Cauchy stress tensor

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Cauchy stress tensor
File:Components stress tensor cartesian.svg
Components of stress in three dimensions
Common symbols
σ
SI unitpascal (Pa)
Other units
Pound per square inch (psi), bar
In SI base unitsPa = kgm−1s−2
Behaviour under
coord transformation
tensor

In continuum mechanics, the Cauchy stress tensor (symbol σ, named after Augustin-Louis Cauchy), also called true stress tensor[1] or simply stress tensor, completely defines the state of stress at a point inside a material in the deformed state, placement, or configuration. The second order tensor consists of nine components σij and relates a unit-length direction vector e to the traction vector T(e) across an imaginary surface perpendicular to e:

T(e)=eσorTj(e)=iσijei.[lower-alpha 1]

The SI base units of both stress tensor and traction vector are newton per square metre (N/m2) or pascal (Pa), corresponding to the stress scalar. The unit vector is dimensionless. The Cauchy stress tensor obeys the tensor transformation law under a change in the system of coordinates. A graphical representation of this transformation law is the Mohr's circle for stress. The Cauchy stress tensor is used for stress analysis of material bodies experiencing small deformations: it is a central concept in the linear theory of elasticity. For large deformations, also called finite deformations, other measures of stress are required, such as the Piola–Kirchhoff stress tensor, the Biot stress tensor, and the Kirchhoff stress tensor. According to the principle of conservation of linear momentum, if the continuum body is in static equilibrium it can be demonstrated that the components of the Cauchy stress tensor in every material point in the body satisfy the equilibrium equations (Cauchy's equations of motion for zero acceleration). At the same time, according to the principle of conservation of angular momentum, equilibrium requires that the summation of moments with respect to an arbitrary point is zero, which leads to the conclusion that the stress tensor is symmetric, thus having only six independent stress components, instead of the original nine. However, in the presence of couple-stresses, i.e. moments per unit volume, the stress tensor is non-symmetric. This also is the case when the Knudsen number is close to one, Kn1, or the continuum is a non-Newtonian fluid, which can lead to rotationally non-invariant fluids, such as polymers. There are certain invariants associated with the stress tensor, whose values do not depend upon the coordinate system chosen, or the area element upon which the stress tensor operates. These are the three eigenvalues of the stress tensor, which are called the principal stresses.

Euler–Cauchy stress principle – stress vector

File:Internal forces in continuum.svg
Figure 2.1a Internal distribution of contact forces and couple stresses on a differential dS of the internal surface S in a continuum, as a result of the interaction between the two portions of the continuum separated by the surface
File:Internal forces in continuum 2.svg
Figure 2.1b Internal distribution of contact forces and couple stresses on a differential dS of the internal surface S in a continuum, as a result of the interaction between the two portions of the continuum separated by the surface
File:Stress vector.svg
Figure 2.1c Stress vector on an internal surface S with normal vector n. Depending on the orientation of the plane under consideration, the stress vector may not necessarily be perpendicular to that plane, i.e. parallel to n, and can be resolved into two components: one component normal to the plane, called normal stress σn, and another component parallel to this plane, called the shearing stress τ.

The Euler–Cauchy stress principle states that upon any surface (real or imaginary) that divides the body, the action of one part of the body on the other is equivalent (equipollent) to the system of distributed forces and couples on the surface dividing the body,[2] and it is represented by a field T(n), called the traction vector, defined on the surface S and assumed to depend continuously on the surface's unit vector n.[3][4]: p.66–96  To formulate the Euler–Cauchy stress principle, consider an imaginary surface S passing through an internal material point P dividing the continuous body into two segments, as seen in Figure 2.1a or 2.1b (one may use either the cutting plane diagram or the diagram with the arbitrary volume inside the continuum enclosed by the surface S). Following the classical dynamics of Newton and Euler, the motion of a material body is produced by the action of externally applied forces which are assumed to be of two kinds: surface forces F and body forces b.[5] Thus, the total force applied to a body or to a portion of the body can be expressed as:

=b+F

Only surface forces will be discussed in this article as they are relevant to the Cauchy stress tensor. When the body is subjected to external surface forces or contact forces F, following Euler's equations of motion, internal contact forces and moments are transmitted from point to point in the body, and from one segment to the other through the dividing surface S, due to the mechanical contact of one portion of the continuum onto the other (Figure 2.1a and 2.1b). On an element of area ΔS containing P, with normal vector n, the force distribution is equipollent to a contact force ΔF exerted at point P and surface moment ΔM. In particular, the contact force is given by

ΔF=T(n)ΔS

where T(n) is the mean surface traction. Cauchy's stress principle asserts[6]: p.47–102  that as ΔS becomes very small and tends to zero the ratio ΔF/ΔS becomes dF/dS and the couple stress vector ΔM vanishes. In specific fields of continuum mechanics the couple stress is assumed not to vanish; however, classical branches of continuum mechanics address non-polar materials which do not consider couple stresses and body moments. The resultant vector dF/dS is defined as the surface traction,[7] also called stress vector,[8] traction,[4] or traction vector.[6] given by T(n)=Ti(n)ei at the point P associated with a plane with a normal vector n:

Ti(n)=limΔS0ΔFiΔS=dFidS.

This equation means that the stress vector depends on its location in the body and the orientation of the plane on which it is acting. This implies that the balancing action of internal contact forces generates a contact force density or Cauchy traction field [5] T(n,x,t) that represents a distribution of internal contact forces throughout the volume of the body in a particular configuration of the body at a given time t. It is not a vector field because it depends not only on the position x of a particular material point, but also on the local orientation of the surface element as defined by its normal vector n.[9] Depending on the orientation of the plane under consideration, the stress vector may not necessarily be perpendicular to that plane, i.e. parallel to n, and can be resolved into two components (Figure 2.1c):

  • one normal to the plane, called normal stress
σn=limΔS0ΔFnΔS=dFndS,
where dFn is the normal component of the force dF to the differential area dS
  • and the other parallel to this plane, called the shear stress
τ=limΔS0ΔFsΔS=dFsdS,
where dFs is the tangential component of the force dF to the differential surface area dS. The shear stress can be further decomposed into two mutually perpendicular vectors.

Cauchy's postulate

According to the Cauchy Postulate, the stress vector T(n) remains unchanged for all surfaces passing through the point P and having the same normal vector n at P,[7][10] i.e., having a common tangent at P. This means that the stress vector is a function of the normal vector n only, and is not influenced by the curvature of the internal surfaces.

Cauchy's fundamental lemma

A consequence of Cauchy's postulate is Cauchy's Fundamental Lemma,[1][7][11] also called the Cauchy reciprocal theorem,[12]: p.103–130  which states that the stress vectors acting on opposite sides of the same surface are equal in magnitude and opposite in direction. Cauchy's fundamental lemma is equivalent to Newton's third law of motion of action and reaction, and is expressed as

T(n)=T(n).

Cauchy's stress theorem—stress tensor

The state of stress at a point in the body is then defined by all the stress vectors T(n) associated with all planes (infinite in number) that pass through that point.[13] However, according to Cauchy's fundamental theorem,[11] also called Cauchy's stress theorem,[1] merely by knowing the stress vectors on three mutually perpendicular planes, the stress vector on any other plane passing through that point can be found through coordinate transformation equations. Cauchy's stress theorem states that there exists a second-order tensor field σ(x, t), called the Cauchy stress tensor, independent of n, such that T is a linear function of n:

T(n)=nσorTj(n)=σijni.

This equation implies that the stress vector T(n) at any point P in a continuum associated with a plane with normal unit vector n can be expressed as a function of the stress vectors on the planes perpendicular to the coordinate axes, i.e. in terms of the components σij of the stress tensor σ. To prove this expression, consider a tetrahedron with three faces oriented in the coordinate planes, and with an infinitesimal area dA oriented in an arbitrary direction specified by a normal unit vector n (Figure 2.2). The tetrahedron is formed by slicing the infinitesimal element along an arbitrary plane with unit normal n. The stress vector on this plane is denoted by T(n). The stress vectors acting on the faces of the tetrahedron are denoted as T(e1), T(e2), and T(e3), and are by definition the components σij of the stress tensor σ. This tetrahedron is sometimes called the Cauchy tetrahedron. The equilibrium of forces, i.e. Euler's first law of motion (Newton's second law of motion), gives:

T(n)dAT(e1)dA1T(e2)dA2T(e3)dA3=ρ(h3dA)a,
File:Cauchy tetrahedron.svg
Figure 2.2. Stress vector acting on a plane with normal unit vector n.
A note on the sign convention: The tetrahedron is formed by slicing a parallelepiped along an arbitrary plane n. So, the force acting on the plane n is the reaction exerted by the other half of the parallelepiped and has an opposite sign.

where the right-hand-side represents the product of the mass enclosed by the tetrahedron and its acceleration: ρ is the density, a is the acceleration, and h is the height of the tetrahedron, considering the plane n as the base. The area of the faces of the tetrahedron perpendicular to the axes can be found by projecting dA into each face (using the dot product):

dA1=(ne1)dA=n1dA,
dA2=(ne2)dA=n2dA,
dA3=(ne3)dA=n3dA,

and then substituting into the equation to cancel out dA:

T(n)T(e1)n1T(e2)n2T(e3)n3=ρ(h3)a.

To consider the limiting case as the tetrahedron shrinks to a point, h must go to 0 (intuitively, the plane n is translated along n toward O). As a result, the right-hand-side of the equation approaches 0, so

T(n)=T(e1)n1+T(e2)n2+T(e3)n3.

Assuming a material element (see figure at the top of the page) with planes perpendicular to the coordinate axes of a Cartesian coordinate system, the stress vectors associated with each of the element planes, i.e. T(e1), T(e2), and T(e3) can be decomposed into a normal component and two shear components, i.e. components in the direction of the three coordinate axes. For the particular case of a surface with normal unit vector oriented in the direction of the x1-axis, denote the normal stress by σ11, and the two shear stresses as σ12 and σ13:

T(e1)=T1(e1)e1+T2(e1)e2+T3(e1)e3=σ11e1+σ12e2+σ13e3,
T(e2)=T1(e2)e1+T2(e2)e2+T3(e2)e3=σ21e1+σ22e2+σ23e3,
T(e3)=T1(e3)e1+T2(e3)e2+T3(e3)e3=σ31e1+σ32e2+σ33e3,

In index notation this is

T(ei)=Tj(ei)ej=σijej.

The nine components σij of the stress vectors are the components of a second-order Cartesian tensor called the Cauchy stress tensor, which can be used to completely define the state of stress at a point and is given by

σ=σij=[T(e1)T(e2)T(e3)]=[σ11σ12σ13σ21σ22σ23σ31σ32σ33][σxxσxyσxzσyxσyyσyzσzxσzyσzz][σxτxyτxzτyxσyτyzτzxτzyσz],

where σ11, σ22, and σ33 are normal stresses, and σ12, σ13, σ21, σ23, σ31, and σ32 are shear stresses. The first index i indicates that the stress acts on a plane normal to the Xi -axis, and the second index j denotes the direction in which the stress acts (For example, σ12 implies that the stress is acting on the plane that is normal to the 1st axis i.e.;X1 and acts along the 2nd axis i.e.;X2). A stress component is positive if it acts in the positive direction of the coordinate axes, and if the plane where it acts has an outward normal vector pointing in the positive coordinate direction. Thus, using the components of the stress tensor

T(n)=T(e1)n1+T(e2)n2+T(e3)n3=i=13T(ei)ni=(σijej)ni=σijniej

or, equivalently,

Tj(n)=σijni.

Alternatively, in matrix form we have

[T1(n)T2(n)T3(n)]=[n1n2n3][σ11σ12σ13σ21σ22σ23σ31σ32σ33].

The Voigt notation representation of the Cauchy stress tensor takes advantage of the symmetry of the stress tensor to express the stress as a six-dimensional vector of the form:

σ=[σ1σ2σ3σ4σ5σ6]T[σ11σ22σ33σ23σ13σ12]T.

The Voigt notation is used extensively in representing stress–strain relations in solid mechanics and for computational efficiency in numerical structural mechanics software.

Transformation rule of the stress tensor

It can be shown that the stress tensor is a contravariant second order tensor, which is a statement of how it transforms under a change of the coordinate system. From an xi-system to an xi' -system, the components σij in the initial system are transformed into the components σij' in the new system according to the tensor transformation rule (Figure 2.4):

σ'ij=aimajnσmnorσ=AσAT,

where A is a rotation matrix with components aij. In matrix form this is

[σ'11σ'12σ'13σ'21σ'22σ'23σ'31σ'32σ'33]=[a11a12a13a21a22a23a31a32a33][σ11σ12σ13σ21σ22σ23σ31σ32σ33][a11a21a31a12a22a32a13a23a33].
File:Stress transformation 3D.svg
Figure 2.4 Transformation of the stress tensor

Expanding the matrix operation, and simplifying terms using the symmetry of the stress tensor, gives

σ11=a112σ11+a122σ22+a132σ33+2a11a12σ12+2a11a13σ13+2a12a13σ23,σ22=a212σ11+a222σ22+a232σ33+2a21a22σ12+2a21a23σ13+2a22a23σ23,σ33=a312σ11+a322σ22+a332σ33+2a31a32σ12+2a31a33σ13+2a32a33σ23,σ12=a11a21σ11+a12a22σ22+a13a23σ33+(a11a22+a12a21)σ12+(a12a23+a13a22)σ23+(a11a23+a13a21)σ13,σ23=a21a31σ11+a22a32σ22+a23a33σ33+(a21a32+a22a31)σ12+(a22a33+a23a32)σ23+(a21a33+a23a31)σ13,σ13=a11a31σ11+a12a32σ22+a13a33σ33+(a11a32+a12a31)σ12+(a12a33+a13a32)σ23+(a11a33+a13a31)σ13.

The Mohr circle for stress is a graphical representation of this transformation of stresses.

Normal and shear stresses

The magnitude of the normal stress component σn of any stress vector T(n) acting on an arbitrary plane with normal unit vector n at a given point, in terms of the components σij of the stress tensor σ, is the dot product of the stress vector and the normal unit vector:

σn=T(n)n=Ti(n)ni=σijninj.

The magnitude of the shear stress component τn, acting orthogonal to the vector n, can then be found using the Pythagorean theorem:

τn=(T(n))2σn2=Ti(n)Ti(n)σn2,

where

(T(n))2=Ti(n)Ti(n)=(σijnj)(σiknk)=σijσiknjnk.

Balance laws – Cauchy's equations of motion

File:Equilibrium equation body.svg
Figure 4. Continuum body in equilibrium

Cauchy's first law of motion

According to the principle of conservation of linear momentum, if the continuum body is in static equilibrium it can be demonstrated that the components of the Cauchy stress tensor in every material point in the body satisfy the equilibrium equations:

σji,j+Fi=0,

where σji,j=jjσji For example, for a hydrostatic fluid in equilibrium conditions, the stress tensor takes on the form:

σij=pδij,

where p is the hydrostatic pressure, and δij is the kronecker delta.

Cauchy's second law of motion

According to the principle of conservation of angular momentum, equilibrium requires that the summation of moments with respect to an arbitrary point is zero, which leads to the conclusion that the stress tensor is symmetric, thus having only six independent stress components, instead of the original nine:

σij=σji

However, in the presence of couple-stresses, i.e. moments per unit volume, the stress tensor is non-symmetric. This also is the case when the Knudsen number is close to one, Kn1, or the continuum is a non-Newtonian fluid, which can lead to rotationally non-invariant fluids, such as polymers.

Principal stresses and stress invariants

File:2D stress.gif
Stress components on a 2D rotating element. Example of how stress components vary on the faces (edges) of a rectangular element as the angle of its orientation is varied. Principal stresses occur when the shear stresses simultaneously disappear from all faces. The orientation at which this occurs gives the principal directions. In this example, when the rectangle is horizontal, the stresses are given by [σ11σ12σ21σ22]=[10101015].

At every point in a stressed body there are at least three planes, called principal planes, with normal vectors n, called principal directions, where the corresponding stress vector is perpendicular to the plane, i.e., parallel or in the same direction as the normal vector n, and where there are no normal shear stresses τn. The three stresses normal to these principal planes are called principal stresses. The components σij of the stress tensor depend on the orientation of the coordinate system at the point under consideration. However, the stress tensor itself is a physical quantity and as such, it is independent of the coordinate system chosen to represent it. There are certain invariants associated with every tensor which are also independent of the coordinate system. For example, a vector is a simple tensor of rank one. In three dimensions, it has three components. The value of these components will depend on the coordinate system chosen to represent the vector, but the magnitude of the vector is a physical quantity (a scalar) and is independent of the Cartesian coordinate system chosen to represent the vector (so long as it is normal). Similarly, every second rank tensor (such as the stress and the strain tensors) has three independent invariant quantities associated with it. One set of such invariants are the principal stresses of the stress tensor, which are just the eigenvalues of the stress tensor. Their direction vectors are the principal directions or eigenvectors. A stress vector parallel to the normal unit vector n is given by:

T(n)=λn=σnn

where λ is a constant of proportionality, and in this particular case corresponds to the magnitudes σn of the normal stress vectors or principal stresses. Knowing that Ti(n)=σijnj and ni=δijnj, we have

Ti(n)=λniσijnj=λniσijnjλni=0(σijλδij)nj=0

This is a homogeneous system, i.e. equal to zero, of three linear equations where nj are the unknowns. To obtain a nontrivial (non-zero) solution for nj, the determinant matrix of the coefficients must be equal to zero, i.e. the system is singular. Thus,

|σijλδij|=|σ11λσ12σ13σ21σ22λσ23σ31σ32σ33λ|=0

Expanding the determinant leads to the characteristic equation

|σijλδij|=λ3+I1λ2I2λ+I3=0

where

I1=σ11+σ22+σ33=σkk=tr(σ)I2=|σ22σ23σ32σ33|+|σ11σ13σ31σ33|+|σ11σ12σ21σ22|=σ11σ22+σ22σ33+σ11σ33σ122σ232σ312=12(σiiσjjσijσji)=12[(tr(σ))2tr(σ2)]I3=det(σij)=det(σ)=σ11σ22σ33+2σ12σ23σ31σ122σ33σ232σ11σ312σ22

The characteristic equation has three real roots λi, i.e. not imaginary due to the symmetry of the stress tensor. The σ1=max(λ1,λ2,λ3), σ3=min(λ1,λ2,λ3) and σ2=I1σ1σ3, are the principal stresses, functions of the eigenvalues λi. The eigenvalues are the roots of the characteristic polynomial. The principal stresses are unique for a given stress tensor. Therefore, from the characteristic equation, the coefficients I1, I2 and I3, called the first, second, and third stress invariants, respectively, always have the same value regardless of the coordinate system's orientation. For each eigenvalue, there is a non-trivial solution for nj in the equation (σijλδij)nj=0. These solutions are the principal directions or eigenvectors defining the plane where the principal stresses act. The principal stresses and principal directions characterize the stress at a point and are independent of the orientation. A coordinate system with axes oriented to the principal directions implies that the normal stresses are the principal stresses and the stress tensor is represented by a diagonal matrix:

σij=[σ1000σ2000σ3]

The principal stresses can be combined to form the stress invariants, I1, I2, and I3. The first and third invariant are the trace and determinant respectively, of the stress tensor. Thus,

I1=σ1+σ2+σ3I2=σ1σ2+σ2σ3+σ3σ1I3=σ1σ2σ3

Because of its simplicity, the principal coordinate system is often useful when considering the state of the elastic medium at a particular point. Principal stresses are often expressed in the following equation for evaluating stresses in the x and y directions or axial and bending stresses on a part.[14]: p.58–59  The principal normal stresses can then be used to calculate the von Mises stress and ultimately the safety factor and margin of safety.

σ1,σ2=σx+σy2±(σxσy2)2+τxy2

Using just the part of the equation under the square root is equal to the maximum and minimum shear stress for plus and minus. This is shown as:

τmax,τmin=±(σxσy2)2+τxy2

Maximum and minimum shear stresses

The maximum shear stress or maximum principal shear stress is equal to one-half the difference between the largest and smallest principal stresses, and acts on the plane that bisects the angle between the directions of the largest and smallest principal stresses, i.e. the plane of the maximum shear stress is oriented 45 from the principal stress planes. The maximum shear stress is expressed as

τmax=12|σmaxσmin|

Assuming σ1σ2σ3 then

τmax=12|σ1σ3|

When the stress tensor is non zero the normal stress component acting on the plane for the maximum shear stress is non-zero and it is equal to

σn=12(σ1+σ3)

Stress deviator tensor

The stress tensor σij can be expressed as the sum of two other stress tensors:

  1. a mean hydrostatic stress tensor or volumetric stress tensor or mean normal stress tensor, πδij, which tends to change the volume of the stressed body; and
  2. a deviatoric component called the stress deviator tensor, sij, which tends to distort it.

So

σij=sij+πδij,

where π is the mean stress given by

π=σkk3=σ11+σ22+σ333=13I1.

Pressure (p) is generally defined as negative one-third the trace of the stress tensor minus any stress the divergence of the velocity contributes with, i.e.

p=λuπ=λukxkπ=kλukxkπ,

where λ is a proportionality constant (viz. the first of the Lamé parameters), is the divergence operator, xk is the k:th Cartesian coordinate, u is the flow velocity and uk is the k:th Cartesian component of u. The deviatoric stress tensor can be obtained by subtracting the hydrostatic stress tensor from the Cauchy stress tensor:

sij=σijσkk3δij,[s11s12s13s21s22s23s31s32s33]=[σ11σ12σ13σ21σ22σ23σ31σ32σ33][π000π000π]=[σ11πσ12σ13σ21σ22πσ23σ31σ32σ33π].

Invariants of the stress deviator tensor

As it is a second order tensor, the stress deviator tensor also has a set of invariants, which can be obtained using the same procedure used to calculate the invariants of the stress tensor. It can be shown that the principal directions of the stress deviator tensor sij are the same as the principal directions of the stress tensor σij. Thus, the characteristic equation is

|sijλδij|=λ3J1λ2J2λJ3=0,

where J1, J2 and J3 are the first, second, and third deviatoric stress invariants, respectively. Their values are the same (invariant) regardless of the orientation of the coordinate system chosen. These deviatoric stress invariants can be expressed as a function of the components of sij or its principal values s1, s2, and s3, or alternatively, as a function of σij or its principal values σ1, σ2, and σ3. Thus,

J1=skk=0,J2=12sijsji=12tr(s2)=12(s12+s22+s32)=16[(σ11σ22)2+(σ22σ33)2+(σ33σ11)2]+σ122+σ232+σ312=16[(σ1σ2)2+(σ2σ3)2+(σ3σ1)2]=13I12I2=12[tr(σ2)13tr(σ)2],J3=det(sij)=13sijsjkski=13tr(s3)=13(s13+s23+s33)=s1s2s3=227I1313I1I2+I3=13[tr(σ3)tr(σ2)tr(σ)+29tr(σ)3].

Because skk=0, the stress deviator tensor is in a state of pure shear. A quantity called the equivalent stress or von Mises stress is commonly used in solid mechanics. The equivalent stress is defined as

σvM=3J2=12[(σ1σ2)2+(σ2σ3)2+(σ3σ1)2].

Octahedral stresses

File:Octahedral stress planes.svg
Figure 6. Octahedral stress planes

Considering the principal directions as the coordinate axes, a plane whose normal vector makes equal angles with each of the principal axes (i.e. having direction cosines equal to |1/3|) is called an octahedral plane. There are a total of eight octahedral planes (Figure 6). The normal and shear components of the stress tensor on these planes are called octahedral normal stress σoct and octahedral shear stress τoct, respectively. Octahedral plane passing through the origin is known as the π-plane (π not to be confused with mean stress denoted by π in above section) . On the π-plane, sij=13I. Knowing that the stress tensor of point O (Figure 6) in the principal axes is

σij=[σ1000σ2000σ3]

the stress vector on an octahedral plane is then given by:

Toct(n)=σijniej=σ1n1e1+σ2n2e2+σ3n3e3=13(σ1e1+σ2e2+σ3e3)

The normal component of the stress vector at point O associated with the octahedral plane is

σoct=Ti(n)ni=σijninj=σ1n1n1+σ2n2n2+σ3n3n3=13(σ1+σ2+σ3)=13I1

which is the mean normal stress or hydrostatic stress. This value is the same in all eight octahedral planes. The shear stress on the octahedral plane is then

τoct=Ti(n)Ti(n)σoct2=[13(σ12+σ22+σ32)19(σ1+σ2+σ3)2]12=13[(σ1σ2)2+(σ2σ3)2+(σ3σ1)2]12=132I126I2=23J2

See also

Notes

  1. In detail:
    [T1(e)T2(e)T3(e)]=[e1e2e3][σ11σ12σ13σ21σ22σ23σ31σ32σ33].

References

  1. 1.0 1.1 1.2 Fridtjov Irgens (2008), "Continuum Mechanics". Springer. ISBN 3-540-74297-2
  2. Truesdell, C.; Toupin, R.A. (1960), "The Classical Field Theories", in Flügge, Siegfried (ed.), Principles of Classical Mechanics and Field Theory/Prinzipien der Klassischen Mechanik und Feldtheorie, Handbuch der Physik (Encyclopedia of Physics), vol. III/1, Berlin–Heidelberg–New York: Springer-Verlag, pp. 226–793, Bibcode:1960HDP.....2.....F, doi:10.1007/978-3-642-45943-6, ISBN 978-3-540-02547-4, MR 0118005, Zbl 0118.39702.
  3. Peter Chadwick (1999), "Continuum Mechanics: Concise Theory and Problems". Dover Publications, series "Books on Physics". ISBN 0-486-40180-4. pages
  4. 4.0 4.1 Yuan-cheng Fung and Pin Tong (2001) "Classical and Computational Solid Mechanics". World Scientific. ISBN 981-02-4124-0
  5. 5.0 5.1 Smith & Truesdell p.97
  6. 6.0 6.1 G. Thomas Mase and George E. Mase (1999), "Continuum Mechanics for Engineers" (2nd edition). CRC Press. ISBN 0-8493-1855-6
  7. 7.0 7.1 7.2 I-Shih Liu (2002), "Continuum Mechanics". Springer ISBN 3-540-43019-9
  8. 8.0 8.1 Han-Chin Wu (2005), "Continuum Mechanics and Plasticity". CRC Press. ISBN 1-58488-363-4
  9. Lubliner
  10. Basar
  11. 11.0 11.1 11.2 Teodor M. Atanackovic and Ardéshir Guran (2000), "Theory of Elasticity for Scientists and Engineers". Springer. ISBN 0-8176-4072-X
  12. Keith D. Hjelmstad (2005), "Fundamentals of Structural Mechanics" (2nd edition). Prentice-Hall. ISBN 0-387-23330-X
  13. 13.0 13.1 Wai-Fah Chen and Da-Jian Han (2007), "Plasticity for Structural Engineers". J. Ross Publishing ISBN 1-932159-75-4
  14. Bernard Hamrock (2005), "Fundamentals of Machine Elements". McGraw–Hill. ISBN 0-07-297682-9
  15. Rabindranath Chatterjee (1999), "Mathematical Theory of Continuum Mechanics". Alpha Science. ISBN 81-7319-244-8
  16. John Conrad Jaeger, N. G. W. Cook, and R. W. Zimmerman (2007), "Fundamentals of Rock Mechanics" (4th edition). Wiley-Blackwell. ISBN 0-632-05759-9
  17. Mohammed Ameen (2005), "Computational Elasticity: Theory of Elasticity and Finite and Boundary Element Methods" (book). Alpha Science, ISBN 1-84265-201-X
  18. William Prager (2004), "Introduction to Mechanics of Continua". Dover Publications. ISBN 0-486-43809-0