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Linearly elastic solids have molecules envisaged as being locked together by springlike elastic forces.
Good examples of composite products are glass-fibre reinforced plastics, for use as tough elastic solids, and thick-film conductor, resistor, and dielectric pastes with tailored electrical properties for the packaging of microcircuits.
Poisson, Cauchy, and George G. Stokes showed that the equations of the general theory of elasticity predicted the existence of two types of elastic deformation waves which could propagate through isotropic elastic solids.
Under greater deformation, such elastic solids exhibit either brittleness (in which the internal elastic forces are broken down) or ductility (in which certain internal mechanisms permit shearing displacements to occur within the atomic structure).
These are fluids in the sense that they cannot long support shear stress, but at the same time they have remarkable properties like those of finitely deformed elastic solids.
The German physicist Heinrich Rudolf Hertz developed solutions for the deformation of elastic solids as they are brought into contact and applied these to model details of impact collisions.
For example, rocks, which may be effectively characterized as elastic solids for normal engineering purposes, would have to be reclassified as viscoelastic solids in geologic studies in which the time scale may be millions of years.
Some of them are nonsimple elastic solids.
All of the studies cited above assumed the adhesive layers are elastic solids because solidified adhesive layers closely resemble elastic solids.
Both Au and polymer are modeled as homogenous and elastic solids.
The theory of micromorphic elastic solids was first elaborated by Eringen (see, for instance, [1]).
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