Original solutions to the paper released at the source request. The complete editable transcription is retained in the private examination archive.
The displacement follows a material point from its reference position to its current position:
The deformation gradient is the Jacobian matrix , and the volume Jacobian is
For an orientation-preserving physical deformation, measures the local volume expansion factor. Incompressibility requires ; conservation of mass gives . For small displacement gradients, . If a spatial representation is desired, the same displacement is .
A Cartesian Cartesian second-rank tensor has components transforming under a constant orthogonal change of axes as
Here and . By the chain rule and orthogonality,
Thus the displacement gradient is a Cartesian second-rank tensor. Its symmetric part transforms in the same way:
Hence the infinitesimal strain tensor is also second-rank. This is a passive coordinate rotation, under which both reference and spatial coordinates rotate; it does not assert finite-deformation frame indifference of the linearized strain formula.
The traction on the oriented solid element is
With constant Lamé coefficients and derivatives in the reference variables,
Substitution into balance of linear momentum gives
To check the vector identity componentwise, contract the two alternating tensors:
Rearranging proves . Therefore
Assume . Dotting the decomposition with gives
Crossing it on the left by and using gives . Thus
Indeed , verifying the decomposition and the imposed transverse condition.
Apply the wave ansatz to the oscillatory displacement about a static body-force balance, or equivalently to the zero-body-force homogeneous equation. The parallel and perpendicular polarizations have speeds
The first is longitudinal and the second transverse. A wave family is dispersive when its phase speed varies with wavenumber. In each of these homogeneous bulk families, , so both are nondispersive and group and phase speeds coincide.
The positivity assumptions imply , hence . Therefore : longitudinal waves travel faster.
Substitution of gives
The oscillatory seam solution requires , giving
For an exponentially decaying exterior, with , so the same differential equation instead requires
The printed exterior plus sign is inconsistent with its decaying ansatz and must be a sign error. The guided mode has , so a slower shear-wave seam than its cladding is necessary.
For an even seam mode , upper-interface displacement and traction continuity give
The lower interface gives the same equations when . Eliminating the amplitudes yields
For an odd seam mode , the equations are
With the lower condition agrees, and elimination gives
These interface conditions together with the two corrected dispersion identities determine the guided-wave branches.
In the formal stiff-cladding limit with a nonvanishing exterior decay rate, the interface displacement tends to zero. The even seam mode then has , whereas the odd mode has . The positive wavenumbers are
The zero odd index would give an identically zero mode and is excluded. The smallest even transverse wavenumber is , so its lowest branch satisfies
This is the symmetric-mode cutoff: the actual limiting branches have the discrete listed values of . If the exterior shear speed remains finite, the separate decay requirement still applies; the cutoff alone does not replace that guided-wave condition.
Differentiate the displacement components. The shear strains involving vanish because and . The full infinitesimal strain tensor is
In particular . Substituting the Lamé coefficients into the constitutive law gives
For example : the thickness-direction strain supplies exactly the plane-stress Poisson correction. Also , confirming the off-diagonal factor.
Contract the tensors, counting both off-diagonal shear terms:
Since , integration gives
For the general midplane deflection, expand the energy density as . A variation gives
For clamped variations, on the boundary, so integrating twice transfers all derivatives to without a boundary contribution. The bulk coefficient is
Stationarity for all compactly supported variations and the fundamental lemma therefore give
Use the same first variation on the half-plane, with no restrictions on the edge traces of . Write . Two integrations of the term produce the boundary term at . The mixed term, after one integration in and one along the edge in , contributes . All other boundary terms vanish at infinity. Hence
The bulk equation makes its area term zero. Stationarity therefore gives exactly
The two edge traces can be prescribed independently: use with near zero and compactly supported smooth . The fundamental lemma on the edge then gives
They are zero bending moment and zero effective transverse shear at a free straight edge. The second includes the edge derivative of the twisting moment; omitting the mixed contribution would give the wrong coefficient.

Articles by others on the same topic (0)

There are currently no matching articles.