Abstract
Let Ω ⊂ ℝ3 be a bounded domain which is taken to be the reference configuration or the rest state of a perfectly elastic body. Classically a deformation of the body, which in its rest position occupies the region Ω, is described by a smooth map u : \(\Omega\to \overset{\lower0.5em\hbox{$\smash{\scriptscriptstyle\frown}$}}{\Omega }\subset {\mathbb{R}^3}\) that is orientation preserving and globally invertible. According to our idealized situation of a perfectly elastic body no heat transfer occurs in the process of loading and unloading a perfectly elastic material, and such loading and unloading process is completely reversible. Therefore it is reasonable to assume that all mechanical properties of a perfectly elastic material are characterized by a stored energy function W(x, G),which depends on the infinitesimal deformations G = Du(x), and that in terms of it the total internal energy stored by the body which undergo the deformation u is given by
Materials whose mechanical properties are characterized by a stored energy functions are often called hyperelastic materials.
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© 1998 Springer-Verlag Berlin Heidelberg
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Giaquinta, M., Modica, G., Souček, J. (1998). Finite Elasticity and Weak Diffeomorphisms. In: Cartesian Currents in the Calculus of Variations II. Ergebnisse der Mathematik und ihrer Grenzgebiete / 3. Folge. A Series of Modern Surveys in Mathematics, vol 38. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-662-06218-0_2
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DOI: https://doi.org/10.1007/978-3-662-06218-0_2
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