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Cauchy stress tensor

Representation of mechanical stress at every point within a deformed 3D object

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Through Stress (mechanics), Direction (geometry) and International System of Units

T(e)=e⋅σorTj(e)=∑iσijei.

The SI unit of both stress tensor and traction vector is the 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 two-dimensional coordinate transformations is 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, ⁠Kn→1⁠, 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

The Euler–Cauchy stress principle states that upon any surface 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, 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 normal unit vector ⁠n⁠.

To formulate the Euler–Cauchy stress principle, consider a 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. Thus, the total force F applied to a body or to a portion of the body can be expressed as:

F=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 that as ΔS 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, also called stress vector, traction, or traction vector. given by T(n)=Ti(n)ei at the point P associated with a plane with a normal vector ⁠n⁠:

Ti(n)=limΔS→0ΔFiΔS=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 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.

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=limΔS→0ΔFnΔS=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=limΔS→0ΔFsΔS=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, 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, also called the Cauchy reciprocal theorem, 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).

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