Large Deformation Constitutive Laws for Isotropic Thermoelastic Materials
Author(s) -
Bradley J. Plohr,
JeeYeon Plohr
Publication year - 2012
Publication title -
osti oai (u.s. department of energy office of scientific and technical information)
Language(s) - English
Resource type - Reports
DOI - 10.2172/1047120
Subject(s) - thermoelastic damping , cauchy elastic material , constitutive equation , strain energy density function , isotropy , cauchy stress tensor , infinitesimal strain theory , simple shear , classical mechanics , hooke's law , finite strain theory , deformation (meteorology) , shear (geology) , second law of thermodynamics , elasticity (physics) , mathematical analysis , mechanics , shear stress , mathematics , physics , materials science , thermodynamics , thermal , finite element method , quantum mechanics , meteorology , composite material
We examine the approximations made in using Hooke's law as a constitutive relation for an isotropic thermoelastic material subjected to large deformation. For a general thermoelastic material, we employ the volume-preserving part of the deformation gradient to facilitate volumetric/shear strain decompositions of the free energy, its first derivatives (the Cauchy stress and entropy), and its second derivatives (the specific heat, Gruneisen tensor, and elasticity tensor). Specializing to isotropic materials, we calculate these constitutive quantities more explicitly. For deformations with limited shear strain, but possibly large changes in volume, we show that the differential equations for the stress involve new terms in addition to the traditional Hooke's law terms. These new terms are of the same order in the shear strain as the objective derivative terms needed for frame indifference; unless the latter terms are negligible, the former cannot be neglected. We also demonstrate that accounting for the new terms requires that the deformation gradient be included as a field variable.
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