For plane strain in under surface normal traction and zero surface shear, use the forward Fourier transform phase . At , biharmonicity gives , whose decaying part is . Boundary traction fixes , , proving the displayed formula. Constitutive inversion and a decaying displacement mode give . Multiplication by produces an unambiguous displacement-gradient convolution kernel.
The zero mode is separate: a nonzero resultant load conflicts with an ordinary fully decaying displacement normalization in two dimensions and leads to a logarithmic reference issue. Balanced loading or a distributional/reference-displacement treatment is required before extending the transformed formulas globally. Dividing by and assigning a finite value at is invalid.
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