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Elastic energy

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Form of energy
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Elastic energy is the mechanicalpotential energy stored in the configuration of a material or physical system as it is subjected toelastic deformation bywork performed upon it. Elastic energy occurs when objects are impermanently compressed, stretched or generallydeformed in any manner.Elasticity theory primarily develops formalisms for the mechanics of solid bodies and materials.[1] The elastic potential energy equation is used in calculations of positions ofmechanical equilibrium. The energy is potential as it will be converted into other forms of energy, such askinetic energy andsound energy, when the object is allowed to return to its original shape (reformation) by itselasticity.

U=12kΔx2{\displaystyle U={\frac {1}{2}}k\,\Delta x^{2}}

The essence of elasticity isreversibility. Forces applied to an elastic material transfer energy into the material which, upon yielding that energy to its surroundings, can recover its original shape. However, all materials have limits to the degree of distortion they can endure without breaking or irreversibly altering their internal structure. Hence, the characterizations of solid materials include specification, usually in terms of strains, of its elastic limits. Beyond the elastic limit, a material is no longer storing all of the energy from mechanical work performed on it in the form of elastic energy.

Elastic energy of or within a substance is static energy of configuration. It corresponds to energy stored principally by changing the interatomic distances between nuclei.Thermal energy is the randomized distribution of kinetic energy within the material, resulting in statistical fluctuations of the material about the equilibrium configuration. There is some interaction, however. For example, for some solid objects, twisting, bending, and other distortions may generate thermal energy, causing the material's temperature to rise. Thermal energy in solids is often carried by internal elastic waves, calledphonons. Elastic waves that are large on the scale of an isolated object usually produce macroscopic vibrations .Although elasticity is most commonly associated with the mechanics of solid bodies or materials, even the early literature on classical thermodynamics defines and uses "elasticity of a fluid" in ways compatible with the broad definition provided in the Introduction above.[2]: 107 et seq. 

Solids include complex crystalline materials with sometimes complicated behavior. By contrast, the behavior of compressible fluids, and especially gases, demonstrates the essence of elastic energy with negligible complication. The simple thermodynamic formula:dU=PdV ,{\displaystyle dU=-P\,dV\ ,} where dU is an infinitesimal change in recoverable internal energyU,P is the uniform pressure (a force per unit area) applied to the material sample of interest, anddV is the infinitesimal change in volume that corresponds to the change in internal energy. The minus sign appears becausedV is negative under compression by a positive applied pressure which also increases the internal energy. Upon reversal, the work that is doneby a system is the negative of the change in its internal energy corresponding to the positivedV of an increasing volume. The system loses stored internal energy when doing work on its surroundings. Pressure is stress and volumetric change corresponds to changing the relative spacing of points within the material. The stress-strain-internal energy relationship of the foregoing formula is repeated in formulations for elastic energy of solid materials with complicated crystalline structure.

Elastic potential energy in mechanical systems

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Components of mechanical systems storeelastic potential energy if they are deformed when forces are applied to the system. Energy is transferred to an object bywork when an external force displaces or deforms the object. The quantity of energy transferred is the vectordot product of the force and the displacement of the object. As forces are applied to the system they are distributed internally to its component parts. While some of the energy transferred can end up stored as the kinetic energy of acquired velocity, the deformation of component objects results in stored elastic energy.

A prototypical elastic component is a coiled spring. The linear elastic performance of a spring is parametrized by a constant of proportionality, called the spring constant. This constant is usually denoted ask (see alsoHooke's law) and depends on the geometry, cross-sectional area, undeformed length and nature of the material from which the coil is fashioned. Within a certain range of deformation,k remains constant and is defined as the negative ratio of displacement to the magnitude of the restoring force produced by the spring at that displacement.

k=FrLLo{\displaystyle k=-{\frac {F_{r}}{L-L_{o}}}}

The deformed length,might have been the result for some L, can be larger or smaller thanLo, the undeformed length, so to keepk positive,Fr must be given as a vector component of the restoring force whose sign is negative forL>Lo and positive forL<Lo. If the displacement is abbreviated asLLo=x,{\displaystyle L-L_{o}=x,} then Hooke's law can be written in the usual formFr=kx.{\displaystyle F_{r}=-k\,x.}

Energy absorbed and held in the spring can be derived using Hooke's law to compute the restoring force as a measure of the applied force. This requires the assumption, sufficiently correct in most circumstances, that at a given moment, the magnitude of applied force.

For each infinitesimal displacementdx, the applied force is simplyk x and the product of these is the infinitesimal transfer of energy into the springdU. The total elastic energy placed into the spring from zero displacement to final length L is thus the integralU=0LLokxdx=12k(LLo)2{\displaystyle U=\int _{0}^{L-L_{o}}k\,x\,dx={\tfrac {1}{2}}k(L-L_{o})^{2}}

For a material of Young's modulus,Y (same as modulus of elasticityλ), cross sectional area,A0, initial length,l0, which is stretched by a length,Δl{\displaystyle \Delta l}:Ue=YA0Δll0d(Δl)=YA0Δl22l0{\displaystyle U_{e}=\int {\frac {YA_{0}\Delta l}{l_{0}}}\,d\left(\Delta l\right)={\frac {YA_{0}{\Delta l}^{2}}{2l_{0}}}} whereUe is the elastic potential energy.

The elastic potential energy per unit volume is given by:UeA0l0=YΔl22l02=12Yε2{\displaystyle {\frac {U_{e}}{A_{0}l_{0}}}={\frac {Y{\Delta l}^{2}}{2l_{0}^{2}}}={\frac {1}{2}}Y{\varepsilon }^{2}}whereε=Δll0{\displaystyle \varepsilon ={\frac {\Delta l}{l_{0}}}} is the strain in the material.

In the general case, elastic energy is given by the free energy per unit of volumef as a function of thestrain tensor componentsεijf(εij)=12λεii2+μεij2{\displaystyle f(\varepsilon _{ij})={\frac {1}{2}}\lambda \varepsilon _{ii}^{2}+\mu \varepsilon _{ij}^{2}}whereλ andμ are the Lamé elastic coefficients and we useEinstein summation convention. Noting the thermodynamic connection between stress tensor components and strain tensor components,[1]σij=(fεij)T,{\displaystyle \sigma _{ij}=\left({\frac {\partial f}{\partial \varepsilon _{ij}}}\right)_{T},}where the subscriptT denotes that temperature is held constant, then we find that if Hooke's law is valid, we can write the elastic energy density asf=12εijσij.{\displaystyle f={\frac {1}{2}}\varepsilon _{ij}\sigma _{ij}.}

Continuum systems

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Matter in bulk can be distorted in many different ways: stretching, shearing, bending, twisting, etc. Each kind of distortion contributes to the elastic energy of a deformed material. Inorthogonal coordinates, the elastic energy per unit volume due to strain is thus a sum of contributions:U=12Cijklεijεkl,{\displaystyle U={\frac {1}{2}}C_{ijkl}\varepsilon _{ij}\varepsilon _{kl},}whereCijkl{\displaystyle C_{ijkl}} is a 4thrank tensor, called theelastic tensor or stiffness tensor[3] which is a generalization of the elastic moduli of mechanical systems, andεij{\displaystyle \varepsilon _{ij}} is thestrain tensor (Einstein summation notation has been used to imply summation over repeated indices). The values ofCijkl{\displaystyle C_{ijkl}} depend upon thecrystal structure of the material: in the general case, due to symmetric nature ofσ{\displaystyle \sigma } andε{\displaystyle \varepsilon }, the elastic tensor consists of 21 independent elastic coefficients.[4] This number can be further reduced by the symmetry of the material: 9 for anorthorhombic crystal, 5 for anhexagonal structure, and 3 for acubic symmetry.[5] Finally, for anisotropic material, there are only two independent parameters, withCijkl=λδijδkl+μ(δikδjl+δilδjk){\displaystyle C_{ijkl}=\lambda \delta _{ij}\delta _{kl}+\mu \left(\delta _{ik}\delta _{jl}+\delta _{il}\delta _{jk}\right)}, whereλ{\displaystyle \lambda } andμ{\displaystyle \mu } are theLamé constants, andδij{\displaystyle \delta _{ij}} is theKronecker delta.

The strain tensor itself can be defined to reflect distortion in any way that results in invariance under total rotation, but the most common definition with regard to which elastic tensors are usually expressed defines strain as the symmetric part of the gradient of displacement with all nonlinear terms suppressed:εij=12(iuj+jui){\displaystyle \varepsilon _{ij}={\frac {1}{2}}\left(\partial _{i}u_{j}+\partial _{j}u_{i}\right)}whereui{\displaystyle u_{i}} is the displacement at a point in thei{\displaystyle i}-th direction andj{\displaystyle \partial _{j}} is the partial derivative in thej{\displaystyle j}-th direction. Note that:εjj=juj{\displaystyle \varepsilon _{jj}=\partial _{j}u_{j}}where no summation is intended. Although full Einstein notation sums over raised and lowered pairs of indices, the values of elastic and strain tensor components are usually expressed with all indices lowered. Thus beware (as here) that in some contexts a repeated index does not imply a sum overvalues of that index (j{\displaystyle j} in this case), but merely a single component of a tensor.

See also

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References

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  1. ^abLandau, L.D.;Lifshitz, E. M. (1986).Theory of Elasticity (3rd ed.). Oxford, England: Butterworth Heinemann.ISBN 0-7506-2633-X.
  2. ^Maxwell, J.C. (1888). Peter Pesic (ed.).Theory of Heat (9th ed.). Mineola, N.Y.: Dover Publications Inc.ISBN 0-486-41735-2.{{cite book}}:ISBN / Date incompatibility (help)
  3. ^Dove, Martin T. (2003).Structure and dynamics: an atomic view of materials. Oxford: Oxford University Press.ISBN 0-19-850677-5.OCLC 50022684.
  4. ^Nye, J. F. (1985).Physical properties of crystals: their representation by tensors and matrices (1st published in pbk. with corrections, 1985 ed.). Oxford [Oxfordshire]: Clarendon Press.ISBN 0-19-851165-5.OCLC 11114089.
  5. ^Mouhat, Félix; Coudert, François-Xavier (2014-12-05). "Necessary and sufficient elastic stability conditions in various crystal systems".Physical Review B.90 (22) 224104.arXiv:1410.0065.Bibcode:2014PhRvB..90v4104M.doi:10.1103/PhysRevB.90.224104.ISSN 1098-0121.S2CID 54058316.

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