Stress (mechanics)
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In continuum mechanics, stress is a measure of the internal forces acting within a deformable body. Quantitatively, it is a measure of the average force per unit area of a surface within the body on which internal forces act. These internal forces are produced between the particles in the body as a reaction to external forces applied on the body. Because the loaded deformable body is assumed to behave as a continuum, these internal forces are distributed continuously within the volume of the material body, and result in deformation of the body's shape. Beyond certain limits of material strength, this can lead to a permanent change of shape or physical failure.
The dimension of stress is that of pressure, and therefore the SI unit for stress is the pascal (symbol Pa), which is equivalent to one newton (force) per square meter (unit area). In Imperial units, stress is measured in pound-force per square inch, which is abbreviated as psi.
Einführung
Stress is a measure of the average force per unit area of a surface within a deformable body on which internal forces act. It is a measure of the intensity of the internal forces acting between particles of a deformable body across imaginary internal surfaces[2]. These internal forces are produced between the particles in the body as a reaction to external forces applied on the body. External forces are either surface forces or body forces. Because the loaded deformable body is assumed to behave as a continuum, these internal forces are distributed continuously within the volume of the material body, i.e. the stress distribution in the body is expressed as a piecewise continuous function of space coordinates and time.
Normal and shear stresses
For the simple case of a body axially loaded, e.g., a prismatic bar subjected to tension oder compression by a force passing through its centroid (Figures 1.2 and 1.3) the stress , or intensity of internal forces, can be obtained by dividing the total normal force , determined from the equilibrium of forces, by the cross-sectional area of the prism it is acting upon. The normal force can be a tensile force if acting outward from the plane, or compressive force if acting inward to the plane. In the case of a prismatic bar axially loaded, the stress is represented by a scalar called engineering stress oder nominal stress that represents an average stress () over the area, meaning that the stress in the cross section is uniformly distributed. Thus, we have
A different type of stress is obtained when transverse forces are applied to the prismatic bar as shown in Figure 1.4. Considering the same cross-section as before, from static equilibrium the internal force has a magnitude equal to and in opposite direction parallel to the cross-section. is called the shear force. Dividing the shear force by the area of the cross section we obtain the shear stress. In this case the shear stress is a scalar quantity representing an average shear stress () in the section, i.e. the stress in the cross-section is uniformly distributed.
In Figure 1.3, the normal stress is observed in two planes and of the axially loaded prismatic bar. The stress on plane , which is closer to the point of application of the load , varies more across the cross-section than that of plane . However, if the cross-sectional area of the bar is very small, i.e. the bar is slender, the variation of stress across the area is small and the normal stress can be approximated by . On the other hand, the variation of shear stress across the section of a prismatic bar cannot be assumed to be uniform.
Stress modeling (Cauchy)
In general, stress is not uniformly distributed over the cross-section of a material body, and consequently the stress at a point in a given region is different from the average stress over the entire area. Therefore, it is necessary to define the stress not over a given area but at a specific point in the body (Figure 1.1). According to Cauchy, the stress at any point in an object assumed to behave as a continuum is completely defined by the nine components of a second-order tensor of type (0,2) known as the Cauchy stress tensor, :
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. For large deformations, also called finite deformations, other measures of stress, such as the first and second Piola-Kirchhoff stress tensors, the Biot stress tensor, and the Kirchhoff stress tensor, are required.
According to the principle of conservation of linear momentum, if a continuous 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.
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. Solids, liquids, and gases have stress fields. Static fluids support normal stress but will flow under shear stress. Moving viscous fluids can support shear stress (dynamic pressure). Solids can support both shear and normal stress, with ductile materials failing under shear and brittle materials failing under normal stress. All materials have temperature dependent variations in stress-related properties, and non-Newtonian materials have rate-dependent variations.
Stress analysis
Stress analysis, i.e. the determination of the internal distribution of stresses is required in engineering for the study and design of structures, e.g., tunnels, dams, mechanical parts, and structural frames, among others, under prescribed or expected loads. To determine the distribution of stress in the structure it is necessary to solve a boundary-value problem by specifying the boundary conditions, i.e. displacements and forces on the boundary. Constitutive equations, such as Hooke’s Law for linear elastic materials, are used to describe the stress-strain relationship in these calculations. A boundary-value problem based on the theory of elasticity is applied to structures expected to deform elastically, with infinitesimal strains, under design loads. When the loads applied to the structure induce plastic deformations, the theory of plasticity is implemented.
The stress analysis can be simplified in cases where the physical dimensions and the distribution of loads allow the structure to be treated as one-dimensional or two-dimensional. For a two-dimensional analysis a plane stress or a plane strain condition can be assumed. Alternatively, experimental determination of stresses can be carried out.
Approximate solutions for boundary-value problems can be obtained through the use of numerical methods such as the Finite Element Method, the Finite Difference Method, and the Boundary Element Method, which are implemented in computer programs. Analytical or closed-form solutions can be obtained for simple geometries, constitutive relations, and boundary conditions.
Theoretical background
Continuum mechanics deals with deformable bodies, as opposed to rigid bodies. The stresses considered in continuum mechanics are only those produced by deformation of the body, sc. only relative changes in stress are considered, not the absolute values. A body is considered stress-free if the only forces present are those inter-atomic forces (ionic, metallic, and van der Waals forces) required to hold the body together and to keep its shape in the absence of all external influences, including gravitational attraction.[3][4] Stresses generated during manufacture of the body to a specific configuration are also excluded.
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]
Surface forces, or contact forces, can act either on the bounding surface of the body, as a result of mechanical contact with other bodies, or on imaginary internal surfaces that bound portions of the body, as a result of the mechanical interaction between the parts of the body to either side of the surface (Euler-Cauchy's stress principle). When a body is acted upon by external contact forces, internal contact forces are then transmitted from point to point inside the body to balance their action, according to Newton's second law of motion of conservation of linear momentum and angular momentum (for continuous bodies these laws are called the Euler's equations of motion). The internal contact forces are related to the body's deformation through constitutive equations. This article is concerned with the manner in which internal contact forces are mathematically described and how they relate to the motion of the body, independent of the body's material makeup.[6]
The concept of stress can then be thought as a measure of the intensity of the internal contact forces acting between particles of the body across imaginary internal surfaces.[2] In other words, stress is a measure of the average quantity of force exerted per unit area of the surface on which these internal forces act. The intensity of contact forces is related, specifically in an inverse proportion, to the area of contact. For example, if a force applied to a small area is compared to a distributed load of the same resultant magnitude applied to a larger area, one finds that the effects or intensities of these two forces are locally different because the stresses are not the same.
Body forces are forces originating from sources outside of the body[7] that act on the volume (or mass) of the body. Saying that body forces are due to outside sources implies that the internal forces are manifested through the contact forces alone.[8] These forces arise from the presence of the body in force fields, (e.g., a gravitational field). As the mass of a continuous body is assumed to be continuously distributed, any force originating from the mass is also continuously distributed. Thus, body forces are assumed to be continuous over the entire volume of the body.[9]
The density of internal forces at every point in a deformable body are not necessarily equal, i.e. there is a distribution of stresses throughout the body. This variation of internal forces throughout the body is governed by Newton's second law of motion of conservation of linear momentum and angular momentum, which normally are applied to a mass particle but are extended in continuum mechanics to a body of continuously distributed mass. For continuous bodies these laws are called Euler’s equations of motion. If a body is represented as an assemblage of discrete particles, each governed by Newton’s laws of motion, then Euler’s equations can be derived from Newton’s laws. Euler’s equations can, however, be taken as axioms describing the laws of motion for extended bodies, independently of any particle structure.[10]
Euler-Cauchy stress principle
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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,[11] and it is represented by a vector field , called the stress vector, defined on the surface and assumed to depend continuously on the surfaces unit vectors .[12][9]
To explain this principle, we consider an imaginary surface passing through an internal material point dividing the continuous body into two segments, as seen in Figure 2.1a or 2.1b (some authors use the cutting plane diagram[citation needed] and others[citation needed] use the diagram with the arbitrary volume inside the continuum enclosed by the surface ). The body is subjected to external surface forces and body forces . The internal contact forces being transmitted from one segment to the other through the dividing plane, due to the action of one portion of the continuum onto the other, generate a force distribution on a small area , with a normal unit vector , on the dividing plane . The force distribution is equipollent to a contact force and a couple stress , as shown in Figure 2.1a and 2.1b. Cauchy’s stress principle asserts[3] that as becomes very small and 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, as stated previously, in classical branches of continuum mechanics we deal with non-polar materials which do not consider couple stresses and body moments. The resultant vector is defined as the stress vector oder traction vector given by at 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.
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:
- 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 shearing 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
According to the Cauchy Postulate, the stress vector remains unchanged for all surfaces passing through a point and having the same normal vector at ,[8][13] i.e. having a common tangent at . This means that the stress vector is only a function of the normal vector , and it 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[8][4][7], also called the Cauchy reciprocal theorem[14], 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 it is expressed as
Derivation of Cauchy’s Lemma Derivation coming soon
Cauchy’s stress theorem – stress tensor
The state of stress at a point in the body is then defined by all the stress vectors associated with all planes (infinite in number) that pass through that point [2]. However, according to Cauchy’s fundamental theorem [4], also called Cauchy’s stress theorem [7], 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 , called the Cauchy stress tensor, independent of such that is a linear function of :
This equation implies that the stress vector at any point in a continuum associated with a plane with normal vector 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 of the stress tensor .
To prove this expression, consider a tetrahedron with three faces oriented in the coordinate planes, and with an infinitesimal area oriented in an arbitrary direction specified by a normal vector (Figure 2.2). The tetrahedron is formed by slicing the infinitesimal element along an arbitrary plane . The stress vector on this plane is denoted by . The stress vectors acting on the faces of the tetrahedron are denoted as , , and , and are by definition the components of the stress tensor . This tetrahedron is sometimes called the Cauchy tetrahedron. From equilibrium of forces, i.e. Euler’s first law of motion (Newton’s second law of motion), we have
![](http://upload.wikimedia.org/wikipedia/commons/thumb/e/eb/Cauchy_tetrahedron.svg/280px-Cauchy_tetrahedron.svg.png)
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 of the equation represents the product of the mass enclosed by the tetrahedron and its acceleration: is the density, is the acceleration, and is the height of the tetrahedron, considering the plane as the base. The area of the faces of the tetrahedron perpendicular to the axes can be found by projecting into each face (using the dot product):
and then can be substituted into the equation to cancel out :
To consider the limiting case as the tetrahedron shrinks to a point, must go to 0 (intuitively, plane is translated along towards ). As a result, the right-hand-side of the equation approaches 0, thus
![](http://upload.wikimedia.org/wikipedia/commons/thumb/b/b3/Components_stress_tensor_cartesian.svg/300px-Components_stress_tensor_cartesian.svg.png)
Assuming a material element (Figure 2.3) with planes perpendicular to the coordinate axes of a Cartesian coordinate system, the stress vectors associated with each of the element planes, i.e. , , and 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 -axis, the normal stress is denoted by , and the two shear stresses are denoted as and :
In index notation this is
The nine components of the stress vectors are the components of a second-order Cartesian tensor called the Cauchy stress tensor, which completely defines the state of stresses at a point and is given by
where
- , , and are normal stresses, and
- , , , , , and are shear stresses.
The first index indicates that the stress acts on a plane normal to the axis, and the second index denotes the direction in which the stress acts. 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.
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.
Thus, using the components of the stress tensor
or, equivalently,
Alternatively, in matrix form we have
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 system to an system, the components in the initial system are transformed into the components in the new system according to the tensor transformation rule (Figure 2.4):
where is the rotation matrix with components . In matrix form this is
![](http://upload.wikimedia.org/wikipedia/commons/thumb/7/76/Stress_transformation_3D.svg/600px-Stress_transformation_3D.svg.png)
Expanding the matrix operation, and simplifying some terms by taking advantage of the symmetry of the stress tensor, gives:
A graphical representation of this transformation of stresses, for a two-dimensional (plane stress and plane strain) and a general three-dimensional state of stresses, is the Mohr's circle for stresses
Normal and shear stresses
The magnitude of the normal stress component, , of any stress vector acting on an arbitrary plane with normal vector at a given point in terms of the component of the stress tensor is the dot product of the stress vector and the normal vector, thus
The magnitude of the shear stress component, , acting in the plane formed by the two vectors and , can then be found using the Pythagorean theorem, thus
where
Equilibrium equations and symmetry of the stress tensor
![](http://upload.wikimedia.org/wikipedia/commons/thumb/b/b7/Equilibrium_equation_body.png/200px-Equilibrium_equation_body.png)
When a body is in equilibrium the components of the stress tensor in every point of the body satisfy the equilibrium equations,
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.
Derivation of equilibrium equations Consider a continuum body (see Figure 4) occupying a volume , having a surface area , with defined traction or surface forces per unit area acting on every point of the body surface, and body forces per unit of volume on every point within the volume . Thus, if the body is in equilibrium the resultant force acting on the volume is zero, thus: By definition the stress vector is , then
Using the Gauss's divergence theorem to convert a surface integral to a volume integral gives
For an arbitrary volume the integral vanishes, and we have the equilibrium equations
At the same time, 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, i.e.
Derivation of symmetry of the stress tensor Summing moments about point O (Figure 4) the resultant moment is zero as the body is in equilibrium. Thus, where is the position vector and is expressed as
Knowing that and using Gauss's divergence theorem to change from a surface integral to a volume integral, we have
The second integral is zero as it contains the equilibrium equations. This leaves the first integral, where , therefore
For an arbitrary volume V, we then have
which is satisfied at every point within the body. Expanding this equation we have
- , , and
or in general
This proves that the stress tensor is symmetric
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
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 length of the vector is a physical quantity (a scalar) and is independent of the coordinate system chosen to represent the vector. 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 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 determinant matrix 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. not imaginary due to the symmetry of the stress tensor. The three roots , , and are the eigenvalues or principal stresses, and they are the roots of the Cayley–Hamilton theorem. The principal stresses are unique for a given stress tensor. Therefore, from the characteristic equation it is seen that the coefficients , and , called the first, second, and third stress invariants, respectively, have always the same value regardless of the orientation of the coordinate system chosen.
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 of the coordinate system.
If we choose a coordinate system with axes oriented to the principal directions, then the normal stresses will be the principal stresses and the stress tensor is represented by a diagonal matrix:
The principal stresses may 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, working and thinking in the principal coordinate system is often very 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.[15] 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 stress for plus and minus. This is shown as:
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 from the principal stress planes. The maximum shear stress is expressed as
Assuming then
The normal stress component acting on the plane for the maximum shear stress is non-zero and it is equal to
Derivation of the maximum and minimum shear stresses [2][16][4][17][18][19][20] The normal stress can be written in terms of principal stresses as Knowing that , the shear stress in terms of principal stresses components is expressed as
The maximum shear stress at a point in a continuum body is determined by maximizing subject to the condition that
This is a constrained maximization problem, which can be solved using the Lagrangian multiplier technique to convert the problem into an unconstrained optimization problem. Thus, the stationary values (maximum and minimum values)of occur where the gradient of is parallel to the gradient of .
The Lagrangian function for this problem can be written as
where is the Lagrangian multiplier (which is different from the use to denote eigenvalues).
The extreme values of these functions are
thence
These three equations together with the condition may be solved for and
By multiplying the first three equations by and , respectively, and knowing that we obtain
Adding these three equations we get
this result can be substituted into each of the first three equations to obtain
Doing the same for the other two equations we have
A first approach to solve these last three equations is to consider the trivial solution . However this options does not fulfill the constrain .
Considering the solution where and , it is determine from the condition that , then from the original equation for it is seen that . The other two possible values for can be obtained similarly by assuming
- and
- and
Thus, one set of solutions for these four equations is:
These correspond to minimum values for and verifies that there are no shear stresses on planes normal to the principal directions of stress, as shown previously.
A second set of solutions is obtained by assuming and . Thus we have
To find the values for and we first add these two equations
Knowing that for
and
we have
and solving for we have
Then solving for we have
and
The other two possible values for can be obtained similarly by assuming
- and
- and
Therefore the second set of solutions for , representing a maximum for is
Therefore, assuming , the maximum shear stress is expressed by
and it can be stated as being equal to one-half the difference between the largest and smallest principal stresses, acting on the plane that bisects the angle between the directions of the largest and smallest principal stresses.
Stress deviator tensor
The stress tensor can be expressed as the sum of two other stress tensors:
- a mean hydrostatic stress tensor oder volumetric stress tensor oder mean normal stress tensor, , which tends to change the volume of the stressed body; and
- a deviatoric component called the stress deviator tensor, , which tends to distort it.
where is the mean stress given by
The deviatoric stress tensor can be obtained by subtracting the hydrostatic stress tensor from the stress tensor:
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 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
![](http://upload.wikimedia.org/wikipedia/commons/thumb/9/9d/Octahedral_stress_planes.png/300px-Octahedral_stress_planes.png)
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.
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
Alternative measures of stress
The Cauchy stress tensor is not the only measure of stress that is used in practice. Other measures of stress include the first and second Piola-Kirchhoff stress tensors, the Biot stress tensor, and the Kirchhoff stress tensor.
Piola-Kirchhoff stress tensor
In the case of finite deformations, the Piola-Kirchhoff stress tensors are used to express the stress relative to the reference configuration. This is in contrast to the Cauchy stress tensor which expresses the stress relative to the present configuration. For infinitesimal deformations or rotations, the Cauchy and Piola-Kirchhoff tensors are identical. These tensors take their names from Gabrio Piola and Gustav Kirchhoff.
Whereas the Cauchy stress tensor, relates stresses in the current configuration, the deformation gradient and strain tensors are described by relating the motion to the reference configuration; thus not all tensors describing the state of the material are in either the reference or current configuration. Having the stress, strain and deformation all described either in the reference or current configuration would make it easier to define constitutive models (for example, the Cauchy Stress tensor is variant to a pure rotation, while the deformation strain tensor is invariant; thus creating problems in defining a constitutive model that relates a varying tensor, in terms of an invariant one during pure rotation; as by definition constitutive models have to be invariant to pure rotations). The 1st Piola-Kirchhoff stress tensor, is one possible solution to this problem. It defines a family of tensors, which describe the configuration of the body in either the current or the reference state.
The 1st Piola-Kirchhoff stress tensor, relates forces in the present configuration with areas in the reference ("material") configuration.
where is the deformation gradient and is the Jacobian determinant.
In terms of components with respect to an orthonormal basis, the first Piola-Kirchhoff stress is given by
Because it relates different coordinate systems, the 1st Piola-Kirchhoff stress is a two-point tensor. In general, it is not symmetric. The 1st Piola-Kirchhoff stress is the 3D generalization of the 1D concept of engineering stress.
If the material rotates without a change in stress state (rigid rotation), the components of the 1st Piola-Kirchhoff stress tensor will vary with material orientation.
The 1st Piola-Kirchhoff stress is energy conjugate to the deformation gradient.
2nd Piola-Kirchhoff stress tensor
Whereas the 1st Piola-Kirchhoff stress relates forces in the current configuration to areas in the reference configuration, the 2nd Piola-Kirchhoff stress tensor relates forces in the reference configuration to areas in the reference configuration. The force in the reference configuration is obtained via a mapping that preserves the relative relationship between the force direction and the area normal in the current configuration.
In index notation with respect to an orthonormal basis,
This tensor is symmetric.
If the material rotates without a change in stress state (rigid rotation), the components of the 2nd Piola-Kirchhoff stress tensor will remain constant, irrespective of material orientation.
The 2nd Piola-Kirchhoff stress tensor is energy conjugate to the Green-Lagrange finite strain tensor.
See also
References
- ^ Walter D. Pilkey, Orrin H. Pilkey (1974). Mechanics of solids. p. 292.
- ^ a b c d Chen
- ^ a b Mase
- ^ a b c d Atanackovic
- ^ Smith & Truesdell p.97
- ^ Slaughter
- ^ a b c Irgens
- ^ a b c Liu
- ^ a b Chadwick
- ^ Lubliner
- ^ Truesdell and Topin 1960
- ^ Fung
- ^ Basar
- ^ Hjelmstad
- ^ Hamrock
- ^ Wu
- ^ Chatterjee
- ^ Jaeger
- ^ Ameen
- ^ Prager
Bibliography
- Ameen, Mohammed (2005). Computational elasticity: theory of elasticity and finite and boundary element methods. Alpha Science Int'l Ltd. pp. 33–66. ISBN 184265201X.
- Atanackovic, Teodor M. (2000). Theory of elasticity for scientists and engineers. Springer. pp. 1–46. ISBN 081764072X.
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ignored (|author=
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- Chakrabarty, J. (2006). Theory of plasticity (3 ed.). Butterworth-Heinemann. pp. 17–32. ISBN 0750666382.
- Chatterjee, Rabindranath (1999). Mathematical Theory of Continuum Mechanics. Alpha Science Int'l Ltd. pp. 111–157. ISBN 8173192448.
- Chen, Wai-Fah (2007). Plasticity for structural engineers. J. Ross Publishing. pp. 46–71. ISBN 1932159754.
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: Unknown parameter|coauthors=
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suggested) (help) - Davis, R. O. (1996). Elasticity and geomechanics. Cambridge University Press. pp. 16–26. ISBN 0521498279.
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ignored (|author=
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- Fung, Yuan-cheng (2001). Classical and computational solid mechanics. Volume 1 of Advanced series in engineering science. World Scientific. pp. 66–96. ISBN 9810241240.
{{cite book}}
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ignored (|author=
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- Hjelmstad, Keith D. (2005). Fundamentals of structural mechanics. Prentice-Hall international series in civil engineering and engineering mechanics (2 ed.). Springer. pp. 103–130. ISBN 038723330X.
- Holtz, Robert D. (1981). An introduction to geotechnical engineering. Prentice-Hall civil engineering and engineering mechanics series. Prentice-Hall. ISBN 0134843940.
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ignored (|author=
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- Jaeger, John Conrad (2007). Fundamentals of rock mechanics (Fourth ed.). Wiley-Blackwell. pp. 9–41. ISBN 0632057599.
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ignored (|author=
suggested) (help) - Jones, Robert Millard (2008). Deformation Theory of Plasticity. Bull Ridge Corporation. pp. 95–112. ISBN 0978722310.
- Jumikis, Alfreds R. (1969). Theoretical soil mechanics: with practical applications to soil mechanics and foundation engineering. Van Nostrand Reinhold Co. ISBN 0442041993.
- Landau, L.D. and E.M.Lifshitz. (1959). Theory of Elasticity.
- Love, A. E. H. (4 ed.). (1944). Treatise on the Mathematical Theory of Elasticity. New York: Dover Publications. ISBN 0-486-60174-9.
- Liu, I-Shih (2002). Continuum mechanics. Springer. pp. 41–50. ISBN 3540430199.
- Lubliner, Jacob (2008). Plasticity Theory (Revised Edition) (PDF). Dover Publications. ISBN 0486462900.
- Marsden, J. E. (1994). Mathematical Foundations of Elasticity. Dover Publications. pp. 132–142. ISBN 0486678652.
{{cite book}}
: Unknown parameter|coauthors=
ignored (|author=
suggested) (help) - Mase, George E. (1970). Continuum Mechanics. McGraw-Hill. pp. 44–76. ISBN 0070406634.
- Mase, G. Thomas (1999). Continuum Mechanics for Engineers (Second ed.). CRC Press. pp. 47–102. ISBN 0-8493-1855-6.
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: Unknown parameter|coauthors=
ignored (|author=
suggested) (help) - Parry, Richard Hawley Grey (2004). Mohr circles, stress paths and geotechnics (2 ed.). Taylor & Francis. pp. 1–30. ISBN 0415272971.
- Prager, William (2004). Introduction to mechanics of continua. Dover Publications. pp. 43–61. ISBN 0486438090.
- Rees, David (2006). Basic Engineering Plasticity - An Introduction with Engineering and Manufacturing Applications. Butterworth-Heinemann. pp. 1–32. ISBN 0750680253.
- Smith, Donald Ray (1993). An introduction to continuum mechanics -after Truesdell and Noll. Springer. ISBN 0792324544.
{{cite book}}
: Unknown parameter|coauthors=
ignored (|author=
suggested) (help) - Timoshenko, Stephen P. (1970). Theory of Elasticity (Third ed.). McGraw-Hill International Editions. ISBN 0-07-085805-5.
{{cite book}}
: Unknown parameter|coauthors=
ignored (|author=
suggested) (help) - Timoshenko, Stephen P. (1983). History of strength of materials: with a brief account of the history of theory of elasticity and theory of structures. Dover Books on Physics. Dover Publications. ISBN 0486611876.
- Wu, Han-Chin (2005). Continuum mechanics and plasticity. CRC Press. pp. 45–78. ISBN 1584883634.