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.
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