Abstract
Equations have been derived to solve the inverse problem of reconstructing the Fourier expansion coefficients for the temperature of a medium as a function of coordinate along elementary layers. These coefficients are reconstructed from the known similar expansion coefficients for the thermal energy flux at the diffraction grating output as a function of the grating displacement along the medium surface. The grating is in the inhomogeneous wave zone.
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More From: Bulletin of the Russian Academy of Sciences: Physics
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