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Hooke's law accurately models the physical properties of common mechanical springs for small changes in length

In mechanics, and physics, Hooke's law of elasticity is an approximation that states that the extension of a spring is in direct proportion with the load added to it as long as this load does not exceed the elastic limit. Materials for which Hooke's law is a useful approximation are known as linear-elastic or "Hookean" materials.

Mathematically, Hooke's law states that

 \mathbf{F}=-k\mathbf{x},

where

x is the displacement of the end of the spring from its equilibrium position;
F is the restoring force exerted by the material; and
k is the force constant (or spring constant).
Continuum mechanics
BernoullisLawDerivationDiagram.svg

When this holds, the behavior is said to be linear. If shown on a graph, the line should show a direct variation. There is a negative sign on the right hand side of the equation because the restoring force always acts in the opposite direction of the displacement (for example, when a spring is stretched to the left, it pulls back to the right).

Hooke's law is named after the 17th century British physicist Robert Hooke. He first stated this law in 1676 as a Latin anagram,[1] whose solution he published in 1678 as Ut tensio, sic vis, meaning, "As the extension, so the force".

Contents

Elastic

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.

We may view a rod of any elastic material as a linear spring. The rod has length L and cross-sectional area A. Its extension (strain) is linearly proportional to its tensile stress σ, by a constant factor, the inverse of its modulus of elasticity, E, hence,

\sigma = E \varepsilon

or

\Delta L = \frac{F}{E A} L = \frac{\sigma}{E} L.

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.

Applications of the law include spring operated weighing machines, stress analysis and modeling of materials.

The spring equation

Stress–strain curve for low-carbon steel. Hooke's law is only valid for the portion of the curve between the origin and the yield point(2).
1. Ultimate strength
2. Yield strength-corresponds to yield point.
3. Rupture
4. Strain hardening region
5. Necking region. A: Apparent stress (F/A0)
B: True stress (F/A)

The most commonly encountered form of Hooke's law is probably the spring equation, which relates the force exerted by a spring to the distance it is stretched by a spring constant, k, measured in force per length.

F=-kx\,

The negative sign indicates that the force exerted by the spring is in direct opposition to the direction of displacement. It is called a "restoring force", as it tends to restore the system to equilibrium. The potential energy stored in a spring is given by

U={1\over2}kx^2

which comes from adding up the energy it takes to incrementally compress the spring. That is, the integral of force over distance. (Note that potential energy of a spring is always non-negative.)

This potential can be visualized as a parabola on the U-x plane. As the spring is stretched in the positive x-direction, the potential energy increases (the same thing happens as the spring is compressed). The corresponding point on the potential energy curve is higher than that corresponding to the equilibrium position (x = 0). The tendency for the spring is to therefore decrease its potential energy by returning to its equilibrium (unstretched) position, just as a ball rolls downhill to decrease its gravitational potential energy.

If a mass m is attached to the end of such a spring, the system becomes a harmonic oscillator. It will oscillate with a natural frequency given either as an angular frequency

\omega = \sqrt{k \over m}

or as a frequency

f = {1 \over 2 \pi} \sqrt{k \over m}.

Multiple springs

When two springs are attached to a mass and compressed, the following table compares values of the springs.

Comparison In Series In Parallel
SpringsInSeries.svg
SpringsInParallel.svg
Equivalent
spring constant
\frac{1}{k_{eq}} = \frac{1}{k_1} + \frac{1}{k_2} \, k_{eq} = k_1 + k_2 \,
Compressed
distance
\frac{x_1}{x_2} = \frac{k_2}{k_1} \, x_1 = x_2 \,
Energy
stored
\frac{E_1}{E_2} = \frac{k_2}{k_1} \, \frac{E_1}{E_2} = \frac{k_1}{k_2} \,
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Derivation

Tensor expression of Hooke's Law

When working with a three-dimensional stress state, a 4th order tensor \mathsf{c} (c_{ijk\ell}) containing 81 elastic coefficients must be defined to link the stress tensor \boldsymbol{\sigma}ij) and the strain tensor \boldsymbol{\epsilon} (\epsilon_{k\ell}).

\boldsymbol{\sigma} = \mathsf{c}:\boldsymbol{\epsilon} ~.

Expressed in terms of components with respect to an orthonormal basis, the generalized form of Hooke's law is written as (using the summation convention)

\sigma_{ij} = c_{ijk\ell}~\epsilon_{k\ell}

The tensor \mathsf{c} is called the stiffness tensor. Due to the symmetry of the stress tensor, strain tensor, and stiffness tensor, only 21 elastic coefficients are independent. As stress is measured in units of pressure and strain is dimensionless, the entries of c_{ijk\ell} are also in units of pressure.

The expression for generalized Hooke's law can be inverted to get a relation for the strain in terms of stress:

 \boldsymbol{\epsilon} = \mathsf{s}:\boldsymbol{\sigma} \qquad {\rm or} \qquad \epsilon_{ij} = s_{ijk\ell}~\sigma_{k\ell} ~.

The tensor \mathsf{s} is called the compliance tensor.

Generalization for the case of large deformations is provided by models of neo-Hookean solids and Mooney-Rivlin solids.

Isotropic materials

(see viscosity for an analogous development for viscous fluids.)

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. (Symon (1971) Ch. 10) Thus:

\varepsilon_{ij}=\left(\frac{1}{3}\varepsilon_{kk}\delta_{ij}\right) +\left(\varepsilon_{ij}-\frac{1}{3}\varepsilon_{kk}\delta_{ij}\right)

where δij is the Kronecker delta. The first term on the right is the constant tensor, also known as the pressure, and the second term is the traceless symmetric tensor, also known as the 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:

\sigma_{ij}=3K\left(\frac{1}{3}\varepsilon_{kk}\delta_{ij}\right) +2G\left(\varepsilon_{ij}-\frac{1}{3}\varepsilon_{kk}\delta_{ij}\right)\,

where K is the bulk modulus and G is the shear modulus.

Using the relationships between the elastic moduli, these equations may also be expressed in various other ways. For example, the strain may be expressed in terms of the stress tensor as:

\varepsilon_{11} = \frac{1}{E}\left( \sigma_{11} - \nu(\sigma_{22}+\sigma_{33}) \right)
\varepsilon_{22} = \frac{1}{E}\left( \sigma_{22} - \nu(\sigma_{11}+\sigma_{33}) \right)
\varepsilon_{33} = \frac{1}{E}\left( \sigma_{33} - \nu(\sigma_{11}+\sigma_{22}) \right)
\varepsilon_{12} = \frac{\sigma_{12}}{2G}
\varepsilon_{13} = \frac{\sigma_{13}}{2G}
\varepsilon_{23} = \frac{\sigma_{23}}{2G}

where E is the modulus of elasticity and ν is Poisson's ratio. (See 3-D elasticity).

Anisotropic materials

The symmetry of the Cauchy stress tensor (\sigma_{ij} = \sigma_{ji}\,) and the generalized Hooke's laws (\sigma_{ij} = c_{ijk\ell}~ \epsilon_{k\ell}) implies that c_{ijk\ell} = c_{jik\ell}\,. Similarly, the symmetry of the infinitesimal strain tensor implies that c_{ijk\ell} = c_{ij\ell k}\,. These symmetries are called the minor symmetries of the stiffness tensor (\mathsf{c}).

If in addition, the stress-strain relation can be derived from a strain energy density functional (U), then

 \sigma_{ij} = c_{ijk\ell}~\epsilon_{k\ell} = \cfrac{\partial U}{\partial \epsilon_{ij}} \quad \implies \quad \cfrac{\partial^2 U}{\partial\epsilon_{ij}~\partial\epsilon_{k\ell}} = c_{ijk\ell} ~.

The arbitrariness of the order of differentiation implies that c_{ijk\ell} = c_{k\ell ij}\,. These are called the major symmetries of the stiffness tensor. The major and minor symmetries indicate that the stiffness tensor has only 21 independent components.

Matrix representation (stiffness tensor)

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 (\mathbf{e}_1,\mathbf{e}_2,\mathbf{e}_3) as

 [\boldsymbol{\sigma}] = \begin{bmatrix}\sigma_{11}\\ \sigma_{22} \\ \sigma_{33} \\ \sigma_{23} \\ \sigma_{31} \\ \sigma_{12} \end{bmatrix} \equiv \begin{bmatrix} \sigma_1 \\ \sigma_2 \\ \sigma_3 \\ \sigma_4 \\ \sigma_5 \\ \sigma_6 \end{bmatrix} ~;~~ [\boldsymbol{\epsilon}] = \begin{bmatrix}\epsilon_{11}\\ \epsilon_{22} \\ \epsilon_{33} \\ 2\epsilon_{23} \\ 2\epsilon_{31} \\ 2\epsilon_{12} \end{bmatrix} \equiv \begin{bmatrix} \epsilon_1 \\ \epsilon_2 \\ \epsilon_3 \\ \epsilon_4 \\ \epsilon_5 \\ \epsilon_6 \end{bmatrix}

Then the stiffness tensor (\mathsf{c}) can be expressed as

 [\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}

and Hooke's law is written as

 [\boldsymbol{\sigma}] = [\mathsf{C}][\boldsymbol{\epsilon}] \qquad \text{or} \qquad \sigma_i = C_{ij} \epsilon_j ~.

Similarly the compliance tensor (\mathsf{s}) can be written as

 [\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}

Change of coordinate system

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 [2]

 c_{pqrs} = l_{pi}~l_{qj}~l_{rk}~l_{s\ell}~c_{ijk\ell}

where lab are the components of an orthogonal rotation matrix [L]. The same relation also holds for inversions.

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

 [\mathbf{e}_i'] = [L][\mathbf{e}_i]

then

 C_{ij}~\epsilon_i~\epsilon_j = C_{ij}'~\epsilon'_i~\epsilon'_j ~.

In addition, if the material is symmetric with respect to the transformation [L] then

 C_{ij} = C'_{ij} \quad \implies \quad C_{ij}~(\epsilon_i~\epsilon_j - \epsilon'_i~\epsilon'_j) = 0 ~.

Orthotropic materials

Orthotropic materials have three orthogonal planes of symmetry. If the basis vectors (\mathbf{e}_1,\mathbf{e}_2,\mathbf{e}_3) are normals to the planes of symmetry then the coordinate transformation relations imply that

 \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} \epsilon_1 \\ \epsilon_2 \\ \epsilon_3 \\ \epsilon_4 \\ \epsilon_5 \\ \epsilon_6 \end{bmatrix}

The inverse of this relation is commonly written as[3]

 \begin{bmatrix} \epsilon_{{\rm xx}} \\ \epsilon_{\rm yy} \\ \epsilon_{\rm zz} \\ 2\epsilon_{\rm yz} \\ 2\epsilon_{\rm zx} \\ 2\epsilon_{\rm xy} \end{bmatrix} = \begin{bmatrix} \tfrac{1}{E_{\rm x}} & - \tfrac{\nu_{\rm xy}}{E_{\rm x}} & - \tfrac{\nu_{\rm xz}}{E_{\rm x}} & 0 & 0 & 0 \ -\tfrac{\nu_{\rm yx}}{E_{\rm y}} & \tfrac{1}{E_{\rm y}} & - \tfrac{\nu_{\rm yz}}{E_{\rm y}} & 0 & 0 & 0 \ -\tfrac{\nu_{\rm zx}}{E_{\rm z}} & - \tfrac{\nu_{\rm zy}}{E_{\rm z}} & \tfrac{1}{E_{\rm z}} & 0 & 0 & 0 \ 0 & 0 & 0 & \tfrac{1}{G_{\rm yz}} & 0 & 0 \ 0 & 0 & 0 & 0 & \tfrac{1}{G_{\rm zx}} & 0 \ 0 & 0 & 0 & 0 & 0 & \tfrac{1}{G_{\rm xy}} \ \end{bmatrix} \begin{bmatrix} \sigma_{\rm xx} \\ \sigma_{\rm yy} \\ \sigma_{\rm zz} \\ \sigma_{\rm yz} \\ \sigma_{\rm zx} \\ \sigma_{\rm xy} \end{bmatrix}

where

{E}_{\rm i}\, is the Young's modulus along axis i
G_{\rm ij}\, is the shear modulus in direction j on the plane whose normal is in direction i
\nu_{\rm ij}\, is the Poisson's ratio that corresponds to a contraction in direction j when an extension is applied in direction i.

Transversely isotropic materials

A transversely isotropic material is symmetric with respect to a rotation about an axis of symmetry. For such a material, if \mathbf{e}_3 is the axis of symmetry, Hooke's law can be expressed as

 \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 & \tfrac{1}{2}(C_{11}-C_{12}) \end{bmatrix} \begin{bmatrix} \epsilon_1 \\ \epsilon_2 \\ \epsilon_3 \\ \epsilon_4 \\ \epsilon_5 \\ \epsilon_6 \end{bmatrix}

More frequently, the x \equiv \mathbf{e}_1 axis is taken to be the axis of symmetry and the inverse Hooke's law is written as [4]

 \begin{bmatrix} \epsilon_{{\rm xx}} \\ \epsilon_{\rm yy} \\ \epsilon_{\rm zz} \\ 2\epsilon_{\rm yz} \\ 2\epsilon_{\rm zx} \\ 2\epsilon_{\rm xy} \end{bmatrix} = \begin{bmatrix} \tfrac{1}{E_{\rm x}} & - \tfrac{\nu_{\rm xy}}{E_{\rm x}} & - \tfrac{\nu_{\rm xy}}{E_{\rm x}} & 0 & 0 & 0 \ -\tfrac{\nu_{\rm yx}}{E_{\rm y}} & \tfrac{1}{E_{\rm y}} & - \tfrac{\nu_{\rm yz}}{E_{\rm y}} & 0 & 0 & 0 \ -\tfrac{\nu_{\rm yx}}{E_{\rm y}} & - \tfrac{\nu_{\rm zy}}{E_{\rm y}} & \tfrac{1}{E_{\rm y}} & 0 & 0 & 0 \ 0 & 0 & 0 & \tfrac{2(1+\nu_{\rm yz})}{E_{\rm y}} & 0 & 0 \ 0 & 0 & 0 & 0 & \tfrac{1}{G_{\rm xy}} & 0 \ 0 & 0 & 0 & 0 & 0 & \tfrac{1}{G_{\rm xy}} \ \end{bmatrix} \begin{bmatrix} \sigma_{\rm xx} \\ \sigma_{\rm yy} \\ \sigma_{\rm zz} \\ \sigma_{\rm yz} \\ \sigma_{\rm zx} \\ \sigma_{\rm xy} \end{bmatrix}

Thermodynamic basis of Hooke's law

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

 \delta W = \delta U\,

where δU is the increase in internal energy and δW is the work done by external forces. The work can be split into two terms

 \delta W = \delta W_s + \delta W_b\,

where δWs is the work done by surface forces while δWb is the work done by body forces. If \delta\mathbf{u} is a variation of the displacement field \mathbf{u} in the body, then the two external work terms can be expressed as

 \delta W_s = \int_{\partial\Omega} \mathbf{t}\cdot\delta\mathbf{u}~{\rm dS} ~;~~ \delta W_b = \int_{\Omega} \mathbf{b}\cdot\delta\mathbf{u}~{\rm dV}

where \mathbf{t} is the surface traction vector, \mathbf{b} is the body force vector, \Omega\, represents the body and \partial\Omega represents its surface. Using the relation between the Cauchy stress and the surface traction, \mathbf{t} = \mathbf{n}\cdot\boldsymbol{\sigma} (where \mathbf{n} is the unit outward normal to \partial\Omega), we have

 \delta W = \delta U = \int_{\partial\Omega} (\mathbf{n}\cdot\boldsymbol{\sigma})\cdot\delta\mathbf{u}~{\rm dS} + \int_{\Omega} \mathbf{b}\cdot\delta\mathbf{u}~{\rm dV}

Converting the surface integral into a volume integral via the divergence theorem gives

 \delta U = \int_{\Omega} [\boldsymbol{\nabla}\cdot(\boldsymbol{\sigma}\cdot\delta\mathbf{u}) + \mathbf{b}\cdot\delta\mathbf{u}]~ {\rm dV} ~.

Using the symmetry of the Cauchy stress and the identity

 \boldsymbol{\nabla}\cdot(\boldsymbol{A}\cdot\mathbf{b}) = (\boldsymbol{\nabla}\cdot\boldsymbol{A})\cdot\mathbf{b}+ \tfrac{1}{2}[\boldsymbol{A}^T:\boldsymbol{\nabla}\mathbf{b}+ \boldsymbol{A}:(\boldsymbol{\nabla}\mathbf{b})^T]

we have

 \delta U = \int_{\Omega} [\boldsymbol{\sigma}: \tfrac{1}{2}\{\boldsymbol{\nabla}\delta\mathbf{u}+(\boldsymbol{\nabla}\delta\mathbf{u})^T\} + \{\boldsymbol{\nabla}\cdot\boldsymbol{\sigma}+\mathbf{b}\}\cdot\delta\mathbf{u}]~{\rm dV} ~.

From the definition of strain and from the equations of equilibrium we have

 \delta\boldsymbol{\epsilon} = \tfrac{1}{2}[\boldsymbol{\nabla}\delta\mathbf{u}+(\boldsymbol{\nabla}\delta\mathbf{u})^T] ~;~~ \boldsymbol{\nabla}\cdot\boldsymbol{\sigma}+\mathbf{b}=\mathbf{0} ~.

Hence we can write

 \delta U = \int_{\Omega} \boldsymbol{\sigma}:\delta\boldsymbol{\epsilon}~{\rm dV}

and therefore the variation in the internal energy density is given by

 \delta U_0 = \boldsymbol{\sigma}:\delta\boldsymbol{\epsilon} ~.

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, U_0 = U_0(\boldsymbol{\epsilon}) and the variation of the internal energy can be expressed as

 \delta U_0 = \cfrac{\partial U_0}{\partial\boldsymbol{\epsilon}}:\delta\boldsymbol{\epsilon} ~.

Since the variation of strain is arbitrary, the stress-strain relation of an elastic material is given by

 \boldsymbol{\sigma} = \cfrac{\partial U_0}{\partial\boldsymbol{\epsilon}}~.

For a linear elastic material, the quantity \partial U_0/\partial\boldsymbol{\epsilon} is a linear function of \boldsymbol{\epsilon}, and can therefore be expressed as

 \boldsymbol{\sigma} = \mathsf{c}:\boldsymbol{\epsilon}

where \mathsf{c} is a fourth-order tensor of material constants, also called the stiffness tensor.

See also

References

  1. ^ The anagram was "ceiiinossssttuu", [1]; cf. the anagram for the Catenary, which appeared in the preceding paragraph.
  2. ^ Slaughter, W. S., 2002, The Linearized Theory of Elasticity, Birkhauser
  3. ^ Boresi, A. P, Schmidt, R. J. and Sidebottom, O. M., 1993, Advanced Mechanics of Materials, Wiley.
  4. ^ Tan, S. C., 1994, Stress Concentrations in Laminated Composites, Technomic Publishing Company, Lancaster, PA.
  • A.C. Ugural, S.K. Fenster, Advanced Strength and Applied Elasticity, 4th ed
  •  Symon, Keith (1971). Mechanics. Addison-Wesley, Reading, MA. ISBN 0-201-07392-7.  

External links

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Wiktionary

Up to date as of January 15, 2010

Definition from Wiktionary, a free dictionary

Contents

English

Etymology

From the name of Robert Hooke, English physicist

Noun

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Wikipedia

Hooke's law

  1. (physics) the principle that the stress applied to a solid is directly proportional to the strain produced. This law describes the behavior of springs and solids stressed within their elastic limit.

Translations

  • French: loi de Hooke fr(fr) f.
  • German: Hookesches Gesetz de(de) n.
  • Italian: legge di Hooke it(it) f.
  • Russian: закон Гука ru(ru) n.

See also


Simple English

The spring equation shows Hooke's Law with math.

= The spring equation

= The length of a spring always changes by the same amount when it is pushed or pulled. The equation for that is:

F=-kx
where
F is how much push or pull is on the spring (e.g. 10 kilograms)
k is the spring constant, or how strong the spring is. Different springs have different strengths or k.
x is how far the spring was pushed or pulled

The negative sign is because the direction of the force is always opposite of the direction that the spring was pushed or pulled. When x = 0, the spring how far it was when there was no push or pull on it. The spring is at the equilibrium position. There is a minus sign because the force of the spring does not go to the same direction as the spring moves. This equation only works on a linear spring. A linear spring is a spring that is only being pushed or pulled in one direction, like left or right or up or down.

Elastic Potential Energy

Elastic potential energy is the energy saved in an object that is stretched, compressed (compression is pressing objects together), twisted or bent. For example, an arrow gets the elastic potential energy from the bow. When it leaves the bow, the potential energy turns into kinetic energy. The equation of the elastic potential energy is:

U=\frac{1}{2}kx^2
where
U is the elastic potential energy.
k is the spring constant.
x is the distance pushed or pulled.

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