For a homogeneous comparison elastic stiffness tensor , the elastic strain Green operator maps an elastic polarization to minus the induced infinitesimal strain tensor. In a bounded domain the induced displacement field has zero boundary data; in an infinite medium it is the decaying perturbation. The defining static elastic equilibrium equation is . The bounded-domain operator is self-adjoint, annihilates constant elastic polarizations, has zero mean output, and satisfies .
For a three-dimensional isotropic comparison material, the contraction of its elastic strain Green operator is the displayed distributional derivative. Its double trace is , because . Away from zero the contraction is ; the full distribution also includes . This contact term must not be discarded when computing hydrostatic strain.
When only the bulk modulus differs from an isotropic matrix, the elastic polarization is spherical: . The double trace of the isotropic elastic strain Green kernel makes the trace equation local, giving the displayed formula. Individual strain components still depend on a nonlocal potential of the spherical polarization, so the complete infinitesimal strain tensor is not generally a local multiple of its reference value.
Let ; its adjoint on symmetric stress tensors is . Then is the acoustic tensor. The directional elastic strain Green operator satisfies the resolvent identity , by the elementary inverse identity .
The elastic polarization is the excess stress relative to a homogeneous comparison elastic stiffness tensor. In heterogeneous linear elasticity, . The comparison static elastic equilibrium equation gives the integral equation , where is the reference strain under the same external loading.

Articles by others on the same topic (0)

There are currently no matching articles.