Template:Short description Template:Pp-semi-indef Template:More footnotes Template:Use dmy dates

File:Hookes-law-springs.png
Hooke's law: the force is proportional to the extension
File:Manometer anim 02.gif
Bourdon tubes are based on Hooke's law. The force created by gas pressure inside the coiled metal tube above unwinds it by an amount proportional to the pressure.
File:Balancier avec ressort spiral.png
The balance wheel at the core of many mechanical clocks and watches depends on Hooke's law. Since the torque generated by the coiled spring is proportional to the angle turned by the wheel, its oscillations have a nearly constant period.

Template:Continuum mechanics

In physics, Hooke's law is an empirical law which states that the force (Template:Mvar) needed to extend or compress a spring by some distance (Template:Mvar) scales linearly with respect to that distance—that is, Template:Nowrap where Template:Mvar is a constant factor characteristic of the spring (i.e., its stiffness), and Template:Mvar is small compared to the total possible deformation of the spring. The law is named after 17th-century British physicist Robert Hooke. He first stated the law in 1676 as a Latin anagram.<ref>The anagram was given in alphabetical order, ceiiinosssttuv, representing {{#invoke:Lang|lang}} – "As the extension, so the force": Template:Cite book</ref><ref>See http://civil.lindahall.org/design.shtml, where one can find also an anagram for catenary.</ref> He published the solution of his anagram in 1678<ref>Robert Hooke, De Potentia Restitutiva, or of Spring. Explaining the Power of Springing Bodies, London, 1678.</ref> as: {{#invoke:Lang|lang}} ("as the extension, so the force" or "the extension is proportional to the force"). Hooke states in the 1678 work that he was aware of the law since 1660.

Hooke's equation holds (to some extent) in many other situations where an elastic body is deformed, such as wind blowing on a tall building, and a musician plucking a string of a guitar. An elastic body or material for which this equation can be assumed is said to be linear-elastic or Hookean.

Hooke's law is only a first-order linear approximation to the real response of springs and other elastic bodies to applied forces. It must eventually fail once the forces exceed some limit, since no material can be compressed beyond a certain minimum size, or stretched beyond a maximum size, without some permanent deformation or change of state. Many materials will noticeably deviate from Hooke's law well before those elastic limits are reached.

On the other hand, Hooke's law is an accurate approximation for most solid bodies, as long as the forces and deformations are small enough. For this reason, Hooke's law is extensively used in all branches of science and engineering, and is the foundation of many disciplines such as seismology, molecular mechanics and acoustics. It is also the fundamental principle behind the spring scale, the manometer, the galvanometer, and the balance wheel of the mechanical clock.

The modern theory of elasticity generalizes Hooke's law to say that the strain (deformation) of an elastic object or material is proportional to the stress applied to it. However, since general stresses and strains may have multiple independent components, the "proportionality factor" may no longer be just a single real number, but rather a linear map (a tensor) that can be represented by a matrix of real numbers.

In this general form, Hooke's law makes it possible to deduce the relation between strain and stress for complex objects in terms of intrinsic properties of the materials they are made of. For example, one can deduce that a homogeneous rod with uniform cross section will behave like a simple spring when stretched, with a stiffness Template:Mvar directly proportional to its cross-section area and inversely proportional to its length.

Formal definitionEdit

Linear springsEdit

File:Spring-elongation-and-forces.svg
Elongation and compression of a spring

Consider a simple helical spring that has one end attached to some fixed object, while the free end is being pulled by a force whose magnitude is Template:Mvar. Suppose that the spring has reached a state of equilibrium, where its length is not changing anymore. Let Template:Mvar be the amount by which the free end of the spring was displaced from its "relaxed" position (when it is not being stretched). Hooke's law states that <math display="block" qid=Q170282>F_s = kx</math> or, equivalently, <math display="block">x = \frac{F_s}{k}</math> where Template:Mvar is a positive real number, characteristic of the spring. A spring with spaces between the coils can be compressed, and the same formula holds for compression, with Template:Mvar and Template:Mvar both negative in that case.<ref>Template:Cite book</ref>

File:Hooke's Law wikipedia.png
Graphical derivation

According to this formula, the graph of the applied force Template:Mvar as a function of the displacement Template:Mvar will be a straight line passing through the origin, whose slope is Template:Mvar.

Hooke's law for a spring is also stated under the convention that Template:Mvar is the restoring force exerted by the spring on whatever is pulling its free end. In that case, the equation becomes <math display="block">F_s = -kx</math> since the direction of the restoring force is opposite to that of the displacement.

Torsional springsEdit

The torsional analog of Hooke's law applies to torsional springs. It states that the torque (τ) required to rotate an object is directly proportional to the angular displacement (θ) from the equilibrium position. It describes the relationship between the torque applied to an object and the resulting angular deformation due to torsion. Mathematically, it can be expressed as:

<math>\tau = -k\theta</math>

Where:

  • τ is the torque measured in Newton-meters or N·m.
  • k is the torsional constant (measured in N·m/radian), which characterizes the stiffness of the torsional spring or the resistance to angular displacement.
  • θ is the angular displacement (measured in radians) from the equilibrium position.

Just as in the linear case, this law shows that the torque is proportional to the angular displacement, and the negative sign indicates that the torque acts in a direction opposite to the angular displacement, providing a restoring force to bring the system back to equilibrium.

General "scalar" springsEdit

Hooke's spring law usually applies to any elastic object, of arbitrary complexity, as long as both the deformation and the stress can be expressed by a single number that can be both positive and negative.

For example, when a block of rubber attached to two parallel plates is deformed by shearing, rather than stretching or compression, the shearing force Template:Math and the sideways displacement of the plates Template:Mvar obey Hooke's law (for small enough deformations).

Hooke's law also applies when a straight steel bar or concrete beam (like the one used in buildings), supported at both ends, is bent by a weight Template:Mvar placed at some intermediate point. The displacement Template:Mvar in this case is the deviation of the beam, measured in the transversal direction, relative to its unloaded shape.

Vector formulationEdit

In the case of a helical spring that is stretched or compressed along its axis, the applied (or restoring) force and the resulting elongation or compression have the same direction (which is the direction of said axis). Therefore, if Template:Mvar and Template:Mvar are defined as vectors, Hooke's equation still holds and says that the force vector is the elongation vector multiplied by a fixed scalar.

General tensor formEdit

Some elastic bodies will deform in one direction when subjected to a force with a different direction. One example is a horizontal wood beam with non-square rectangular cross section that is bent by a transverse load that is neither vertical nor horizontal. In such cases, the magnitude of the displacement Template:Mvar will be proportional to the magnitude of the force Template:Mvar, as long as the direction of the latter remains the same (and its value is not too large); so the scalar version of Hooke's law Template:Math will hold. However, the force and displacement vectors will not be scalar multiples of each other, since they have different directions. Moreover, the ratio Template:Mvar between their magnitudes will depend on the direction of the vector Template:Mvar.

Yet, in such cases there is often a fixed linear relation between the force and deformation vectors, as long as they are small enough. Namely, there is a function Template:Mvar from vectors to vectors, such that Template:Math, and Template:Math for any real numbers Template:Mvar, Template:Mvar and any displacement vectors Template:Math, Template:Math. Such a function is called a (second-order) tensor.

With respect to an arbitrary Cartesian coordinate system, the force and displacement vectors can be represented by 3 × 1 matrices of real numbers. Then the tensor Template:Math connecting them can be represented by a 3 × 3 matrix Template:Mvar of real coefficients, that, when multiplied by the displacement vector, gives the force vector:

<math display="block"> \mathbf{F} \,=\,

\begin{bmatrix} F_1\\ F_2 \\ F_3 \end{bmatrix} \,=\,
\begin{bmatrix} 
\kappa_{11}& \kappa_{12}& \kappa_{13}\\ 
\kappa_{21}& \kappa_{22}& \kappa_{23}\\ 
\kappa_{31}& \kappa_{32}& \kappa_{33}
\end{bmatrix}
\begin{bmatrix} X_1\\ X_2 \\ X_3 \end{bmatrix}
\,=\, \boldsymbol{\kappa} \mathbf{X}</math>

That is, <math display="block">F_i = \kappa_{i1} X_1 + \kappa_{i2} X_2 + \kappa_{i3} X_3</math> for Template:Math. Therefore, Hooke's law Template:Math can be said to hold also when Template:Math and Template:Math are vectors with variable directions, except that the stiffness of the object is a tensor Template:Mvar, rather than a single real number Template:Mvar.

Hooke's law for continuous mediaEdit

{{#invoke:Labelled list hatnote|labelledList|Main article|Main articles|Main page|Main pages}}

File:Hookes law nanoscale.jpg
(a) Schematic of a polymer nanospring. The coil radius, R, pitch, P, length of the spring, L, and the number of turns, N, are 2.5 μm, 2.0 μm, 13 μm, and 4, respectively. Electron micrographs of the nanospring, before loading (b-e), stretched (f), compressed (g), bent (h), and recovered (i). All scale bars are 2 μm. The spring followed a linear response against applied force, demonstrating the validity of Hooke's law at the nanoscale.<ref>Template:Cite journal</ref>

The stresses and strains of the material inside a continuous elastic material (such as a block of rubber, the wall of a boiler, or a steel bar) are connected by a linear relationship that is mathematically similar to Hooke's spring law, and is often referred to by that name.

However, the strain state in a solid medium around some point cannot be described by a single vector. The same parcel of material, no matter how small, can be compressed, stretched, and sheared at the same time, along different directions. Likewise, the stresses in that parcel can be at once pushing, pulling, and shearing.

In order to capture this complexity, the relevant state of the medium around a point must be represented by two-second-order tensors, the strain tensor Template:Math (in lieu of the displacement Template:Math) and the stress tensor Template:Math (replacing the restoring force Template:Math). The analogue of Hooke's spring law for continuous media is then <math display="block"> \boldsymbol{\sigma} = \mathbf{c} \boldsymbol{\varepsilon},</math> where Template:Math is a fourth-order tensor (that is, a linear map between second-order tensors) usually called the stiffness tensor or elasticity tensor. One may also write it as <math display="block"> \boldsymbol{\varepsilon} = \mathbf{s} \boldsymbol{\sigma},</math> where the tensor Template:Math, called the compliance tensor, represents the inverse of said linear map.

In a Cartesian coordinate system, the stress and strain tensors can be represented by 3 × 3 matrices

<math display="block"> \boldsymbol{\varepsilon} \,=\, \begin{bmatrix} \varepsilon_{11} & \varepsilon_{12} & \varepsilon_{13}\\ \varepsilon_{21} & \varepsilon_{22} & \varepsilon_{23}\\ \varepsilon_{31} & \varepsilon_{32} & \varepsilon_{33} \end{bmatrix} \,;\qquad \boldsymbol{\sigma} \,=\, \begin{bmatrix} \sigma_{11} & \sigma_{12} & \sigma_{13} \\ \sigma_{21} & \sigma_{22} & \sigma_{23} \\ \sigma_{31} & \sigma_{32} & \sigma_{33} \end{bmatrix}</math>

Being a linear mapping between the nine numbers Template:Math and the nine numbers Template:Math, the stiffness tensor Template:Math is represented by a matrix of Template:Math real numbers Template:Math. Hooke's law then says that <math display="block">\sigma_{ij} = \sum_{k=1}^3 \sum_{l=1}^3 c_{ijkl} \varepsilon_{kl}</math> where Template:Math.

All three tensors generally vary from point to point inside the medium, and may vary with time as well. The strain tensor Template:Math merely specifies the displacement of the medium particles in the neighborhood of the point, while the stress tensor Template:Math specifies the forces that neighboring parcels of the medium are exerting on each other. Therefore, they are independent of the composition and physical state of the material. The stiffness tensor Template:Math, on the other hand, is a property of the material, and often depends on physical state variables such as temperature, pressure, and microstructure.

Due to the inherent symmetries of Template:Math, Template:Math, and Template:Math, only 21 elastic coefficients of the latter are independent.<ref>Template:Cite journal</ref> This number can be further reduced by the symmetry of the material: 9 for an orthorhombic crystal, 5 for an hexagonal structure, and 3 for a cubic symmetry.<ref>Template:Cite journal</ref> For isotropic media (which have the same physical properties in any direction), Template:Math can be reduced to only two independent numbers, the bulk modulus Template:Mvar and the shear modulus Template:Mvar, that quantify the material's resistance to changes in volume and to shearing deformations, respectively.

Analogous lawsEdit

Since Hooke's law is a simple proportionality between two quantities, its formulas and consequences are mathematically similar to those of many other physical laws, such as those describing the motion of fluids, or the polarization of a dielectric by an electric field.

In particular, the tensor equation Template:Math relating elastic stresses to strains is entirely similar to the equation Template:Math relating the viscous stress tensor Template:Math and the strain rate tensor Template:Math in flows of viscous fluids; although the former pertains to static stresses (related to amount of deformation) while the latter pertains to dynamical stresses (related to the rate of deformation).

Units of measurementEdit

In SI units, displacements are measured in meters (m), and forces in newtons (N or kg·m/s2). Therefore, the spring constant Template:Mvar, and each element of the tensor Template:Math, is measured in newtons per meter (N/m), or kilograms per second squared (kg/s2).

For continuous media, each element of the stress tensor Template:Math is a force divided by an area; it is therefore measured in units of pressure, namely pascals (Pa, or N/m2, or kg/(m·s2). The elements of the strain tensor Template:Math are dimensionless (displacements divided by distances). Therefore, the entries of Template:Mvar are also expressed in units of pressure.

General application to elastic materialsEdit

Objects that quickly regain their original shape after being deformed by a force, with the molecules or atoms of their material returning to the initial state of stable equilibrium, often obey Hooke's law.

Hooke's law only holds for some materials under certain loading conditions. Steel exhibits linear-elastic behavior in most engineering applications; Hooke's law is valid for it throughout its elastic range (i.e., for stresses below the yield strength). For some other materials, such as aluminium, Hooke's law is only valid for a portion of the elastic range. For these materials a proportional limit stress is defined, below which the errors associated with the linear approximation are negligible.

Rubber is generally regarded as a "non-Hookean" material because its elasticity is stress dependent and sensitive to temperature and loading rate.

Generalizations of Hooke's law for the case of large deformations is provided by models of neo-Hookean solids and Mooney–Rivlin solids.

Derived formulaeEdit

Tensional stress of a uniform barEdit

A rod of any elastic material may be viewed as a linear spring. The rod has length Template:Mvar and cross-sectional area Template:Mvar. Its tensile stress Template:Mvar is linearly proportional to its fractional extension or strain Template:Mvar by the modulus of elasticity Template:Mvar: <math display="block">\sigma = E \varepsilon.</math>

The modulus of elasticity may often be considered constant. In turn, <math display="block">\varepsilon = \frac{\Delta L}{L}</math> (that is, the fractional change in length), and since <math display="block">\sigma = \frac{F}{A} \,,</math> it follows that:

<math display="block"> \varepsilon = \frac{\sigma}{E} = \frac{F}{A E}\,.</math>

The change in length may be expressed as

<math display="block">\Delta L = \varepsilon L = \frac{F L}{A E}\,.</math>

Spring energyEdit

The potential energy Template:Math stored in a spring is given by <math display="block">U_\mathrm{el}(x) = \tfrac 1 2 kx^2</math> which comes from adding up the energy it takes to incrementally compress the spring. That is, the integral of force over displacement. Since the external force has the same general direction as the displacement, the potential energy of a spring is always non-negative. Substituting <math>x=F/k</math> gives <math display="block">U_\mathrm{el}(F) = \frac{F^2}{2 k}.</math>

This potential Template:Math can be visualized as a parabola on the Template:Mvar-plane such that Template:Math. As the spring is stretched in the positive Template:Mvar-direction, the potential energy increases parabolically (the same thing happens as the spring is compressed). Since the change in potential energy changes at a constant rate: <math display="block"> \frac{d^2 U_\mathrm{el}}{dx^2}=k\,.</math> Note that the change in the change in Template:Mvar is constant even when the displacement and acceleration are zero.

Relaxed force constants (generalized compliance constants)Edit

Relaxed force constants (the inverse of generalized compliance constants) are uniquely defined for molecular systems, in contradistinction to the usual "rigid" force constants, and thus their use allows meaningful correlations to be made between force fields calculated for reactants, transition states, and products of a chemical reaction. Just as the potential energy can be written as a quadratic form in the internal coordinates, so it can also be written in terms of generalized forces. The resulting coefficients are termed compliance constants. A direct method exists for calculating the compliance constant for any internal coordinate of a molecule, without the need to do the normal mode analysis.<ref>Template:Cite journal</ref> The suitability of relaxed force constants (inverse compliance constants) as covalent bond strength descriptors was demonstrated as early as 1980. Recently, the suitability as non-covalent bond strength descriptors was demonstrated too.<ref>Template:Cite journal</ref>

Harmonic oscillatorEdit

Template:See also

File:Mass-spring-system.png
A mass suspended by a spring is the classical example of a harmonic oscillator

A mass Template:Mvar attached to the end of a spring is a classic example of a harmonic oscillator. By pulling slightly on the mass and then releasing it, the system will be set in sinusoidal oscillating motion about the equilibrium position. To the extent that the spring obeys Hooke's law, and that one can neglect friction and the mass of the spring, the amplitude of the oscillation will remain constant; and its frequency Template:Mvar will be independent of its amplitude, determined only by the mass and the stiffness of the spring: <math display="block">f = \frac{1}{2 \pi} \sqrt\frac{k}{m}</math> This phenomenon made possible the construction of accurate mechanical clocks and watches that could be carried on ships and people's pockets.

Rotation in gravity-free spaceEdit

If the mass Template:Mvar were attached to a spring with force constant Template:Mvar and rotating in free space, the spring tension (Template:Math) would supply the required centripetal force (Template:Math):

<math display="block">F_\mathrm{t} = kx\,; \qquad F_\mathrm{c} = m \omega^2 r</math> Since Template:Math and Template:Math, then: <math display="block">k = m \omega^2</math> Given that Template:Math, this leads to the same frequency equation as above: <math display="block">f = \frac{1}{2 \pi} \sqrt\frac{k}{m}</math>

Linear elasticity theory for continuous mediaEdit

Template:See also Template:Einstein summation convention

Isotropic materialsEdit

Template:For

Isotropic materials are characterized by properties which are independent of direction in space. Physical equations involving isotropic materials must therefore be independent of the coordinate system chosen to represent them. The strain tensor is a symmetric tensor. Since the trace of any tensor is independent of any coordinate system, the most complete coordinate-free decomposition of a symmetric tensor is to represent it as the sum of a constant tensor and a traceless symmetric tensor.<ref>Template:Cite book</ref> Thus in index notation:

<math display="block"> \varepsilon_{ij} = \left(\tfrac13\varepsilon_{kk}\delta_{ij}\right) + \left(\varepsilon_{ij}-\tfrac13\varepsilon_{kk}\delta_{ij}\right)</math> where Template:Mvar is the Kronecker delta. In direct tensor notation: <math display="block">

\boldsymbol{\varepsilon} = \operatorname{vol}(\boldsymbol{\varepsilon}) +
\operatorname{dev}(\boldsymbol{\varepsilon}) \,; \qquad
\operatorname{vol}(\boldsymbol{\varepsilon}) = \tfrac13\operatorname{tr}(\boldsymbol{\varepsilon})~\mathbf{I} \,; \qquad
\operatorname{dev}(\boldsymbol{\varepsilon}) = \boldsymbol{\varepsilon} - \operatorname{vol}(\boldsymbol{\varepsilon})
</math>

where Template:Math is the second-order identity tensor.

The first term on the right is the constant tensor, also known as the volumetric strain tensor, and the second term is the traceless symmetric tensor, also known as the deviatoric strain tensor or shear tensor.

The most general form of Hooke's law for isotropic materials may now be written as a linear combination of these two tensors:

<math display="block"> \sigma_{ij}=3K\left(\tfrac{1}{3}\varepsilon_{kk}\delta_{ij}\right)

+2G\left(\varepsilon_{ij}-\tfrac{1}{3}\varepsilon_{kk}\delta_{ij}\right)\,; \qquad
\boldsymbol{\sigma} = 3K\operatorname{vol}(\boldsymbol{\varepsilon}) + 2G\operatorname{dev}(\boldsymbol{\varepsilon})</math>

where Template:Mvar is the bulk modulus and Template:Mvar is the shear modulus.

Using the relationships between the elastic moduli, these equations may also be expressed in various other ways. A common form of Hooke's law for isotropic materials, expressed in direct tensor notation, is <ref name=Simo98>Template:Cite book</ref>

<math> \boldsymbol{\sigma} = \lambda\operatorname{tr}(\boldsymbol{\varepsilon})\mathbf{I} + 2\mu\boldsymbol{\varepsilon}

= \mathsf{c}:\boldsymbol{\varepsilon} \,; \qquad \mathsf{c} = \lambda\mathbf{I}\otimes\mathbf{I} + 2\mu\mathsf{I} </math>

where Template:Math and Template:Math are the Lamé constants, Template:Math is the second-rank identity tensor, and I is the symmetric part of the fourth-rank identity tensor. In index notation: <math display="block"> \sigma_{ij} = \lambda\varepsilon_{kk}~\delta_{ij} + 2\mu\varepsilon_{ij} = c_{ijkl}\varepsilon_{kl} \,;\qquad c_{ijkl} = \lambda\delta_{ij}\delta_{kl} + \mu\left(\delta_{ik}\delta_{jl} + \delta_{il}\delta_{jk}\right) </math>

The inverse relationship is<ref name=Milton02>Template:Cite book</ref>

<math display="block"> \boldsymbol{\varepsilon} = \frac{1}{2\mu}\boldsymbol{\sigma} - \frac{\lambda}{2\mu(3\lambda+2\mu)}\operatorname{tr}(\boldsymbol{\sigma})\mathbf{I} = \frac{1}{2G} \boldsymbol{\sigma} + \left(\frac{1}{9K} - \frac{1}{6G}\right)\operatorname{tr}(\boldsymbol{\sigma})\mathbf{I} </math>

Therefore, the compliance tensor in the relation Template:Math is

<math display="block"> \mathsf{s} = - \frac{\lambda}{2\mu(3\lambda+2\mu)}\mathbf{I}\otimes\mathbf{I} + \frac{1}{2\mu}\mathsf{I}

= \left(\frac{1}{9K} - \frac{1}{6G}\right)\mathbf{I}\otimes\mathbf{I} + \frac{1}{2G}\mathsf{I} </math>

In terms of Young's modulus and Poisson's ratio, Hooke's law for isotropic materials can then be expressed as

<math display="block"> \varepsilon_{ij}=\frac{1}{E}\big(\sigma_{ij}-\nu(\sigma_{kk}\delta_{ij}-\sigma_{ij})\big) \,; \qquad

\boldsymbol{\varepsilon} = \frac{1}{E} \big(\boldsymbol{\sigma} - \nu(\operatorname{tr}(\boldsymbol{\sigma})\mathbf{I} - \boldsymbol{\sigma})\big) = \frac{1+\nu}{E}\boldsymbol{\sigma} - \frac{\nu}{E}\operatorname{tr}(\boldsymbol{\sigma})\mathbf{I} </math>

This is the form in which the strain is expressed in terms of the stress tensor in engineering. The expression in expanded form is <math display="block"> \begin{align}

\varepsilon_{11} & = \frac{1}{E} \big(\sigma_{11} - \nu(\sigma_{22}+\sigma_{33}) \big) \\
\varepsilon_{22} & = \frac{1}{E} \big(\sigma_{22} - \nu(\sigma_{11}+\sigma_{33}) \big) \\
\varepsilon_{33} & = \frac{1}{E} \big(\sigma_{33} - \nu(\sigma_{11}+\sigma_{22}) \big) \\
\varepsilon_{12} & = \frac{1}{2G} \sigma_{12} \,;\qquad
\varepsilon_{13} = \frac{1}{2G}\sigma_{13} \,;\qquad
\varepsilon_{23} = \frac{1}{2G}\sigma_{23}
\end{align}</math>

where Template:Mvar is Young's modulus and Template:Mvar is Poisson's ratio. (See 3-D elasticity).

Template:Math proof In matrix form, Hooke's law for isotropic materials can be written as <math display="block">

\begin{bmatrix}\varepsilon_{11} \\ \varepsilon_{22} \\ \varepsilon_{33} \\ 2\varepsilon_{23} \\ 2\varepsilon_{13} \\ 2\varepsilon_{12} \end{bmatrix} \,=\, 
\begin{bmatrix}\varepsilon_{11} \\ \varepsilon_{22} \\ \varepsilon_{33} \\ \gamma_{23} \\ \gamma_{13} \\ \gamma_{12} \end{bmatrix} \,=\, 
\frac{1}{E}
\begin{bmatrix} 1 & -\nu & -\nu & 0 & 0 & 0 \\
-\nu & 1 & -\nu & 0 & 0 & 0 \\
-\nu & -\nu & 1 & 0 & 0 & 0 \\
0 & 0 & 0 & 2+2\nu & 0 & 0 \\
0 & 0 & 0 & 0 & 2+2\nu & 0 \\
0 & 0 & 0 & 0 & 0 & 2+2\nu \end{bmatrix}
\begin{bmatrix}\sigma_{11} \\ \sigma_{22} \\ \sigma_{33} \\ \sigma_{23} \\ \sigma_{13} \\ \sigma_{12} \end{bmatrix}
</math>

where Template:Math is the engineering shear strain. The inverse relation may be written as <math display="block">

\begin{bmatrix}\sigma_{11} \\ \sigma_{22} \\ \sigma_{33} \\ \sigma_{23} \\ \sigma_{13} \\ \sigma_{12} \end{bmatrix}
\,=\, \frac{E}{(1+\nu)(1-2\nu)}
\begin{bmatrix} 1-\nu & \nu & \nu & 0 & 0 & 0 \\
\nu & 1-\nu & \nu & 0 & 0 & 0 \\
\nu & \nu & 1-\nu & 0 & 0 & 0 \\
0 & 0 & 0 & \frac{1-2\nu}{2} & 0 & 0 \\
0 & 0 & 0 & 0 & \frac{1-2\nu}{2} & 0 \\
0 & 0 & 0 & 0 & 0 & \frac{1-2\nu}{2} \end{bmatrix}
\begin{bmatrix}\varepsilon_{11} \\ \varepsilon_{22} \\ \varepsilon_{33} \\ 2\varepsilon_{23} \\ 2\varepsilon_{13} \\ 2\varepsilon_{12} \end{bmatrix}

</math> which can be simplified thanks to the Lamé constants: <math display="block">

\begin{bmatrix}\sigma_{11} \\ \sigma_{22} \\ \sigma_{33} \\ \sigma_{23} \\ \sigma_{13} \\ \sigma_{12} \end{bmatrix}
\,=\, 
\begin{bmatrix} 2\mu+\lambda & \lambda & \lambda & 0 & 0 & 0 \\
\lambda & 2\mu+\lambda & \lambda & 0 & 0 & 0 \\
\lambda & \lambda & 2\mu+\lambda & 0 & 0 & 0 \\
0 & 0 & 0 & \mu & 0 & 0 \\
0 & 0 & 0 & 0 & \mu & 0 \\
0 & 0 & 0 & 0 & 0 & \mu \end{bmatrix}
\begin{bmatrix} \varepsilon_{11} \\ \varepsilon_{22} \\ \varepsilon_{33} \\ 2\varepsilon_{23} \\ 2\varepsilon_{13} \\ 2\varepsilon_{12} \end{bmatrix}

</math> In vector notation this becomes <math display="block"> \begin{bmatrix} \sigma_{11} & \sigma_{12} & \sigma_{13} \\

\sigma_{12} & \sigma_{22} & \sigma_{23} \\ \sigma_{13} & \sigma_{23} & \sigma_{33} \end{bmatrix}
\,=\, 2\mu \begin{bmatrix} \varepsilon_{11} & \varepsilon_{12} & \varepsilon_{13} \\ 
\varepsilon_{12} & \varepsilon_{22} & \varepsilon_{23} \\ \varepsilon_{13} & \varepsilon_{23} & \varepsilon_{33} \end{bmatrix} + \lambda \mathbf{I}\left(\varepsilon_{11} + \varepsilon_{22} + \varepsilon_{33} \right)</math>

where Template:Math is the identity tensor.

Plane stressEdit

Under plane stress conditions, Template:Math. In that case Hooke's law takes the form <math display="block">

\begin{bmatrix}\sigma_{11} \\ \sigma_{22} \\ \sigma_{12} \end{bmatrix}
\,=\, \frac{E}{1-\nu^2}
\begin{bmatrix} 1 & \nu & 0 \\
\nu & 1 & 0 \\
0 & 0 & \frac{1-\nu}{2} \end{bmatrix}
\begin{bmatrix}\varepsilon_{11} \\ \varepsilon_{22} \\ 2\varepsilon_{12} \end{bmatrix}
</math>

In vector notation this becomes <math display="block"> \begin{bmatrix} \sigma_{11} & \sigma_{12} \\

\sigma_{12} & \sigma_{22} \end{bmatrix}
\,=\, \frac{E}{1-\nu^2} \left((1-\nu) \begin{bmatrix} \varepsilon_{11} & \varepsilon_{12} \\ 
\varepsilon_{12} & \varepsilon_{22} \end{bmatrix} + \nu \mathbf{I} \left(\varepsilon_{11} + \varepsilon_{22} \right) \right)</math>

The inverse relation is usually written in the reduced form <math display="block">

\begin{bmatrix}\varepsilon_{11} \\ \varepsilon_{22} \\ 2\varepsilon_{12} \end{bmatrix} \,=\, \frac{1}{E}
\begin{bmatrix} 1 & -\nu & 0 \\
-\nu & 1 & 0 \\
0 & 0 & 2+2\nu \end{bmatrix}
\begin{bmatrix}\sigma_{11} \\ \sigma_{22} \\ \sigma_{12} \end{bmatrix}
</math>

Plane strainEdit

Under plane strain conditions, Template:Math. In this case Hooke's law takes the form <math display="block">

\begin{bmatrix}\sigma_{11} \\ \sigma_{22} \\ \sigma_{12} \end{bmatrix}
\,=\, \frac{E}{(1 + \nu)(1 - 2\nu)}
\begin{bmatrix} 1 - \nu & \nu & 0 \\
\nu & 1 - \nu & 0 \\
0 & 0 & \frac{1 - 2\nu}{2} \end{bmatrix}
\begin{bmatrix}\varepsilon_{11} \\ \varepsilon_{22} \\ 2\varepsilon_{12} \end{bmatrix}
</math>

Anisotropic materialsEdit

The symmetry of the Cauchy stress tensor (Template:Math) and the generalized Hooke's laws (Template:Math) implies that Template:Math. Similarly, the symmetry of the infinitesimal strain tensor implies that Template:Math. These symmetries are called the minor symmetries of the stiffness tensor c. This reduces the number of elastic constants from 81 to 36.

If in addition, since the displacement gradient and the Cauchy stress are work conjugate, the stress–strain relation can be derived from a strain energy density functional (Template:Mvar), then <math display="block"> \sigma_{ij} = \frac{\partial U}{\partial \varepsilon_{ij}} \quad \implies \quad c_{ijkl} = \frac{\partial^2 U}{\partial \varepsilon_{ij}\partial \varepsilon_{kl}}\,. </math> The arbitrariness of the order of differentiation implies that Template:Math. These are called the major symmetries of the stiffness tensor. This reduces the number of elastic constants from 36 to 21. The major and minor symmetries indicate that the stiffness tensor has only 21 independent components.

Matrix representation (stiffness tensor)Edit

It is often useful to express the anisotropic form of Hooke's law in matrix notation, also called Voigt notation. To do this we take advantage of the symmetry of the stress and strain tensors and express them as six-dimensional vectors in an orthonormal coordinate system (Template:Math) as <math display="block">

[\boldsymbol{\sigma}] \,=\, \begin{bmatrix}\sigma_{11}\\ \sigma_{22} \\ \sigma_{33} \\ \sigma_{23} \\ \sigma_{13} \\ \sigma_{12} \end{bmatrix} \,\equiv\,

\begin{bmatrix} \sigma_1 \\ \sigma_2 \\ \sigma_3 \\ \sigma_4 \\ \sigma_5 \\ \sigma_6 \end{bmatrix} \,;\qquad [\boldsymbol{\varepsilon}] \,=\, \begin{bmatrix}\varepsilon_{11}\\ \varepsilon_{22} \\ \varepsilon_{33} \\ 2\varepsilon_{23} \\ 2\varepsilon_{13} \\ 2\varepsilon_{12} \end{bmatrix} \,\equiv\, \begin{bmatrix} \varepsilon_1 \\ \varepsilon_2 \\ \varepsilon_3 \\ \varepsilon_4 \\ \varepsilon_5 \\ \varepsilon_6 \end{bmatrix}

</math>

Then the stiffness tensor (c) can be expressed as <math display="block">

[\mathsf{c}] \,=\, \begin{bmatrix} c_{1111} & c_{1122} & c_{1133} & c_{1123} & c_{1131} & c_{1112} \\
c_{2211} & c_{2222} & c_{2233} & c_{2223} & c_{2231} & c_{2212} \\

c_{3311} & c_{3322} & c_{3333} & c_{3323} & c_{3331} & c_{3312} \\ c_{2311} & c_{2322} & c_{2333} & c_{2323} & c_{2331} & c_{2312} \\ c_{3111} & c_{3122} & c_{3133} & c_{3123} & c_{3131} & c_{3112} \\ c_{1211} & c_{1222} & c_{1233} & c_{1223} & c_{1231} & c_{1212}

\end{bmatrix} \,\equiv\, \begin{bmatrix}
C_{11} & C_{12} & C_{13} & C_{14} & C_{15} & C_{16} \\

C_{12} & C_{22} & C_{23} & C_{24} & C_{25} & C_{26} \\ C_{13} & C_{23} & C_{33} & C_{34} & C_{35} & C_{36} \\ C_{14} & C_{24} & C_{34} & C_{44} & C_{45} & C_{46} \\ C_{15} & C_{25} & C_{35} & C_{45} & C_{55} & C_{56} \\ C_{16} & C_{26} & C_{36} & C_{46} & C_{56} & C_{66} \end{bmatrix}

</math>

and Hooke's law is written as

<math display="block"> [\boldsymbol{\sigma}] = [\mathsf{C}][\boldsymbol{\varepsilon}] \qquad \text{or} \qquad \sigma_i = C_{ij} \varepsilon_j \,. </math> Similarly the compliance tensor (s) can be written as <math display="block">

[\mathsf{s}] \,=\, \begin{bmatrix}

s_{1111} & s_{1122} & s_{1133} & 2s_{1123} & 2s_{1131} & 2s_{1112} \\ s_{2211} & s_{2222} & s_{2233} & 2s_{2223} & 2s_{2231} & 2s_{2212} \\ s_{3311} & s_{3322} & s_{3333} & 2s_{3323} & 2s_{3331} & 2s_{3312} \\ 2s_{2311} & 2s_{2322} & 2s_{2333} & 4s_{2323} & 4s_{2331} & 4s_{2312} \\ 2s_{3111} & 2s_{3122} & 2s_{3133} & 4s_{3123} & 4s_{3131} & 4s_{3112} \\ 2s_{1211} & 2s_{1222} & 2s_{1233} & 4s_{1223} & 4s_{1231} & 4s_{1212}

\end{bmatrix} \,\equiv\, \begin{bmatrix}

S_{11} & S_{12} & S_{13} & S_{14} & S_{15} & S_{16} \\ S_{12} & S_{22} & S_{23} & S_{24} & S_{25} & S_{26} \\ S_{13} & S_{23} & S_{33} & S_{34} & S_{35} & S_{36} \\ S_{14} & S_{24} & S_{34} & S_{44} & S_{45} & S_{46} \\ S_{15} & S_{25} & S_{35} & S_{45} & S_{55} & S_{56} \\ S_{16} & S_{26} & S_{36} & S_{46} & S_{56} & S_{66} \end{bmatrix}

</math>

Change of coordinate systemEdit

If a linear elastic material is rotated from a reference configuration to another, then the material is symmetric with respect to the rotation if the components of the stiffness tensor in the rotated configuration are related to the components in the reference configuration by the relation<ref name=Slaughter>Template:Cite book</ref>

<math display="block"> c_{pqrs} = l_{pi}l_{qj}l_{rk}l_{sl}c_{ijkl} </math> where Template:Mvar are the components of an orthogonal rotation matrix Template:Math. The same relation also holds for inversions.

In matrix notation, if the transformed basis (rotated or inverted) is related to the reference basis by

<math display="block"> [\mathbf{e}_i'] = [L][\mathbf{e}_i] </math>

then

<math display="block"> C_{ij}\varepsilon_i\varepsilon_j = C_{ij}'\varepsilon'_i\varepsilon'_j \,. </math> In addition, if the material is symmetric with respect to the transformation Template:Math then <math display="block"> C_{ij} = C'_{ij} \quad \implies \quad C_{ij}(\varepsilon_i\varepsilon_j - \varepsilon'_i\varepsilon'_j) = 0 \,. </math>

Orthotropic materialsEdit

{{#invoke:Labelled list hatnote|labelledList|Main article|Main articles|Main page|Main pages}}

Orthotropic materials have three orthogonal planes of symmetry. If the basis vectors (Template:Math) are normals to the planes of symmetry then the coordinate transformation relations imply that

<math display="block"> \begin{bmatrix} \sigma_1 \\ \sigma_2 \\ \sigma_3 \\ \sigma_4 \\ \sigma_5 \\ \sigma_6 \end{bmatrix} \,=\, \begin{bmatrix}

C_{11} & C_{12} & C_{13} & 0 & 0 & 0 \\

C_{12} & C_{22} & C_{23} & 0 & 0 & 0 \\ C_{13} & C_{23} & C_{33} & 0 & 0 & 0 \\ 0 & 0 & 0 & C_{44} & 0 & 0 \\ 0 & 0 & 0 & 0 & C_{55} & 0 \\ 0 & 0 & 0 & 0 & 0 & C_{66} \end{bmatrix} \begin{bmatrix} \varepsilon_1 \\ \varepsilon_2 \\ \varepsilon_3 \\ \varepsilon_4 \\ \varepsilon_5 \\ \varepsilon_6 \end{bmatrix} </math> The inverse of this relation is commonly written as<ref name=Boresi>Template:Cite book</ref>Template:Page needed <math display="block">

\begin{bmatrix}
\varepsilon_{xx} \\ \varepsilon_{yy} \\ \varepsilon_{zz} \\ 2\varepsilon_{yz} \\ 2\varepsilon_{zx} \\ 2\varepsilon_{xy}
\end{bmatrix}
\,=\, \begin{bmatrix}
\frac{1}{E_{x}} & - \frac{\nu_{yx}}{E_{y}} & - \frac{\nu_{zx}}{E_{z}} & 0 & 0 & 0 \\
-\frac{\nu_{xy}}{E_{x}} & \frac{1}{E_{y}} & - \frac{\nu_{zy}}{E_{z}} & 0 & 0 & 0 \\
-\frac{\nu_{xz}}{E_{x}} & - \frac{\nu_{yz}}{E_{y}} & \frac{1}{E_{z}} & 0 & 0 & 0 \\
0 & 0 & 0 & \frac{1}{G_{yz}} & 0 & 0 \\
0 & 0 & 0 & 0 & \frac{1}{G_{zx}} & 0 \\
0 & 0 & 0 & 0 & 0 & \frac{1}{G_{xy}} \\
\end{bmatrix}
\begin{bmatrix}
\sigma_{xx} \\ \sigma_{yy} \\ \sigma_{zz} \\ \sigma_{yz} \\ \sigma_{zx} \\ \sigma_{xy}
\end{bmatrix}
</math>

where

Under plane stress conditions, Template:Math, Hooke's law for an orthotropic material takes the form <math display="block">

\begin{bmatrix}\varepsilon_{xx} \\ \varepsilon_{yy} \\ 2\varepsilon_{xy} \end{bmatrix} \,=\, 
\begin{bmatrix} \frac{1}{E_{x}} & -\frac{\nu_{yx}}{E_{y}} & 0 \\
-\frac{\nu_{xy}}{E_{x}} & \frac{1}{E_{y}} & 0 \\
0 & 0 & \frac{1}{G_{xy}} \end{bmatrix}
\begin{bmatrix}\sigma_{xx} \\ \sigma_{yy} \\ \sigma_{xy} \end{bmatrix} \,.
</math>

The inverse relation is <math display="block">

\begin{bmatrix}\sigma_{xx} \\ \sigma_{yy} \\ \sigma_{xy} \end{bmatrix}
\,=\, \frac{1}{1-\nu_{xy}\nu_{yx}}
\begin{bmatrix} E_{x} & \nu_{yx}E_{x} & 0 \\
\nu_{xy}E_{y} & E_{y} & 0 \\
0 & 0 & G_{xy}(1-\nu_{xy}\nu_{yx}) \end{bmatrix}
\begin{bmatrix}\varepsilon_{xx} \\ \varepsilon_{yy} \\ 2\varepsilon_{xy} \end{bmatrix} \,.
</math>

The transposed form of the above stiffness matrix is also often used.

Transversely isotropic materialsEdit

A transversely isotropic material is symmetric with respect to a rotation about an axis of symmetry. For such a material, if Template:Math is the axis of symmetry, Hooke's law can be expressed as <math display="block"> \begin{bmatrix} \sigma_1 \\ \sigma_2 \\ \sigma_3 \\ \sigma_4 \\ \sigma_5 \\ \sigma_6 \end{bmatrix} \,=\, \begin{bmatrix}

C_{11} & C_{12} & C_{13} & 0 & 0 & 0 \\

C_{12} & C_{11} & C_{13} & 0 & 0 & 0 \\ C_{13} & C_{13} & C_{33} & 0 & 0 & 0 \\ 0 & 0 & 0 & C_{44} & 0 & 0 \\ 0 & 0 & 0 & 0 & C_{44} & 0 \\ 0 & 0 & 0 & 0 & 0 & \frac{C_{11}-C_{12}}{2} \end{bmatrix} \begin{bmatrix} \varepsilon_1 \\ \varepsilon_2 \\ \varepsilon_3 \\ \varepsilon_4 \\ \varepsilon_5 \\ \varepsilon_6 \end{bmatrix} </math>

More frequently, the Template:Math axis is taken to be the axis of symmetry and the inverse Hooke's law is written as <ref name=Tan>Template:Cite book</ref> <math display="block"> \begin{bmatrix}

\varepsilon_{xx} \\ \varepsilon_{yy} \\ \varepsilon_{zz} \\ 2\varepsilon_{yz} \\ 2\varepsilon_{zx} \\ 2\varepsilon_{xy}
\end{bmatrix}
\,=\, \begin{bmatrix}
        \frac{1}{E_{x}} & - \frac{\nu_{yx}}{E_{y}} & - \frac{\nu_{zx}}{E_{z}} & 0                & 0                & 0 \\
-\frac{\nu_{xy}}{E_{x}} &          \frac{1}{E_{y}} & - \frac{\nu_{zy}}{E_{z}} & 0                & 0                & 0 \\
-\frac{\nu_{xz}}{E_{x}} & - \frac{\nu_{yz}}{E_{y}} &          \frac{1}{E_{z}} & 0                & 0                & 0 \\
0                       & 0                        & 0                        & \frac{1}{G_{yz}} & 0                & 0 \\
0                       & 0                        & 0                        &  0               & \frac{1}{G_{xz}} & 0 \\
0                       & 0                        & 0                        & 0                & 0                & \frac{1}{G_{xy}} \\
\end{bmatrix}
\begin{bmatrix}
\sigma_{xx} \\ \sigma_{yy} \\ \sigma_{zz} \\ \sigma_{yz} \\ \sigma_{zx} \\ \sigma_{xy}
\end{bmatrix}
</math>

Universal elastic anisotropy indexEdit

To grasp the degree of anisotropy of any class, a universal elastic anisotropy index (AU)<ref>Template:Cite journal</ref> was formulated. It replaces the Zener ratio, which is suited for cubic crystals.

Thermodynamic basisEdit

Linear deformations of elastic materials can be approximated as adiabatic. Under these conditions and for quasistatic processes the first law of thermodynamics for a deformed body can be expressed as <math display="block"> \delta W = \delta U </math> where Template:Mvar is the increase in internal energy and Template:Mvar is the work done by external forces. The work can be split into two terms <math display="block"> \delta W = \delta W_\mathrm{s} + \delta W_\mathrm{b} </math> where Template:Math is the work done by surface forces while Template:Math is the work done by body forces. If Template:Math is a variation of the displacement field Template:Math in the body, then the two external work terms can be expressed as <math display="block"> \delta W_\mathrm{s} = \int_{\partial\Omega} \mathbf{t}\cdot\delta\mathbf{u}\,dS \,; \qquad \delta W_\mathrm{b} = \int_{\Omega} \mathbf{b}\cdot\delta\mathbf{u}\,dV </math> where Template:Math is the surface traction vector, Template:Math is the body force vector, Template:Mvar represents the body and Template:Math represents its surface. Using the relation between the Cauchy stress and the surface traction, Template:Math (where Template:Math is the unit outward normal to Template:Math), we have <math display="block"> \delta W = \delta U = \int_{\partial\Omega} (\mathbf{n}\cdot\boldsymbol{\sigma})\cdot\delta\mathbf{u}\,dS + \int_{\Omega} \mathbf{b}\cdot\delta\mathbf{u}\,dV\,. </math> Converting the surface integral into a volume integral via the divergence theorem gives <math display="block"> \delta U = \int_{\Omega} \big(\nabla\cdot(\boldsymbol{\sigma}\cdot\delta\mathbf{u}) + \mathbf{b}\cdot\delta\mathbf{u}\big)\, dV \,. </math> Using the symmetry of the Cauchy stress and the identity <math display="block">\nabla\cdot(\mathbf{a}\cdot\mathbf{b}) = (\nabla\cdot\mathbf{a})\cdot\mathbf{b}+\tfrac12\left(\mathbf{a}^\mathsf{T} : \nabla\mathbf{b}+ \mathbf{a}:(\nabla\mathbf{b})^\mathsf{T}\right)</math> we have the following

<math display="block"> \delta U = \int_{\Omega} \left(\boldsymbol{\sigma}:\tfrac12\left(\nabla\delta\mathbf{u}+(\nabla\delta\mathbf{u})^\mathsf{T}\right) + \left(\nabla\cdot\boldsymbol{\sigma}+\mathbf{b}\right)\cdot\delta\mathbf{u}\right)\,dV \,. </math> From the definition of strain and from the equations of equilibrium we have <math display="block"> \delta\boldsymbol{\varepsilon} = \tfrac12\left(\nabla\delta\mathbf{u}+(\nabla\delta\mathbf{u})^\mathsf{T}\right) \,;\qquad \nabla\cdot\boldsymbol{\sigma}+\mathbf{b}=\mathbf{0} \,. </math> Hence we can write <math display="block"> \delta U = \int_{\Omega} \boldsymbol{\sigma}:\delta\boldsymbol{\varepsilon}\,dV </math> and therefore the variation in the internal energy density is given by <math display="block"> \delta U_0 = \boldsymbol{\sigma}:\delta\boldsymbol{\varepsilon} \,. </math> An elastic material is defined as one in which the total internal energy is equal to the potential energy of the internal forces (also called the elastic strain energy). Therefore, the internal energy density is a function of the strains, Template:Math and the variation of the internal energy can be expressed as <math display="block"> \delta U_0 = \frac{\partial U_0}{\partial\boldsymbol{\varepsilon}}:\delta\boldsymbol{\varepsilon} \,. </math> Since the variation of strain is arbitrary, the stress–strain relation of an elastic material is given by <math display="block"> \boldsymbol{\sigma} = \frac{\partial U_0}{\partial\boldsymbol{\varepsilon}}\,. </math> For a linear elastic material, the quantity Template:Math is a linear function of Template:Math, and can therefore be expressed as <math display="block"> \boldsymbol{\sigma} = \mathsf{c}:\boldsymbol{\varepsilon} </math> where c is a fourth-rank tensor of material constants, also called the stiffness tensor. We can see why c must be a fourth-rank tensor by noting that, for a linear elastic material, <math display="block"> \frac{\partial}{\partial\boldsymbol{\varepsilon}}\boldsymbol{\sigma}(\boldsymbol{\varepsilon}) = \text{constant} = \mathsf{c} \,. </math> In index notation <math display="block"> \frac{\partial\sigma_{ij}}{\partial\varepsilon_{kl}} = \text{constant} = c_{ijkl} \,. </math>

The right-hand side constant requires four indices and is a fourth-rank quantity. We can also see that this quantity must be a tensor because it is a linear transformation that takes the strain tensor to the stress tensor. We can also show that the constant obeys the tensor transformation rules for fourth-rank tensors.

See alsoEdit

NotesEdit

Template:Reflist

ReferencesEdit

External linksEdit

Template:Elastic moduli