition of the deformation gradient

The deformation gradient  , like any invertible 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   for all non-zero  , 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).

Due to the orthogonality of     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, which is unique as   is invertible with a positive determinant, is a corollary of the singular-value decomposition.

Transformation of a surface and volume element

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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 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  .

The corresponding formula for the transformation of the volume element is  

Derivation of Nanson's relation (see also [3])

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,   so,   So we get   or,   Q.E.D.

Fundamental strain tensors

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A strain tensor is defined by the IUPAC as:[4]

"A symmetric tensor that results when a deformation gradient tensor is factorized into a rotation tensor followed or preceded by a symmetric tensor".

Since a pure rotation should not induce any strains 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 the deformation gradient tensor   by its transpose.

Several rotation-independent deformation gradient tensors (or "deformation tensors", for short) are used in mechanics. In solid mechanics, the most popular of these are the right and left Cauchy–Green deformation tensors.

Cauchy strain tensor (right Cauchy–Green deformation tensor)

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In 1839, George Green introduced a deformation tensor known as the right Cauchy–Green deformation tensor or Green's deformation tensor (the IUPAC recommends that this tensor be called the Cauchy strain tensor),[4] 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   where   is the determinant of the deformation gradient   and   are stretch ratios for the unit fibers that are initially oriented along the eigenvector directions of the right (reference) stretch tensor (these are not generally aligned with the three axis of the coordinate systems).

Finger strain tensor

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The IUPAC recommends[4] that the inverse of the right Cauchy–Green deformation tensor (called the Cauchy strain tensor in that document), i. e.,  , be called the Finger strain tensor. However, that nomenclature is not universally accepted in applied mechanics.

 

Green strain tensor (left Cauchy–Green deformation tensor)

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Reversing the order of multiplication in the formula for the right Cauchy-Green deformation tensor leads to the left Cauchy–Green deformation tensor which is defined as:  

The left Cauchy–Green deformation tensor is often called the Finger deformation tensor, named after Josef Finger (1894).[5]

The IUPAC recommends that this tensor be called the Green strain tensor.[4]

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 compressible materials, a slightly different set of invariants is used:  

Piola strain tensor (Cauchy deformation tensor)

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Earlier in 1828,[6] Augustin-Louis Cauchy introduced a deformation tensor defined as the inverse of the left Cauchy–Green deformation tensor,  . This tensor has also been called the Piola strain tensor by the IUPAC[4] and the Finger tensor[7] in the rheology and fluid dynamics literature.

 

Spectral representation

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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

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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
   

Derivatives of stretch

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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  

Physical interpretation of deformation tensors

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Let   be a Cartesian coordinate system defined on the undeformed body and let   be another system defined on the deformed body. Let a curve   in the undeformed body be parametrized using  . Its image in the deformed body is  .

The undeformed length of the curve is given by   After deformation, the length becomes   Note that the right Cauchy–Green deformation tensor is defined as   Hence,   which indicates that changes in length are characterized by  .

Finite strain tensors

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The concept of strain is used to evaluate how much a given displacement differs locally from a rigid body displacement.[1][8][9] 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  .

The Eulerian finite strain tensor, or 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 Eulerian 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 have

  where 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

 

Seth–Hill family of generalized strain tensors

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B. R. Seth from the Indian Institute of Technology Kharagpur was the first to show that the Green and Almansi strain tensors are special cases of a more general strain measure.[10][11] The idea was further expanded upon by Rodney Hill in 1968.[12] The Seth–Hill family of strain measures (also called Doyle-Ericksen tensors)[13] can be expressed as

 

For different values of   we have:

  • Green-Lagrangian strain tensor  
  • Biot strain tensor  
  • Logarithmic strain, Natural strain, True strain, or Hencky strain  
  • Almansi strain  

The second-order approximation of these tensors is   where   is the infinitesimal strain tensor.

Many other different definitions of tensors   are admissible, provided that they all satisfy the conditions that:[14]

  •   vanishes for all rigid-body motions
  • the dependence of   on the displacement gradient tensor   is continuous, continuously differentiable and monotonic
  • it is also desired that   reduces to the infinitesimal strain tensor   as the norm  

An example is the set of tensors   which do not belong to the Seth–Hill class, but have the same 2nd-order approximation as the Seth–Hill measures at   for any value of  .[15]

Physical interpretation of the finite strain tensor

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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 as  

The 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 as

 

solving for   we have

 

The shear strain, or change in angle between two line elements   and   initially perpendicular, and oriented in the principal directions   and  , respectively, can also be expressed as a function of the stretch ratio. From the dot product between the deformed lines   and   we have

 

where   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 have

  thus,   then  

or

 

Compatibility conditions

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The problem of compatibility in continuum mechanics involves the determination of allowable single-valued continuous fields on bodies. These allowable conditions leave the body without unphysical gaps or overlaps after a deformation. Most such conditions apply to simply-connected bodies. Additional conditions are required for the internal boundaries of multiply connected bodies.

Compatibility of the deformation gradient

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The necessary and sufficient conditions for the existence of a compatible   field over a simply connected body are  

Compatibility of the right Cauchy–Green deformation tensor

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The necessary and sufficient conditions for the existence of a compatible   field over a simply connected body are   We can show these are the mixed components of the Riemann–Christoffel curvature tensor. Therefore, the necessary conditions for  -compatibility are that the Riemann–Christoffel curvature of the deformation is zero.

Compatibility of the left Cauchy–Green deformation tensor

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General sufficiency conditions for the left Cauchy–Green deformation tensor in three-dimensions were derived by Amit Acharya.[16] Compatibility conditions for two-dimensional   fields were found by Janet Blume.[17]

See also

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References

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  1. ^ a b Lubliner, Jacob (2008). Plasticity Theory (PDF) (Revised ed.). Dover Publications. ISBN 978-0-486-46290-5. Archived from the original (PDF) on 2010-03-31.
  2. ^ A. Yavari, J.E. Marsden, and M. Ortiz, On spatial and material covariant balance laws in elasticity, Journal of Mathematical Physics, 47, 2006, 042903; pp. 1–53.
  3. ^ Eduardo de Souza Neto; Djordje Peric; Owens, David (2008). Computational methods for plasticity : theory and applications. Chichester, West Sussex, UK: Wiley. p. 65. ISBN 978-0-470-69452-7.
  4. ^ a b c d e A. Kaye, R. F. T. Stepto, W. J. Work, J. V. Aleman (Spain), A. Ya. Malkin (1998). "Definition of terms relating to the non-ultimate mechanical properties of polymers". Pure Appl. Chem. 70 (3): 701–754. doi:10.1351/pac199870030701.{{cite journal}}: CS1 maint: multiple names: authors list (link)
  5. ^ Eduardo N. Dvorkin, Marcela B. Goldschmit, 2006 Nonlinear Continua, p. 25, Springer ISBN 3-540-24985-0.
  6. ^ Jirásek,Milan; Bažant, Z. P. (2002) Inelastic analysis of structures, Wiley, p. 463 ISBN 0-471-98716-6
  7. ^ J. N. Reddy, David K. Gartling (2000) The finite element method in heat transfer and fluid dynamics, p. 317, CRC Press ISBN 1-4200-8598-0.
  8. ^ Belytschko, Ted; Liu, Wing Kam; Moran, Brian (2000). Nonlinear Finite Elements for Continua and Structures (reprint with corrections, 2006 ed.). John Wiley & Sons Ltd. pp. 92–94. ISBN 978-0-471-98773-4.
  9. ^ Zeidi, Mahdi; Kim, Chun IL (2018). "Mechanics of an elastic solid reinforced with bidirectional fiber in finite plane elastostatics: complete analysis". Continuum Mechanics and Thermodynamics. 30 (3): 573–592. Bibcode:2018CMT....30..573Z. doi:10.1007/s00161-018-0623-0. ISSN 1432-0959. S2CID 253674037.
  10. ^ Seth, B. R. (1961), "Generalized strain measure with applications to physical problems", MRC Technical Summary Report #248, Mathematics Research Center, United States Army, University of Wisconsin: 1–18, archived from the original on August 22, 2013
  11. ^ Seth, B. R. (1962), "Generalized strain measure with applications to physical problems", IUTAM Symposium on Second Order Effects in Elasticity, Plasticity and Fluid Mechanics, Haifa, 1962.
  12. ^ Hill, R. (1968), "On constitutive inequalities for simple materials—I", Journal of the Mechanics and Physics of Solids, 16 (4): 229–242, Bibcode:1968JMPSo..16..229H, doi:10.1016/0022-5096(68)90031-8
  13. ^ T.C. Doyle and J.L. Eriksen (1956). "Non-linear elasticity." Advances in Applied Mechanics 4, 53–115.
  14. ^ Z.P. Bažant and L. Cedolin (1991). Stability of Structures. Elastic, Inelastic, Fracture and Damage Theories. Oxford Univ. Press, New York (2nd ed. Dover Publ., New York 2003; 3rd ed., World Scientific 2010).
  15. ^ Z.P. Bažant (1998). "Easy-to-compute tensors with symmetric inverse approximating Hencky finite strain and its rate." Journal of Materials of Technology ASME, 120 (April), 131–136.
  16. ^ Acharya, A. (1999). "On Compatibility Conditions for the Left Cauchy–Green Deformation Field in Three Dimensions" (PDF). Journal of Elasticity. 56 (2): 95–105. doi:10.1023/A:1007653400249. S2CID 116767781.
  17. ^ Blume, J. A. (1989). "Compatibility conditions for a left Cauchy–Green strain field". Journal of Elasticity. 21 (3): 271–308. doi:10.1007/BF00045780. S2CID 54889553.

Further reading

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