On the construction of general solutions of the theory of the elasticity of inhomogeneous solids
The elasticity theory equations are decomposed in the case when the shear modulus is a function of one Cartesian coordinate while Poisson's ratio is a function of three coordinates. Such a separation is possible for transverse isotropy when both shear coefficients depend just on the coordinates of the normal isotropy plane. It is assumed that the mass forces are potential.
scientific article; zbMATH DE number 56421