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Infinitesimal strain theory

In continuum mechanics, the infinitesimal strain theory is a mathematical approach to the description of the deformation of a solid body in which the displacements of the material particles are assumed to be much smaller (indeed, infinitesimally smaller) than any relevant dimension of the body; so that its geometry and the constitutive properties of the material (such as density and stiffness) at each point of space can be assumed to be unchanged by the deformation.

With this assumption, the equations of continuum mechanics are considerably simplified. This approach may also be called small deformation theory, small displacement theory, or small displacement-gradient theory. It is contrasted with the finite strain theory where the opposite assumption is made.

The infinitesimal strain theory is commonly adopted in civil and mechanical engineering for the stress analysis of structures built from relatively stiff elastic materials like concrete and steel, since a common goal in the design of such structures is to minimize their deformation under typical loads. However, this approximation demands caution in the case of thin flexible bodies, such as rods, plates, and shells which are susceptible to significant rotations, thus making the results unreliable.[1]

Infinitesimal strain tensor edit

For infinitesimal deformations of a continuum body, in which the displacement gradient tensor (2nd order tensor) is small compared to unity, i.e.  , it is possible to perform a geometric linearization of any one of the finite strain tensors used in finite strain theory, e.g. the Lagrangian finite strain tensor  , and the Eulerian finite strain tensor  . In such a linearization, the non-linear or second-order terms of the finite strain tensor are neglected. Thus we have

 
or
 
and
 
or
 

This linearization implies that the Lagrangian description and the Eulerian description are approximately the same as there is little difference in the material and spatial coordinates of a given material point in the continuum. Therefore, the material displacement gradient tensor components and the spatial displacement gradient tensor components are approximately equal. Thus we have

 
or
 
where   are the components of the infinitesimal strain tensor  , also called Cauchy's strain tensor, linear strain tensor, or small strain tensor.
 
or using different notation:
 

Furthermore, since the deformation gradient can be expressed as   where   is the second-order identity tensor, we have

 

Also, from the general expression for the Lagrangian and Eulerian finite strain tensors we have

 

Geometric derivation edit

 
Figure 1. Two-dimensional geometric deformation of an infinitesimal material element.

Consider a two-dimensional deformation of an infinitesimal rectangular material element with dimensions   by   (Figure 1), which after deformation, takes the form of a rhombus. From the geometry of Figure 1 we have

 

For very small displacement gradients, i.e.,  , we have

 

The normal strain in the  -direction of the rectangular element is defined by

 
and knowing that  , we have
 

Similarly, the normal strain in the  -direction, and  -direction, becomes

 

The engineering shear strain, or the change in angle between two originally orthogonal material lines, in this case line   and  , is defined as

 

From the geometry of Figure 1 we have

 

For small rotations, i.e.,   and   are   we have

 
and, again, for small displacement gradients, we have
 
thus
 
By interchanging   and   and   and  , it can be shown that  .

Similarly, for the  -  and  -  planes, we have

 

It can be seen that the tensorial shear strain components of the infinitesimal strain tensor can then be expressed using the engineering strain definition,  , as

 

Physical interpretation edit

From finite strain theory we have

 

For infinitesimal strains then we have

 

Dividing by   we have

 

For small deformations we assume that  , thus the second term of the left hand side becomes:  .

Then we have

 
where  , is the unit vector in the direction of  , and the left-hand-side expression is the normal strain   in the direction of  . For the particular case of   in the   direction, i.e.,  , we have
 

Similarly, for   and   we can find the normal strains   and  , respectively. Therefore, the diagonal elements of the infinitesimal strain tensor are the normal strains in the coordinate directions.

Strain transformation rules edit

If we choose an orthonormal coordinate system ( ) we can write the tensor in terms of components with respect to those base vectors as

 
In matrix form,
 
We can easily choose to use another orthonormal coordinate system ( ) instead. In that case the components of the tensor are different, say
 
The components of the strain in the two coordinate systems are related by
 
where the Einstein summation convention for repeated indices has been used and  . In matrix form
 
or
 

Strain invariants edit

Certain operations on the strain tensor give the same result without regard to which orthonormal coordinate system is used to represent the components of strain. The results of these operations are called strain invariants. The most commonly used strain invariants are

 
In terms of components
 

Principal strains edit

It can be shown that it is possible to find a coordinate system ( ) in which the components of the strain tensor are

 
The components of the strain tensor in the ( ) coordinate system are called the principal strains and the directions   are called the directions of principal strain. Since there are no shear strain components in this coordinate system, the principal strains represent the maximum and minimum stretches of an elemental volume.

If we are given the components of the strain tensor in an arbitrary orthonormal coordinate system, we can find the principal strains using an eigenvalue decomposition determined by solving the system of equations

 
This system of equations is equivalent to finding the vector   along which the strain tensor becomes a pure stretch with no shear component.

Volumetric strain edit

The volumetric strain, also called bulk strain, is the relative variation of the volume, as arising from dilation or compression; it is the first strain invariant or trace of the tensor:

 
Actually, if we consider a cube with an edge length a, it is a quasi-cube after the deformation (the variations of the angles do not change the volume) with the dimensions   and V0 = a3, thus
 
as we consider small deformations,
 
therefore the formula.

 

In case of pure shear, we can see that there is no change of the volume.

Strain deviator tensor edit

The infinitesimal strain tensor  , similarly to the Cauchy stress tensor, can be expressed as the sum of two other tensors:

  1. a mean strain tensor or volumetric strain tensor or spherical strain tensor,  , related to dilation or volume change; and
  2. a deviatoric component called the strain deviator tensor,  , related to distortion.
 
where   is the mean strain given by
 

The deviatoric strain tensor can be obtained by subtracting the mean strain tensor from the infinitesimal strain tensor:

 

Octahedral strains edit

Let ( ) be the directions of the three principal strains. An octahedral plane is one whose normal makes equal angles with the three principal directions. The engineering shear strain on an octahedral plane is called the octahedral shear strain and is given by

 
where   are the principal strains. [citation needed]

The normal strain on an octahedral plane is given by

 
[citation needed]

Equivalent strain edit

A scalar quantity called the equivalent strain, or the von Mises equivalent strain, is often used to describe the state of strain in solids. Several definitions of equivalent strain can be found in the literature. A definition that is commonly used in the literature on plasticity is

 
This quantity is work conjugate to the equivalent stress defined as
 

Compatibility equations edit

For prescribed strain components   the strain tensor equation   represents a system of six differential equations for the determination of three displacements components  , giving an over-determined system. Thus, a solution does not generally exist for an arbitrary choice of strain components. Therefore, some restrictions, named compatibility equations, are imposed upon the strain components. With the addition of the three compatibility equations the number of independent equations are reduced to three, matching the number of unknown displacement components. These constraints on the strain tensor were discovered by Saint-Venant, and are called the "Saint Venant compatibility equations".

The compatibility functions serve to assure a single-valued continuous displacement function  . If the elastic medium is visualised as a set of infinitesimal cubes in the unstrained state, after the medium is strained, an arbitrary strain tensor may not yield a situation in which the distorted cubes still fit together without overlapping.

In index notation, the compatibility equations are expressed as

 

In engineering notation,

  •  
  •  
  •  
  •  
  •  
  •  

Special cases edit

Plane strain edit

 
Plane strain state in a continuum.

In real engineering components, stress (and strain) are 3-D tensors but in prismatic structures such as a long metal billet, the length of the structure is much greater than the other two dimensions. The strains associated with length, i.e., the normal strain   and the shear strains   and   (if the length is the 3-direction) are constrained by nearby material and are small compared to the cross-sectional strains. Plane strain is then an acceptable approximation. The strain tensor for plane strain is written as:

 
in which the double underline indicates a second order tensor. This strain state is called plane strain. The corresponding stress tensor is:
 
in which the non-zero   is needed to maintain the constraint  . This stress term can be temporarily removed from the analysis to leave only the in-plane terms, effectively reducing the 3-D problem to a much simpler 2-D problem.

Antiplane strain edit

Antiplane strain is another special state of strain that can occur in a body, for instance in a region close to a screw dislocation. The strain tensor for antiplane strain is given by

 

Relation to infinitesimal rotation tensor edit

The infinitesimal strain tensor is defined as

 
Therefore the displacement gradient can be expressed as
 
where
 
The quantity   is the infinitesimal rotation tensor or infinitesimal angular displacement tensor (related to the infinitesimal rotation matrix). This tensor is skew symmetric. For infinitesimal deformations the scalar components of   satisfy the condition  . Note that the displacement gradient is small only if both the strain tensor and the rotation tensor are infinitesimal.

The axial vector edit

A skew symmetric second-order tensor has three independent scalar components. These three components are used to define an axial vector,  , as follows

 
where   is the permutation symbol. In matrix form
 
The axial vector is also called the infinitesimal rotation vector. The rotation vector is related to the displacement gradient by the relation
 
In index notation
 
If   and   then the material undergoes an approximate rigid body rotation of magnitude   around the vector  .

Relation between the strain tensor and the rotation vector edit

Given a continuous, single-valued displacement field   and the corresponding infinitesimal strain tensor  , we have (see Tensor derivative (continuum mechanics))

 
Since a change in the order of differentiation does not change the result,  . Therefore
 
Also
 
Hence
 

Relation between rotation tensor and rotation vector edit

From an important identity regarding the curl of a tensor we know that for a continuous, single-valued displacement field  ,

 
Since   we have
 

Strain tensor in non-Cartesian coordinates edit

Strain tensor in cylindrical coordinates edit

In cylindrical polar coordinates ( ), the displacement vector can be written as

 
The components of the strain tensor in a cylindrical coordinate system are given by:[2]
 

Strain tensor in spherical coordinates edit

 
Spherical coordinates (r, θ, φ) as commonly used in physics: radial distance r, polar angle θ (theta), and azimuthal angle φ (phi). The symbol ρ (rho) is often used instead of r.

In spherical coordinates ( ), the displacement vector can be written as

 
The components of the strain tensor in a spherical coordinate system are given by [2]
infinitesimal, strain, theory, this, article, includes, list, general, references, lacks, sufficient, corresponding, inline, citations, please, help, improve, this, article, introducing, more, precise, citations, august, 2023, learn, when, remove, this, messag. This article includes a list of general references but it lacks sufficient corresponding inline citations Please help to improve this article by introducing more precise citations August 2023 Learn how and when to remove this message In continuum mechanics the infinitesimal strain theory is a mathematical approach to the description of the deformation of a solid body in which the displacements of the material particles are assumed to be much smaller indeed infinitesimally smaller than any relevant dimension of the body so that its geometry and the constitutive properties of the material such as density and stiffness at each point of space can be assumed to be unchanged by the deformation With this assumption the equations of continuum mechanics are considerably simplified This approach may also be called small deformation theory small displacement theory or small displacement gradient theory It is contrasted with the finite strain theory where the opposite assumption is made The infinitesimal strain theory is commonly adopted in civil and mechanical engineering for the stress analysis of structures built from relatively stiff elastic materials like concrete and steel since a common goal in the design of such structures is to minimize their deformation under typical loads However this approximation demands caution in the case of thin flexible bodies such as rods plates and shells which are susceptible to significant rotations thus making the results unreliable 1 Contents 1 Infinitesimal strain tensor 1 1 Geometric derivation 1 2 Physical interpretation 1 3 Strain transformation rules 1 4 Strain invariants 1 5 Principal strains 1 6 Volumetric strain 1 7 Strain deviator tensor 1 8 Octahedral strains 1 9 Equivalent strain 2 Compatibility equations 3 Special cases 3 1 Plane strain 3 2 Antiplane strain 4 Relation to infinitesimal rotation tensor 4 1 The axial vector 4 2 Relation between the strain tensor and the rotation vector 4 3 Relation between rotation tensor and rotation vector 5 Strain tensor in non Cartesian coordinates 5 1 Strain tensor in cylindrical coordinates 5 2 Strain tensor in spherical coordinates 6 See also 7 References 8 External linksInfinitesimal strain tensor editFor infinitesimal deformations of a continuum body in which the displacement gradient tensor 2nd order tensor is small compared to unity i e u 1 displaystyle nabla mathbf u ll 1 nbsp it is possible to perform a geometric linearization of any one of the finite strain tensors used in finite strain theory e g the Lagrangian finite strain tensor E displaystyle mathbf E nbsp and the Eulerian finite strain tensor e displaystyle mathbf e nbsp In such a linearization the non linear or second order terms of the finite strain tensor are neglected Thus we haveE 1 2 X u X u T X u T X u 1 2 X u X u T displaystyle mathbf E frac 1 2 left nabla mathbf X mathbf u nabla mathbf X mathbf u T nabla mathbf X mathbf u T nabla mathbf X mathbf u right approx frac 1 2 left nabla mathbf X mathbf u nabla mathbf X mathbf u T right nbsp or E K L 1 2 U K X L U L X K U M X K U M X L 1 2 U K X L U L X K displaystyle E KL 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 approx frac 1 2 left frac partial U K partial X L frac partial U L partial X K right nbsp and e 1 2 x u x u T x u x u T 1 2 x u x u T displaystyle mathbf e frac 1 2 left nabla mathbf x mathbf u nabla mathbf x mathbf u T nabla mathbf x mathbf u nabla mathbf x mathbf u T right approx frac 1 2 left nabla mathbf x mathbf u nabla mathbf x mathbf u T right nbsp or e r s 1 2 u r x s u s x r u k x r u k x s 1 2 u r x s u s x r displaystyle e rs frac 1 2 left frac partial u r partial x s frac partial u s partial x r frac partial u k partial x r frac partial u k partial x s right approx frac 1 2 left frac partial u r partial x s frac partial u s partial x r right nbsp This linearization implies that the Lagrangian description and the Eulerian description are approximately the same as there is little difference in the material and spatial coordinates of a given material point in the continuum Therefore the material displacement gradient tensor components and the spatial displacement gradient tensor components are approximately equal Thus we haveE e e 1 2 u T u displaystyle mathbf E approx mathbf e approx boldsymbol varepsilon frac 1 2 left nabla mathbf u T nabla mathbf u right nbsp or E K L e r s e i j 1 2 u i j u j i displaystyle E KL approx e rs approx varepsilon ij frac 1 2 left u i j u j i right nbsp where e i j displaystyle varepsilon ij nbsp are the components of the infinitesimal strain tensor e displaystyle boldsymbol varepsilon nbsp also called Cauchy s strain tensor linear strain tensor or small strain tensor e i j 1 2 u i j u j i e 11 e 12 e 13 e 21 e 22 e 23 e 31 e 32 e 33 u 1 x 1 1 2 u 1 x 2 u 2 x 1 1 2 u 1 x 3 u 3 x 1 1 2 u 2 x 1 u 1 x 2 u 2 x 2 1 2 u 2 x 3 u 3 x 2 1 2 u 3 x 1 u 1 x 3 1 2 u 3 x 2 u 2 x 3 u 3 x 3 displaystyle begin aligned varepsilon ij amp frac 1 2 left u i j u j i right amp begin bmatrix varepsilon 11 amp varepsilon 12 amp varepsilon 13 varepsilon 21 amp varepsilon 22 amp varepsilon 23 varepsilon 31 amp varepsilon 32 amp varepsilon 33 end bmatrix amp begin bmatrix frac partial u 1 partial x 1 amp frac 1 2 left frac partial u 1 partial x 2 frac partial u 2 partial x 1 right amp frac 1 2 left frac partial u 1 partial x 3 frac partial u 3 partial x 1 right frac 1 2 left frac partial u 2 partial x 1 frac partial u 1 partial x 2 right amp frac partial u 2 partial x 2 amp frac 1 2 left frac partial u 2 partial x 3 frac partial u 3 partial x 2 right frac 1 2 left frac partial u 3 partial x 1 frac partial u 1 partial x 3 right amp frac 1 2 left frac partial u 3 partial x 2 frac partial u 2 partial x 3 right amp frac partial u 3 partial x 3 end bmatrix end aligned nbsp or using different notation e x x e x y e x z e y x e y y e y z e z x e z y e z z u x x 1 2 u x y u y x 1 2 u x z u z x 1 2 u y x u x y u y y 1 2 u y z u z y 1 2 u z x u x z 1 2 u z y u y z u z z displaystyle begin bmatrix varepsilon xx amp varepsilon xy amp varepsilon xz varepsilon yx amp varepsilon yy amp varepsilon yz varepsilon zx amp varepsilon zy amp varepsilon zz end bmatrix begin bmatrix frac partial u x partial x amp frac 1 2 left frac partial u x partial y frac partial u y partial x right amp frac 1 2 left frac partial u x partial z frac partial u z partial x right frac 1 2 left frac partial u y partial x frac partial u x partial y right amp frac partial u y partial y amp frac 1 2 left frac partial u y partial z frac partial u z partial y right frac 1 2 left frac partial u z partial x frac partial u x partial z right amp frac 1 2 left frac partial u z partial y frac partial u y partial z right amp frac partial u z partial z end bmatrix nbsp Furthermore since the deformation gradient can be expressed as F u I displaystyle boldsymbol F boldsymbol nabla mathbf u boldsymbol I nbsp where I displaystyle boldsymbol I nbsp is the second order identity tensor we havee 1 2 F T F I displaystyle boldsymbol varepsilon frac 1 2 left boldsymbol F T boldsymbol F right boldsymbol I nbsp Also from the general expression for the Lagrangian and Eulerian finite strain tensors we haveE m 1 2 m U 2 m I 1 2 m F T F m I 1 2 m u u T I m I e e m 1 2 m V 2 m I 1 2 m F F T m I e displaystyle begin aligned mathbf E m amp frac 1 2m mathbf U 2m boldsymbol I frac 1 2m boldsymbol F T boldsymbol F m boldsymbol I approx frac 1 2m boldsymbol nabla mathbf u boldsymbol nabla mathbf u T boldsymbol I m boldsymbol I approx boldsymbol varepsilon mathbf e m amp frac 1 2m mathbf V 2m boldsymbol I frac 1 2m boldsymbol F boldsymbol F T m boldsymbol I approx boldsymbol varepsilon end aligned nbsp Geometric derivation edit nbsp Figure 1 Two dimensional geometric deformation of an infinitesimal material element Consider a two dimensional deformation of an infinitesimal rectangular material element with dimensions d x displaystyle dx nbsp by d y displaystyle dy nbsp Figure 1 which after deformation takes the form of a rhombus From the geometry of Figure 1 we havea b d x u x x d x 2 u y x d x 2 d x 1 2 u x x u x x 2 u y x 2 displaystyle begin aligned overline ab amp sqrt left dx frac partial u x partial x dx right 2 left frac partial u y partial x dx right 2 amp dx sqrt 1 2 frac partial u x partial x left frac partial u x partial x right 2 left frac partial u y partial x right 2 end aligned nbsp For very small displacement gradients i e u 1 displaystyle nabla mathbf u ll 1 nbsp we havea b d x u x x d x displaystyle overline ab approx dx frac partial u x partial x dx nbsp The normal strain in the x displaystyle x nbsp direction of the rectangular element is defined bye x a b A B A B displaystyle varepsilon x frac overline ab overline AB overline AB nbsp and knowing that A B d x displaystyle overline AB dx nbsp we have e x u x x displaystyle varepsilon x frac partial u x partial x nbsp Similarly the normal strain in the y displaystyle y nbsp direction and z displaystyle z nbsp direction becomese y u y y e z u z z displaystyle varepsilon y frac partial u y partial y quad qquad varepsilon z frac partial u z partial z nbsp The engineering shear strain or the change in angle between two originally orthogonal material lines in this case line A C displaystyle overline AC nbsp and A B displaystyle overline AB nbsp is defined asg x y a b displaystyle gamma xy alpha beta nbsp From the geometry of Figure 1 we havetan a u y x d x d x u x x d x u y x 1 u x x tan b u x y d y d y u y y d y u x y 1 u y y displaystyle tan alpha frac dfrac partial u y partial x dx dx dfrac partial u x partial x dx frac dfrac partial u y partial x 1 dfrac partial u x partial x quad qquad tan beta frac dfrac partial u x partial y dy dy dfrac partial u y partial y dy frac dfrac partial u x partial y 1 dfrac partial u y partial y nbsp For small rotations i e a displaystyle alpha nbsp and b displaystyle beta nbsp are 1 displaystyle ll 1 nbsp we havetan a a tan b b displaystyle tan alpha approx alpha quad qquad tan beta approx beta nbsp and again for small displacement gradients we have a u y x b u x y displaystyle alpha frac partial u y partial x quad qquad beta frac partial u x partial y nbsp thus g x y a b u y x u x y displaystyle gamma xy alpha beta frac partial u y partial x frac partial u x partial y nbsp By interchanging x displaystyle x nbsp and y displaystyle y nbsp and u x displaystyle u x nbsp and u y displaystyle u y nbsp it can be shown that g x y g y x displaystyle gamma xy gamma yx nbsp Similarly for the y displaystyle y nbsp z displaystyle z nbsp and x displaystyle x nbsp z displaystyle z nbsp planes we haveg y z g z y u y z u z y g z x g x z u z x u x z displaystyle gamma yz gamma zy frac partial u y partial z frac partial u z partial y quad qquad gamma zx gamma xz frac partial u z partial x frac partial u x partial z nbsp It can be seen that the tensorial shear strain components of the infinitesimal strain tensor can then be expressed using the engineering strain definition g displaystyle gamma nbsp as e x x e x y e x z e y x e y y e y z e z x e z y e z z e x x g x y 2 g x z 2 g y x 2 e y y g y z 2 g z x 2 g z y 2 e z z displaystyle begin bmatrix varepsilon xx amp varepsilon xy amp varepsilon xz varepsilon yx amp varepsilon yy amp varepsilon yz varepsilon zx amp varepsilon zy amp varepsilon zz end bmatrix begin bmatrix varepsilon xx amp gamma xy 2 amp gamma xz 2 gamma yx 2 amp varepsilon yy amp gamma yz 2 gamma zx 2 amp gamma zy 2 amp varepsilon zz end bmatrix nbsp Physical interpretation edit From finite strain theory we haved x 2 d X 2 d X 2 E d X or d x 2 d X 2 2 E K L d X K d X L displaystyle d mathbf x 2 d mathbf X 2 d mathbf X cdot 2 mathbf E cdot d mathbf X quad text or quad dx 2 dX 2 2E KL dX K dX L nbsp For infinitesimal strains then we haved x 2 d X 2 d X 2 e d X or d x 2 d X 2 2 e K L d X K d X L displaystyle d mathbf x 2 d mathbf X 2 d mathbf X cdot 2 mathbf boldsymbol varepsilon cdot d mathbf X quad text or quad dx 2 dX 2 2 varepsilon KL dX K dX L nbsp Dividing by d X 2 displaystyle dX 2 nbsp we haved x d X d X d x d X d X 2 e i j d X i d X d X j d X displaystyle frac dx dX dX frac dx dX dX 2 varepsilon ij frac dX i dX frac dX j dX nbsp For small deformations we assume that d x d X displaystyle dx approx dX nbsp thus the second term of the left hand side becomes d x d X d X 2 displaystyle frac dx dX dX approx 2 nbsp Then we haved x d X d X e i j N i N j N e N displaystyle frac dx dX dX varepsilon ij N i N j mathbf N cdot boldsymbol varepsilon cdot mathbf N nbsp where N i d X i d X displaystyle N i frac dX i dX nbsp is the unit vector in the direction of d X displaystyle d mathbf X nbsp and the left hand side expression is the normal strain e N displaystyle e mathbf N nbsp in the direction of N displaystyle mathbf N nbsp For the particular case of N displaystyle mathbf N nbsp in the X 1 displaystyle X 1 nbsp direction i e N I 1 displaystyle mathbf N mathbf I 1 nbsp we have e I 1 I 1 e I 1 e 11 displaystyle e mathbf I 1 mathbf I 1 cdot boldsymbol varepsilon cdot mathbf I 1 varepsilon 11 nbsp Similarly for N I 2 displaystyle mathbf N mathbf I 2 nbsp and N I 3 displaystyle mathbf N mathbf I 3 nbsp we can find the normal strains e 22 displaystyle varepsilon 22 nbsp and e 33 displaystyle varepsilon 33 nbsp respectively Therefore the diagonal elements of the infinitesimal strain tensor are the normal strains in the coordinate directions Strain transformation rules edit If we choose an orthonormal coordinate system e 1 e 2 e 3 displaystyle mathbf e 1 mathbf e 2 mathbf e 3 nbsp we can write the tensor in terms of components with respect to those base vectors ase i 1 3 j 1 3 e i j e i e j displaystyle boldsymbol varepsilon sum i 1 3 sum j 1 3 varepsilon ij mathbf e i otimes mathbf e j nbsp In matrix form e e 11 e 12 e 13 e 12 e 22 e 23 e 13 e 23 e 33 displaystyle underline underline boldsymbol varepsilon begin bmatrix varepsilon 11 amp varepsilon 12 amp varepsilon 13 varepsilon 12 amp varepsilon 22 amp varepsilon 23 varepsilon 13 amp varepsilon 23 amp varepsilon 33 end bmatrix nbsp We can easily choose to use another orthonormal coordinate system e 1 e 2 e 3 displaystyle hat mathbf e 1 hat mathbf e 2 hat mathbf e 3 nbsp instead In that case the components of the tensor are different say e i 1 3 j 1 3 e i j e i e j e e 11 e 12 e 13 e 12 e 22 e 23 e 13 e 23 e 33 displaystyle boldsymbol varepsilon sum i 1 3 sum j 1 3 hat varepsilon ij hat mathbf e i otimes hat mathbf e j quad implies quad underline underline hat boldsymbol varepsilon begin bmatrix hat varepsilon 11 amp hat varepsilon 12 amp hat varepsilon 13 hat varepsilon 12 amp hat varepsilon 22 amp hat varepsilon 23 hat varepsilon 13 amp hat varepsilon 23 amp hat varepsilon 33 end bmatrix nbsp The components of the strain in the two coordinate systems are related by e i j ℓ i p ℓ j q e p q displaystyle hat varepsilon ij ell ip ell jq varepsilon pq nbsp where the Einstein summation convention for repeated indices has been used and ℓ i j e i e j displaystyle ell ij hat mathbf e i cdot mathbf e j nbsp In matrix form e L e L T displaystyle underline underline hat boldsymbol varepsilon underline underline mathbf L underline underline boldsymbol varepsilon underline underline mathbf L T nbsp or e 11 e 12 e 13 e 21 e 22 e 23 e 31 e 32 e 33 ℓ 11 ℓ 12 ℓ 13 ℓ 21 ℓ 22 ℓ 23 ℓ 31 ℓ 32 ℓ 33 e 11 e 12 e 13 e 21 e 22 e 23 e 31 e 32 e 33 ℓ 11 ℓ 12 ℓ 13 ℓ 21 ℓ 22 ℓ 23 ℓ 31 ℓ 32 ℓ 33 T displaystyle begin bmatrix hat varepsilon 11 amp hat varepsilon 12 amp hat varepsilon 13 hat varepsilon 21 amp hat varepsilon 22 amp hat varepsilon 23 hat varepsilon 31 amp hat varepsilon 32 amp hat varepsilon 33 end bmatrix begin bmatrix ell 11 amp ell 12 amp ell 13 ell 21 amp ell 22 amp ell 23 ell 31 amp ell 32 amp ell 33 end bmatrix begin bmatrix varepsilon 11 amp varepsilon 12 amp varepsilon 13 varepsilon 21 amp varepsilon 22 amp varepsilon 23 varepsilon 31 amp varepsilon 32 amp varepsilon 33 end bmatrix begin bmatrix ell 11 amp ell 12 amp ell 13 ell 21 amp ell 22 amp ell 23 ell 31 amp ell 32 amp ell 33 end bmatrix T nbsp Strain invariants edit Certain operations on the strain tensor give the same result without regard to which orthonormal coordinate system is used to represent the components of strain The results of these operations are called strain invariants The most commonly used strain invariants areI 1 t r e I 2 1 2 t r e 2 t r e 2 I 3 det e displaystyle begin aligned I 1 amp mathrm tr boldsymbol varepsilon I 2 amp tfrac 1 2 mathrm tr boldsymbol varepsilon 2 mathrm tr boldsymbol varepsilon 2 I 3 amp det boldsymbol varepsilon end aligned nbsp In terms of components I 1 e 11 e 22 e 33 I 2 e 11 e 22 e 22 e 33 e 33 e 11 e 12 2 e 23 2 e 31 2 I 3 e 11 e 22 e 33 e 23 2 e 12 e 21 e 33 e 23 e 31 e 13 e 21 e 32 e 22 e 31 displaystyle begin aligned I 1 amp varepsilon 11 varepsilon 22 varepsilon 33 I 2 amp varepsilon 11 varepsilon 22 varepsilon 22 varepsilon 33 varepsilon 33 varepsilon 11 varepsilon 12 2 varepsilon 23 2 varepsilon 31 2 I 3 amp varepsilon 11 varepsilon 22 varepsilon 33 varepsilon 23 2 varepsilon 12 varepsilon 21 varepsilon 33 varepsilon 23 varepsilon 31 varepsilon 13 varepsilon 21 varepsilon 32 varepsilon 22 varepsilon 31 end aligned nbsp Principal strains edit It can be shown that it is possible to find a coordinate system n 1 n 2 n 3 displaystyle mathbf n 1 mathbf n 2 mathbf n 3 nbsp in which the components of the strain tensor aree e 1 0 0 0 e 2 0 0 0 e 3 e e 1 n 1 n 1 e 2 n 2 n 2 e 3 n 3 n 3 displaystyle underline underline boldsymbol varepsilon begin bmatrix varepsilon 1 amp 0 amp 0 0 amp varepsilon 2 amp 0 0 amp 0 amp varepsilon 3 end bmatrix quad implies quad boldsymbol varepsilon varepsilon 1 mathbf n 1 otimes mathbf n 1 varepsilon 2 mathbf n 2 otimes mathbf n 2 varepsilon 3 mathbf n 3 otimes mathbf n 3 nbsp The components of the strain tensor in the n 1 n 2 n 3 displaystyle mathbf n 1 mathbf n 2 mathbf n 3 nbsp coordinate system are called the principal strains and the directions n i displaystyle mathbf n i nbsp are called the directions of principal strain Since there are no shear strain components in this coordinate system the principal strains represent the maximum and minimum stretches of an elemental volume If we are given the components of the strain tensor in an arbitrary orthonormal coordinate system we can find the principal strains using an eigenvalue decomposition determined by solving the system of equations e e i I n i 0 displaystyle underline underline boldsymbol varepsilon varepsilon i underline underline mathbf I mathbf n i underline mathbf 0 nbsp This system of equations is equivalent to finding the vector n i displaystyle mathbf n i nbsp along which the strain tensor becomes a pure stretch with no shear component Volumetric strain edit The volumetric strain also called bulk strain is the relative variation of the volume as arising from dilation or compression it is the first strain invariant or trace of the tensor d D V V 0 I 1 e 11 e 22 e 33 displaystyle delta frac Delta V V 0 I 1 varepsilon 11 varepsilon 22 varepsilon 33 nbsp Actually if we consider a cube with an edge length a it is a quasi cube after the deformation the variations of the angles do not change the volume with the dimensions a 1 e 11 a 1 e 22 a 1 e 33 displaystyle a cdot 1 varepsilon 11 times a cdot 1 varepsilon 22 times a cdot 1 varepsilon 33 nbsp and V0 a3 thus D V V 0 1 e 11 e 22 e 33 e 11 e 22 e 11 e 33 e 22 e 33 e 11 e 22 e 33 a 3 a 3 a 3 displaystyle frac Delta V V 0 frac left 1 varepsilon 11 varepsilon 22 varepsilon 33 varepsilon 11 cdot varepsilon 22 varepsilon 11 cdot varepsilon 33 varepsilon 22 cdot varepsilon 33 varepsilon 11 cdot varepsilon 22 cdot varepsilon 33 right cdot a 3 a 3 a 3 nbsp as we consider small deformations 1 e i i e i i e j j e 11 e 22 e 33 displaystyle 1 gg varepsilon ii gg varepsilon ii cdot varepsilon jj gg varepsilon 11 cdot varepsilon 22 cdot varepsilon 33 nbsp therefore the formula nbsp In case of pure shear we can see that there is no change of the volume Strain deviator tensor edit The infinitesimal strain tensor e i j displaystyle varepsilon ij nbsp similarly to the Cauchy stress tensor can be expressed as the sum of two other tensors a mean strain tensor or volumetric strain tensor or spherical strain tensor e M d i j displaystyle varepsilon M delta ij nbsp related to dilation or volume change and a deviatoric component called the strain deviator tensor e i j displaystyle varepsilon ij nbsp related to distortion e i j e i j e M d i j displaystyle varepsilon ij varepsilon ij varepsilon M delta ij nbsp where e M displaystyle varepsilon M nbsp is the mean strain given by e M e k k 3 e 11 e 22 e 33 3 1 3 I 1 e displaystyle varepsilon M frac varepsilon kk 3 frac varepsilon 11 varepsilon 22 varepsilon 33 3 tfrac 1 3 I 1 e nbsp The deviatoric strain tensor can be obtained by subtracting the mean strain tensor from the infinitesimal strain tensor e i j e i j e k k 3 d i j e 11 e 12 e 13 e 21 e 22 e 23 e 31 e 32 e 33 e 11 e 12 e 13 e 21 e 22 e 23 e 31 e 32 e 33 e M 0 0 0 e M 0 0 0 e M e 11 e M e 12 e 13 e 21 e 22 e M e 23 e 31 e 32 e 33 e M displaystyle begin aligned varepsilon ij amp varepsilon ij frac varepsilon kk 3 delta ij begin bmatrix varepsilon 11 amp varepsilon 12 amp varepsilon 13 varepsilon 21 amp varepsilon 22 amp varepsilon 23 varepsilon 31 amp varepsilon 32 amp varepsilon 33 end bmatrix amp begin bmatrix varepsilon 11 amp varepsilon 12 amp varepsilon 13 varepsilon 21 amp varepsilon 22 amp varepsilon 23 varepsilon 31 amp varepsilon 32 amp varepsilon 33 end bmatrix begin bmatrix varepsilon M amp 0 amp 0 0 amp varepsilon M amp 0 0 amp 0 amp varepsilon M end bmatrix amp begin bmatrix varepsilon 11 varepsilon M amp varepsilon 12 amp varepsilon 13 varepsilon 21 amp varepsilon 22 varepsilon M amp varepsilon 23 varepsilon 31 amp varepsilon 32 amp varepsilon 33 varepsilon M end bmatrix end aligned nbsp Octahedral strains edit Let n 1 n 2 n 3 displaystyle mathbf n 1 mathbf n 2 mathbf n 3 nbsp be the directions of the three principal strains An octahedral plane is one whose normal makes equal angles with the three principal directions The engineering shear strain on an octahedral plane is called the octahedral shear strain and is given byg o c t 2 3 e 1 e 2 2 e 2 e 3 2 e 3 e 1 2 displaystyle gamma mathrm oct tfrac 2 3 sqrt varepsilon 1 varepsilon 2 2 varepsilon 2 varepsilon 3 2 varepsilon 3 varepsilon 1 2 nbsp where e 1 e 2 e 3 displaystyle varepsilon 1 varepsilon 2 varepsilon 3 nbsp are the principal strains citation needed The normal strain on an octahedral plane is given bye o c t 1 3 e 1 e 2 e 3 displaystyle varepsilon mathrm oct tfrac 1 3 varepsilon 1 varepsilon 2 varepsilon 3 nbsp citation needed Equivalent strain edit A scalar quantity called the equivalent strain or the von Mises equivalent strain is often used to describe the state of strain in solids Several definitions of equivalent strain can be found in the literature A definition that is commonly used in the literature on plasticity ise e q 2 3 e d e v e d e v 2 3 e i j d e v e i j d e v e d e v e 1 3 t r e I displaystyle varepsilon mathrm eq sqrt tfrac 2 3 boldsymbol varepsilon mathrm dev boldsymbol varepsilon mathrm dev sqrt tfrac 2 3 varepsilon ij mathrm dev varepsilon ij mathrm dev boldsymbol varepsilon mathrm dev boldsymbol varepsilon tfrac 1 3 mathrm tr boldsymbol varepsilon boldsymbol I nbsp This quantity is work conjugate to the equivalent stress defined as s e q 3 2 s d e v s d e v displaystyle sigma mathrm eq sqrt tfrac 3 2 boldsymbol sigma mathrm dev boldsymbol sigma mathrm dev nbsp Compatibility equations editMain article Compatibility mechanics For prescribed strain components e i j displaystyle varepsilon ij nbsp the strain tensor equation u i j u j i 2 e i j displaystyle u i j u j i 2 varepsilon ij nbsp represents a system of six differential equations for the determination of three displacements components u i displaystyle u i nbsp giving an over determined system Thus a solution does not generally exist for an arbitrary choice of strain components Therefore some restrictions named compatibility equations are imposed upon the strain components With the addition of the three compatibility equations the number of independent equations are reduced to three matching the number of unknown displacement components These constraints on the strain tensor were discovered by Saint Venant and are called the Saint Venant compatibility equations The compatibility functions serve to assure a single valued continuous displacement function u i displaystyle u i nbsp If the elastic medium is visualised as a set of infinitesimal cubes in the unstrained state after the medium is strained an arbitrary strain tensor may not yield a situation in which the distorted cubes still fit together without overlapping In index notation the compatibility equations are expressed ase i j k m e k m i j e i k j m e j m i k 0 displaystyle varepsilon ij km varepsilon km ij varepsilon ik jm varepsilon jm ik 0 nbsp In engineering notation 2 ϵ x y 2 2 ϵ y x 2 2 2 ϵ x y x y displaystyle frac partial 2 epsilon x partial y 2 frac partial 2 epsilon y partial x 2 2 frac partial 2 epsilon xy partial x partial y nbsp 2 ϵ y z 2 2 ϵ z y 2 2 2 ϵ y z y z displaystyle frac partial 2 epsilon y partial z 2 frac partial 2 epsilon z partial y 2 2 frac partial 2 epsilon yz partial y partial z nbsp 2 ϵ x z 2 2 ϵ z x 2 2 2 ϵ z x z x displaystyle frac partial 2 epsilon x partial z 2 frac partial 2 epsilon z partial x 2 2 frac partial 2 epsilon zx partial z partial x nbsp 2 ϵ x y z x ϵ y z x ϵ z x y ϵ x y z displaystyle frac partial 2 epsilon x partial y partial z frac partial partial x left frac partial epsilon yz partial x frac partial epsilon zx partial y frac partial epsilon xy partial z right nbsp 2 ϵ y z x y ϵ y z x ϵ z x y ϵ x y z displaystyle frac partial 2 epsilon y partial z partial x frac partial partial y left frac partial epsilon yz partial x frac partial epsilon zx partial y frac partial epsilon xy partial z right nbsp 2 ϵ z x y z ϵ y z x ϵ z x y ϵ x y z displaystyle frac partial 2 epsilon z partial x partial y frac partial partial z left frac partial epsilon yz partial x frac partial epsilon zx partial y frac partial epsilon xy partial z right nbsp Special cases editPlane strain edit nbsp Plane strain state in a continuum In real engineering components stress and strain are 3 D tensors but in prismatic structures such as a long metal billet the length of the structure is much greater than the other two dimensions The strains associated with length i e the normal strain e 33 displaystyle varepsilon 33 nbsp and the shear strains e 13 displaystyle varepsilon 13 nbsp and e 23 displaystyle varepsilon 23 nbsp if the length is the 3 direction are constrained by nearby material and are small compared to the cross sectional strains Plane strain is then an acceptable approximation The strain tensor for plane strain is written as e e 11 e 12 0 e 21 e 22 0 0 0 0 displaystyle underline underline boldsymbol varepsilon begin bmatrix varepsilon 11 amp varepsilon 12 amp 0 varepsilon 21 amp varepsilon 22 amp 0 0 amp 0 amp 0 end bmatrix nbsp in which the double underline indicates a second order tensor This strain state is called plane strain The corresponding stress tensor is s s 11 s 12 0 s 21 s 22 0 0 0 s 33 displaystyle underline underline boldsymbol sigma begin bmatrix sigma 11 amp sigma 12 amp 0 sigma 21 amp sigma 22 amp 0 0 amp 0 amp sigma 33 end bmatrix nbsp in which the non zero s 33 displaystyle sigma 33 nbsp is needed to maintain the constraint ϵ 33 0 displaystyle epsilon 33 0 nbsp This stress term can be temporarily removed from the analysis to leave only the in plane terms effectively reducing the 3 D problem to a much simpler 2 D problem Antiplane strain edit Main article Antiplane shear Antiplane strain is another special state of strain that can occur in a body for instance in a region close to a screw dislocation The strain tensor for antiplane strain is given bye 0 0 e 13 0 0 e 23 e 13 e 23 0 displaystyle underline underline boldsymbol varepsilon begin bmatrix 0 amp 0 amp varepsilon 13 0 amp 0 amp varepsilon 23 varepsilon 13 amp varepsilon 23 amp 0 end bmatrix nbsp Relation to infinitesimal rotation tensor editSee also Spin tensor mechanics The infinitesimal strain tensor is defined ase 1 2 u u T displaystyle boldsymbol varepsilon frac 1 2 boldsymbol nabla mathbf u boldsymbol nabla mathbf u T nbsp Therefore the displacement gradient can be expressed as u e W displaystyle boldsymbol nabla mathbf u boldsymbol varepsilon boldsymbol W nbsp where W 1 2 u u T displaystyle boldsymbol W frac 1 2 boldsymbol nabla mathbf u boldsymbol nabla mathbf u T nbsp The quantity W displaystyle boldsymbol W nbsp is the infinitesimal rotation tensor or infinitesimal angular displacement tensor related to the infinitesimal rotation matrix This tensor is skew symmetric For infinitesimal deformations the scalar components of W displaystyle boldsymbol W nbsp satisfy the condition W i j 1 displaystyle W ij ll 1 nbsp Note that the displacement gradient is small only if both the strain tensor and the rotation tensor are infinitesimal The axial vector edit A skew symmetric second order tensor has three independent scalar components These three components are used to define an axial vector w displaystyle mathbf w nbsp as followsW i j ϵ i j k w k w i 1 2 ϵ i j k W j k displaystyle W ij epsilon ijk w k w i tfrac 1 2 epsilon ijk W jk nbsp where ϵ i j k displaystyle epsilon ijk nbsp is the permutation symbol In matrix form W 0 w 3 w 2 w 3 0 w 1 w 2 w 1 0 w w 1 w 2 w 3 displaystyle underline underline boldsymbol W begin bmatrix 0 amp w 3 amp w 2 w 3 amp 0 amp w 1 w 2 amp w 1 amp 0 end bmatrix underline mathbf w begin bmatrix w 1 w 2 w 3 end bmatrix nbsp The axial vector is also called the infinitesimal rotation vector The rotation vector is related to the displacement gradient by the relation w 1 2 u displaystyle mathbf w tfrac 1 2 boldsymbol nabla times mathbf u nbsp In index notation w i 1 2 ϵ i j k u k j displaystyle w i tfrac 1 2 epsilon ijk u k j nbsp If W 1 displaystyle lVert boldsymbol W rVert ll 1 nbsp and e 0 displaystyle boldsymbol varepsilon boldsymbol 0 nbsp then the material undergoes an approximate rigid body rotation of magnitude w displaystyle mathbf w nbsp around the vector w displaystyle mathbf w nbsp Relation between the strain tensor and the rotation vector edit Given a continuous single valued displacement field u displaystyle mathbf u nbsp and the corresponding infinitesimal strain tensor e displaystyle boldsymbol varepsilon nbsp we have see Tensor derivative continuum mechanics e e i j k e l j i e k e l 1 2 e i j k u l j i u j l i e k e l displaystyle boldsymbol nabla times boldsymbol varepsilon e ijk varepsilon lj i mathbf e k otimes mathbf e l tfrac 1 2 e ijk u l ji u j li mathbf e k otimes mathbf e l nbsp Since a change in the order of differentiation does not change the result u l j i u l i j displaystyle u l ji u l ij nbsp Therefore e i j k u l j i e 12 k e 21 k u l 12 e 13 k e 31 k u l 13 e 23 k e 32 k u l 32 0 displaystyle e ijk u l ji e 12k e 21k u l 12 e 13k e 31k u l 13 e 23k e 32k u l 32 0 nbsp Also 1 2 e i j k u j l i 1 2 e i j k u j i l 1 2 e k i j u j i l w k l displaystyle tfrac 1 2 e ijk u j li left tfrac 1 2 e ijk u j i right l left tfrac 1 2 e kij u j i right l w k l nbsp Hence e w k l e k e l w displaystyle boldsymbol nabla times boldsymbol varepsilon w k l mathbf e k otimes mathbf e l boldsymbol nabla mathbf w nbsp Relation between rotation tensor and rotation vector edit From an important identity regarding the curl of a tensor we know that for a continuous single valued displacement field u displaystyle mathbf u nbsp u 0 displaystyle boldsymbol nabla times boldsymbol nabla mathbf u boldsymbol 0 nbsp Since u e W displaystyle boldsymbol nabla mathbf u boldsymbol varepsilon boldsymbol W nbsp we have W e w displaystyle boldsymbol nabla times boldsymbol W boldsymbol nabla times boldsymbol varepsilon boldsymbol nabla mathbf w nbsp Strain tensor in non Cartesian coordinates editStrain tensor in cylindrical coordinates edit In cylindrical polar coordinates r 8 z displaystyle r theta z nbsp the displacement vector can be written asu u r e r u 8 e 8 u z e z displaystyle mathbf u u r mathbf e r u theta mathbf e theta u z mathbf e z nbsp The components of the strain tensor in a cylindrical coordinate system are given by 2 e r r u r r e 8 8 1 r u 8 8 u r e z z u z z e r 8 1 2 1 r u r 8 u 8 r u 8 r e 8 z 1 2 u 8 z 1 r u z 8 e z r 1 2 u r z u z r displaystyle begin aligned varepsilon rr amp cfrac partial u r partial r varepsilon theta theta amp cfrac 1 r left cfrac partial u theta partial theta u r right varepsilon zz amp cfrac partial u z partial z varepsilon r theta amp cfrac 1 2 left cfrac 1 r cfrac partial u r partial theta cfrac partial u theta partial r cfrac u theta r right varepsilon theta z amp cfrac 1 2 left cfrac partial u theta partial z cfrac 1 r cfrac partial u z partial theta right varepsilon zr amp cfrac 1 2 left cfrac partial u r partial z cfrac partial u z partial r right end aligned nbsp Strain tensor in spherical coordinates edit nbsp Spherical coordinates r 8 f as commonly used in physics radial distance r polar angle 8 theta and azimuthal angle f phi The symbol r rho is often used instead of r In spherical coordinates r 8 ϕ displaystyle r theta phi nbsp the displacement vector can be written asu u r e r u 8 e 8 u ϕ e ϕ displaystyle mathbf u u r mathbf e r u theta mathbf e theta u phi mathbf e phi nbsp The components of the strain tensor in a spherical coordinate system are given by 2 e r r u r r e 8 8 1 r u 8 8 u r e ϕ ϕ 1 r sin 8 u ϕ ϕ u r sin 8 u 8 cos 8 e r 8 1 2 mrow clas, wikipedia, wiki, book, books, library,

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