Hubbry Logo
Cauchy stress tensorCauchy stress tensorMain
Open search
Cauchy stress tensor
Community hub
Cauchy stress tensor
logo
8 pages, 0 posts
0 subscribers
Be the first to start a discussion here.
Be the first to start a discussion here.
Cauchy stress tensor
Cauchy stress tensor
from Wikipedia
Cauchy stress tensor
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
Dimension

In continuum mechanics, the Cauchy stress tensor (symbol , 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 and relates a unit-length direction vector e to the traction vector T(e) across a surface perpendicular to e:

[a]

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 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, , 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

[edit]
Figure 2.1a Internal distribution of contact forces and couple stresses on a differential of the internal surface in a continuum, as a result of the interaction between the two portions of the continuum separated by the surface
Figure 2.1b Internal distribution of contact forces and couple stresses on a differential of the internal surface in a continuum, as a result of the interaction between the two portions of the continuum separated by the surface
Figure 2.1c Stress vector on an internal surface S with normal vector n

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,[2] and it is represented by a field , called the traction vector, defined on the surface and assumed to depend continuously on the surface's normal unit vector .[3][4]: p.66–96 

To formulate the Euler–Cauchy stress principle, consider a surface passing through an internal material point 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 ).

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 and body forces .[5] Thus, the total force applied to a body or to a portion of the body can be expressed as:

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 , 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 , 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 containing , with normal vector , the force distribution is equipollent to a contact force exerted at point and surface moment . In particular, the contact force is given by

where is the mean surface traction.

Cauchy's stress principle asserts[6]: 47–102  that as tends to zero the ratio becomes and the couple stress vector 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 is defined as the surface traction,[7] also called stress vector,[8] traction,[4] or traction vector.[6] given by at the point associated with a plane with a normal vector :

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] 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 . It is not a vector field because it depends not only on the position of a particular material point, but also on the local orientation of the surface element as defined by its normal vector .[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 , and can be resolved into two components (Figure 2.1c):

  • one normal to the plane, called normal stress
where is the normal component of the force to the differential area
  • and the other parallel to this plane, called the shear stress
where is the tangential component of the force to the differential surface area . The shear stress can be further decomposed into two mutually perpendicular vectors.

Cauchy's postulate

[edit]

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

Cauchy's fundamental lemma

[edit]

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

Cauchy's stress theorem—stress tensor

[edit]

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:

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:

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):

and then substituting into the equation to cancel out dA:

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

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:

In index notation this is

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

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

or, equivalently,

Alternatively, in matrix form we have

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:

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

[edit]

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):

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

Figure 2.4 Transformation of the stress tensor

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

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

Normal and shear stresses

[edit]

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:

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

where

Balance laws – Cauchy's equations of motion

[edit]
Figure 4. Continuum body in equilibrium

Cauchy's first law of motion

[edit]

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:

where

For example, for a hydrostatic fluid in equilibrium conditions, the stress tensor takes on the form:

where is the hydrostatic pressure, and is the Kronecker delta.

Cauchy's second law of motion

[edit]

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, , or the continuum is a non-Newtonian fluid, which can lead to rotationally non-invariant fluids, such as polymers.

Principal stresses and stress invariants

[edit]
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

At every point in a stressed body there are at least three planes, called principal planes, with normal vectors , 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 , and where there are no normal shear stresses . The three stresses normal to these principal planes are called principal stresses.

The components 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 is given by:

where is a constant of proportionality, and in this particular case corresponds to the magnitudes of the normal stress vectors or principal stresses.

Knowing that and , we have

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

Expanding the determinant leads to the characteristic equation

where

The characteristic equation has three real roots (i.e. with a zero imaginary component) due to the stress tensor being symmetric. The , and , are the principal stresses, functions of the eigenvalues . 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 , and , 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 in the equation . 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:

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

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.

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:

Maximum and minimum shear stresses

[edit]

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 from the principal stress planes. The maximum shear stress is expressed as

Assuming then

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

Stress deviator tensor

[edit]

The stress tensor 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, , which tends to change the volume of the stressed body; and
  2. a deviatoric component called the stress deviator tensor, , which tends to distort it.

So

where is the mean stress given by

Pressure () 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.

where is a proportionality constant (viz. the Volume viscosity), is the divergence operator, is the kth Cartesian coordinate, is the flow velocity and is the kth Cartesian component of .

The deviatoric stress tensor can be obtained by subtracting the hydrostatic stress tensor from the Cauchy stress tensor:

Invariants of the stress deviator tensor

[edit]

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 are the same as the principal directions of the stress tensor . Thus, the characteristic equation is

where , and 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 or its principal values , , and , or alternatively, as a function of or its principal values , , and . Thus,

Because , 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

Octahedral stresses

[edit]
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 ) 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 and octahedral shear stress , 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, .

Knowing that the stress tensor of point O (Figure 6) in the principal axes is

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

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

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

See also

[edit]

Notes

[edit]

References

[edit]
Revisions and contributorsEdit on WikipediaRead on Wikipedia
from Grokipedia
The Cauchy stress tensor is a second-order tensor fundamental to continuum mechanics, representing the state of internal stress at a point in a material by specifying the force per unit area (traction) acting on any oriented surface passing through that point. Mathematically, it relates the traction vector t on a surface with unit normal n via Cauchy's theorem: t = σ · n, where σ denotes the tensor, ensuring a complete description of stresses in the current (deformed) configuration. This tensor, often denoted as σ or T, is symmetric (σ = σᵀ) due to the balance of angular momentum, which implies no net torque on infinitesimal elements in the absence of distributed couples. Named after the French mathematician Augustin-Louis Cauchy, who formalized the concept in 1822 as part of his foundational work on elasticity and the equilibrium of continuous media, the tensor provides a rigorous framework for analyzing forces in deforming bodies. Unlike earlier scalar or vector notions of stress, Cauchy's tensorial approach captures the directional dependence of stresses, with its nine components (reduced to six independent ones by symmetry) fully characterizing the stress state, including normal and shear components. It serves as the basis for Cauchy's equilibrium equations, ∇ · σ + b = ρ a, where b is body force density, ρ is mass density, and a is acceleration, linking stress to motion in continuous media. In applications, the Cauchy stress tensor is central to constitutive relations in solids (e.g., Hooke's law for linear elasticity) and fluids (e.g., Navier-Stokes equations for viscous flows), enabling predictions of deformation, failure, and flow behavior. It contrasts with other stress measures, such as the first Piola-Kirchhoff tensor (referential, unsymmetric), by being objective and tied to the instantaneous geometry, making it ideal for large-deformation analyses. Its eigenvalues represent principal stresses, and invariants (e.g., hydrostatic pressure as trace(σ)/3) quantify overall stress levels, influencing material stability and fracture criteria.

Introduction

Definition and Physical Interpretation

The Cauchy stress tensor, denoted by σ\boldsymbol{\sigma}, is a second-order tensor that fully characterizes the state of stress at a point in a continuum material. In three-dimensional space, it is represented as a 3×33 \times 3 symmetric matrix with nine components, where symmetry arises from the balance of angular momentum in the absence of body couples. This tensor encapsulates the distribution of internal forces acting across imaginary surfaces within the material. The fundamental relation defining the Cauchy stress tensor is the Cauchy stress formula, which connects the traction vector (or stress vector) t(n)\mathbf{t}^{(\mathbf{n})}—the force per unit area acting on a surface with unit outward normal n\mathbf{n}—to the tensor itself: t(n)=σn.\mathbf{t}^{(\mathbf{n})} = \boldsymbol{\sigma} \cdot \mathbf{n}. Here, t(n)\mathbf{t}^{(\mathbf{n})} represents the resultant force density on the oriented surface, with the dot product indicating a linear mapping from the normal direction to the traction components. In index notation, this is expressed as ti(n)=σijnjt_i^{(\mathbf{n})} = \sigma_{ij} n_j, where σij\sigma_{ij} denotes the component of the traction in the ii-th direction on a face perpendicular to the jj-th axis (using Einstein summation convention over repeated indices). Physically, the Cauchy stress tensor quantifies the true stresses in the current, deformed configuration of the body, measuring forces per unit area on surfaces as they exist after deformation, without reference to an undeformed state. It thus captures the internal resistance to deformation due to applied loads, such as tension, compression, or shear, at the material point. This makes it essential in continuum mechanics for modeling the response of solids, fluids, and other media under various loading conditions, enabling predictions of equilibrium, motion, and failure.

Historical Development

The concept of stress in continua began to take shape in the mid-18th century with Leonhard Euler's investigations into fluid motion. In works such as his 1761 "Principia motus fluidorum," Euler conceptualized the internal forces in fluids as directional pressures acting on surface elements, laying groundwork for a tensor-like representation of stress, though he primarily focused on inviscid flows where pressure was isotropic. This marked an initial shift from scalar notions of force in one-dimensional structures like bars toward more general descriptions in three-dimensional media. The modern formulation of the stress tensor emerged through Augustin-Louis Cauchy's pioneering efforts in the 1820s. In a memoir presented to the Académie des Sciences on September 30, 1822, Cauchy introduced the fundamental principles of stress, including the idea of a traction vector acting on arbitrary surface elements within a continuum, establishing the existence of a stress tensor for general solids and fluids. He further developed these ideas in his 1823 paper "Sur les équations qui expriment les conditions d'équilibre et les lois de mouvement des fluides," where he explicitly derived the tensor form for fluid equilibrium and motion, generalizing from scalar pressure to a full second-order tensor with directional components. This work represented a critical evolution, extending stress from simple normal forces in uniaxial cases to a complete 3D framework applicable to arbitrary continua, independent of specific material models. Subsequent refinements in the 19th century built upon Cauchy's foundation, particularly in linking the stress tensor to elastic and viscous behaviors. Claude-Louis Navier's 1822 memoir on the motion of elastic solids incorporated molecular force assumptions to relate stress components to deformations, influencing early tensor applications in elasticity. George Gabriel Stokes advanced this in 1845 by deriving the viscous stress contributions, completing the form now known as the Navier-Stokes equations and solidifying the tensor's role in both solids and fluids. The abstract tensor notation was later formalized by Gregorio Ricci-Curbastro in his 1890s development of tensor calculus, though its application to stress awaited broader adoption in the 20th century.

Stress Vector

Euler–Cauchy Stress Principle

The Euler–Cauchy stress principle asserts that the traction vector, or stress vector t(n)\mathbf{t}^{(\mathbf{n})}, acting across any oriented surface element within a continuum at a given point depends solely on the unit outward normal n\mathbf{n} to that surface and the location of the point itself, independent of the size, shape, or specific geometry of the surface element. This hypothesis, often termed the Euler-Cauchy hypothesis, ensures that the force per unit area transmitted between adjacent material parts is a continuous function of the surface orientation alone. Historically, the principle draws from Leonhard Euler's 18th-century conceptualization of pressure as an isotropic normal stress in fluids, which Augustin-Louis Cauchy extended in 1827 to a general directional stress vector applicable to deformable solids, thereby unifying the treatment of internal forces across different media. Cauchy's generalization transformed Euler's fluid-specific ideas into a foundational axiom for continuum mechanics, emphasizing the directional nature of stress beyond mere pressure. Conceptually, the principle underscores that stress is inherently a local property at each material point, allowing for a precise, pointwise description of internal interactions in continuous bodies without reliance on macroscopic surface details. This locality is essential for both solids, where stresses arise from deformation resistance, and fluids, where they stem from viscous and pressure effects, enabling consistent application across diverse continua under equilibrium or dynamic conditions. To illustrate this independence from global geometry, consider a thought experiment with an infinitesimal tetrahedral volume element embedded in the continuum, bounded by three faces aligned with coordinate planes and a fourth inclined face with normal n\mathbf{n}. Applying the linear momentum balance to this tetrahedron and taking the limit as its volume shrinks to zero reveals that body forces contribute negligibly compared to surface tractions, confirming that each traction t(n)\mathbf{t}^{(\mathbf{n})} is determined exclusively by the local normal n\mathbf{n} at the vertex point, unaffected by the element's distant boundaries or overall body shape.

Cauchy's Postulate

Cauchy's postulate states that the stress vector t(n)\mathbf{t}^{(\mathbf{n})} acting on a surface at a point within a continuous medium depends solely on the unit normal vector n\mathbf{n} to that surface and is a linear function of n\mathbf{n}, expressed as t(n)=σn\mathbf{t}^{(\mathbf{n})} = \boldsymbol{\sigma} \cdot \mathbf{n}, where σ\boldsymbol{\sigma} is the Cauchy stress tensor. This linearity implies that in component form, ti=σijnjt_i = \sigma_{ij} n_j, allowing the traction to be computed as a matrix-vector product without requiring knowledge of the specific surface geometry beyond its orientation. The postulate is justified through consideration of force equilibrium on an infinitesimal tetrahedral element at the point, where the contributions from body forces become negligible compared to surface tractions as the element size approaches zero, leading to a balance that enforces the linear dependence on n\mathbf{n}. This assumption also relies on the homogeneity of the continuum, ensuring that material properties and stress responses are uniform at the infinitesimal scale, independent of microscopic variations or surface curvature effects. A key implication of this linear relationship is that the complete state of stress at the point can be fully characterized by the nine independent components of the second-order tensor σ\boldsymbol{\sigma}, providing a compact representation that applies universally to any oriented surface passing through the point (with the number later reduced to six due to tensor symmetry). This finite parameterization facilitates the analysis of stress distribution in engineering and physical applications, transforming an infinite family of possible tractions into a manageable set of scalar values. To illustrate the linearity, consider a simple shear scenario in a viscous fluid between parallel plates, where the velocity gradient induces a shear stress σxy=μuy\sigma_{xy} = \mu \frac{\partial u}{\partial y} (with μ\mu as viscosity and all other components zero except possibly normal stresses). For a surface with normal n=(nx,ny,0)\mathbf{n} = (n_x, n_y, 0), the stress vector components become tx=σxynyt_x = \sigma_{xy} n_y and ty=σyxnx=σxynxt_y = \sigma_{yx} n_x = \sigma_{xy} n_x (by symmetry), demonstrating how the traction varies linearly with the normal's direction, yielding pure shear on the xyxy-plane (n=(0,1,0)\mathbf{n} = (0,1,0)) and zero traction on perpendicular planes.

Cauchy's Fundamental Lemma

Cauchy's fundamental lemma establishes the linear relationship between the stress vector on an arbitrary surface and the stress vectors on the coordinate faces through a geometric argument based on force equilibrium in a vanishingly small tetrahedral element. Formulated by Augustin-Louis Cauchy in his foundational work on continuum mechanics, the lemma posits that the stress vector t(n)\mathbf{t}^{( \mathbf{n} )} acting on a surface with unit normal n\mathbf{n} can be expressed as a weighted sum of the stress vectors t(ei)\mathbf{t}^{( \mathbf{e}_i )} on the faces perpendicular to the coordinate axes ei\mathbf{e}_i (for i=1,2,3i = 1, 2, 3), with weights given by the direction cosines ni=nein_i = \mathbf{n} \cdot \mathbf{e}_i. To derive this, consider an infinitesimal tetrahedron at a point in the continuum, with one vertex at the point and the opposite face having area ΔA\Delta A and outward unit normal n\mathbf{n}. The three adjacent faces have areas ΔAi=niΔA\Delta A_i = n_i \Delta A (for ni>0n_i > 0) and outward unit normals ei\mathbf{e}_i. The force balance on the tetrahedron requires that the sum of the surface tractions plus the body force equals the rate of change of momentum: t(n)ΔA+i=13t(ei)(ΔAi)+VρbdV=ddtVρvdV,\mathbf{t}^{(\mathbf{n})} \Delta A + \sum_{i=1}^3 \mathbf{t}^{(\mathbf{e}_i)} (-\Delta A_i) + \int_V \rho \mathbf{b} \, dV = \frac{d}{dt} \int_V \rho \mathbf{v} \, dV, where ρ\rho is the density, b\mathbf{b} the body force per unit mass, and v\mathbf{v} the velocity. As the edge length hh of the tetrahedron approaches zero, the volume V13hΔA=O(h3)V \approx \frac{1}{3} h \Delta A = O(h^3) tends to zero faster than the surface areas O(h2)O(h^2), rendering the body force integral and momentum term negligible compared to the surface terms. Substituting ΔAi=niΔA\Delta A_i = n_i \Delta A and dividing through by ΔA\Delta A yields t(n)=i=13nit(ei),\mathbf{t}^{(\mathbf{n})} = \sum_{i=1}^3 n_i \mathbf{t}^{(\mathbf{e}_i)}, in the limit h0h \to 0. This relation holds for any orientation n\mathbf{n}, assuming the continuum is in local equilibrium. The key assumptions underlying this derivation are that body forces and inertial effects are of higher order and vanish in the infinitesimal limit, allowing surface tractions to dominate the equilibrium. This neglect is valid for the local state of stress at a point, independent of global dynamics. The lemma thus provides a rigorous physical justification for the linearity assumed in Cauchy's postulate, enabling the representation of the stress state via a second-order tensor that linearly transforms surface normals into stress vectors.

The Cauchy Stress Tensor

Cauchy's Stress Theorem

Cauchy's stress theorem establishes the existence of a second-order tensor that relates the stress vector to the surface normal at any point in a continuum. Specifically, the theorem states that there exists a unique second-order tensor σ\sigma, called the Cauchy stress tensor, such that the stress vector t(n)\mathbf{t}^{(\mathbf{n})} acting on a surface element with unit outward normal n\mathbf{n} is given by t(n)=σn\mathbf{t}^{(\mathbf{n})} = \sigma \cdot \mathbf{n} for all unit vectors n\mathbf{n} in the three-dimensional Euclidean space. This relation holds pointwise and encapsulates the local state of stress in the material. The proof of the theorem relies on the linearity of the stress vector mapping, as established by prior principles in the theory of stress vectors. In a right-handed orthonormal Cartesian basis {e1,e2,e3}\{\mathbf{e}_1, \mathbf{e}_2, \mathbf{e}_3\}, the nine components of σ\sigma are defined by σij=t(ej)ei\sigma_{ij} = \mathbf{t}^{(\mathbf{e}_j)} \cdot \mathbf{e}_i, where t(ej)\mathbf{t}^{(\mathbf{e}_j)} is the stress vector on the plane perpendicular to ej\mathbf{e}_j. These components uniquely determine σ\sigma because the mapping nt(n)\mathbf{n} \mapsto \mathbf{t}^{(\mathbf{n})} is linear and continuous. In Euclidean space, every such linear transformation from vectors to vectors is uniquely represented by a second-order tensor, ensuring both existence and uniqueness. In matrix form within the same Cartesian coordinates, the Cauchy stress tensor σ\sigma is expressed as the 3×33 \times 3 array [σ]=(σ11σ12σ13σ21σ22σ23σ31σ32σ33),[\sigma] = \begin{pmatrix} \sigma_{11} & \sigma_{12} & \sigma_{13} \\ \sigma_{21} & \sigma_{22} & \sigma_{23} \\ \sigma_{31} & \sigma_{32} & \sigma_{33} \end{pmatrix},
Add your contribution
Related Hubs
User Avatar
No comments yet.