Write for the reference outer radius and for the current outer radius. The inner material normal is . A fluid pressure applies traction there, so the radial Cauchy stress tensor component must be negative:
The second condition uses zero external gauge pressure. Both faces also have zero shear traction; the axisymmetric diagonal stress field satisfies those conditions automatically. The axial constraint is plane strain, so supports may supply an axial reaction; it does not imply zero axial stress.
In the current configuration, balance of linear momentum is the Cauchy momentum equation
Here is the Cauchy stress tensor, is current mass density, is body force per unit mass, and is the velocity of the material particle currently at . The expression in parentheses is the material acceleration. The divergence is taken in current spatial coordinates, with .
Equivalently the right side is evaluated at the particle, because this is the same material acceleration in Lagrangian coordinates. For the subsequent static inflation with negligible body force, the equation reduces to .
Choose the outward unit normal to the boundary of the chosen current material subbody. The traction is the contact force exerted on that subbody per unit current area at the boundary point. Reversing the subbody side reverses and .
By Cauchy's stress theorem, the dependence on is linear. With the usual column-vector convention the Cauchy stress tensor satisfies
The same point has different traction vectors on differently oriented planes, but a single Cauchy stress tensor encodes all of them. In the absence of body couples, conservation of angular momentum makes symmetric.
The deformation gradient is the derivative of the deformation map with respect to the reference configuration coordinates, at fixed time:
Its determinant is the local ratio of current to reference volume: for an orientation-preserving deformation in continuum mechanics. Thus elastic incompressibility is the pointwise constraint , rather than a requirement that each individual principal stretch be one.
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.
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
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.
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.
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.
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.
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.
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
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 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 .
Insert the two constitutive stresses into the radial component of the Cauchy momentum equation. After collecting terms, , so . Its stresses are
The far pressure gives . At the tunnel wall, compressive bracing imposes , so . Hence
With no shear and , divide the yield identity by the nonzero to obtain . Solving its quadratic gives
To locate first yield, the stress-circle center is the constant , while its radius is . The radius is maximal at , so that is where it first meets the friction envelope as the bracing departs from the hydrostatic value. At the wall and ; hence and
For lowering bracing from , the hoop stress becomes more compressive, so and . Increasing bracing instead selects and reaches the other threshold . Stating the loading direction removes any ambiguity between the two reciprocal stress ratios. These conclusions describe first yield of the elastic field, not the later plastic-zone solution.
The Mohr circle has center on the normal-stress axis and radius . In the compressive regime , yield occurs when the circle first touches either friction line . The perpendicular distance of its center from either line is . Tangency therefore gives , or . But . Thus
The compressive sign restriction remains part of this equivalence: squaring alone would also produce algebraic branches that do not represent cohesionless compressive friction.
Figure 1.
Mohr-circle tangency to the cohesionless friction envelope in tension-positive coordinates
. Details.
For dry friction, the tangential contact force opposes sliding and has limiting magnitude , where is the compressive normal force and . Sticking requires ; impending sliding reaches equality.
The cohesionless Mohr-Coulomb failure criterion applies the same local condition on internal planes: yield begins when some plane has . In the tension-positive Cauchy convention used here, for a compressive plane, so
A cohesive material would add a positive intercept, but the later formulas in this paper are explicitly the zero-cohesion case. The model does not supply a tensile strength law.

Pinned article: Introduction to the OurBigBook Project

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