At a perfectly bonded elastic interface without an interfacial force, displacement and traction are continuous:
Tangential derivatives of the common displacement trace are also continuous. Thus the jump of a piecewise constant displacement gradient tensor annihilates every tangential vector, and has the form . Taking its symmetric part shows that the strain jump is , where
The adjoint formula follows from for symmetric stress tensors. Tangential-tangential strain components are therefore common to all layers. Conversely, such gradient jumps can be realized by continuous piecewise affine displacement in the layered geometry.
Take positive elastic stiffness tensors with their usual minor and major symmetries, and a positive comparison elastic stiffness tensor . A fictitious layer can have the same tangential displacement derivatives and the same traction as the physical layers. Hence . The common traction condition gives
where is the positive acoustic tensor, with components . Solving for gives
Expanding the two occurrences of gives exactly the symmetrization over and in the directional elastic strain Green operator specified in the paper.
For any two layers, the inverse identity for their acoustic tensors proves the required resolvent relation without interchanging noncommuting tensors:
With , this identity also gives . Therefore
These finite-dimensional operators are inverses. Define . Then , and averaging strains and stresses gives
Eliminating the fictitious strain yields
All products have the displayed order; the elastic stiffness tensors need not commute.
It remains to justify the inverse and comparison independence. Consider two compatible equilibrated layer solutions with the same mean strain. Their difference has zero common tangential-tangential strain, so , with because is injective and the mean difference is zero. Their traction difference is one common vector . Therefore
Positive elastic energy forces every to vanish. In particular, if , all physical layer strains vanish. Their common tangential components then force , and their zero traction gives . Hence , proving that is invertible. Finally, every positive choice of constructs the unique layer solution for the same . Its averaged stress is unique, so the displayed effective stiffness is independent of the fictitious comparison material. This is the exact layered constitutive response, rather than a claim that piecewise constant fields meet arbitrary finite-body boundary data.
An elastic deformation is reversible: after removal of the deforming loads the material returns to its reference state, and its instantaneous stress is determined by its current deformation rather than a plastic or viscous history. In the infinitesimal approximation the displacement field gives the infinitesimal strain tensor . The Cauchy stress tensor is defined by traction on a plane of unit normal ; absence of body couples makes .
Let be the recoverable elastic energy per unit mass. The local mechanical power per unit volume is
because the symmetric Cauchy stress tensor annihilates the antisymmetric part of the velocity gradient. Conservation of energy during the deformation gives . Since for arbitrary symmetric strain rates,
Here the derivative is the gradient on the space of symmetric tensors, with the double-contraction inner product. This convention accounts for the two occurrences of each off-diagonal entry; treating six independent coordinates without their corresponding factors would give an erroneous factor of two in shear components.
Take a stress-free reference state of mass density . The Taylor series of the elastic energy starts quadratically:
Using gives , the relation of linear elasticity. If the reference state has initial stress, the first-order expansion also retains that constant stress. Symmetry of stress and strain gives the minor symmetries , while equality of the mixed second derivatives of elastic energy gives the major symmetry . Thus the elastic stiffness tensor is a symmetric map on a six-dimensional strain space: there are independent coefficients.
For twofold elastic symmetry, choose the symmetry axis as . Rotation through is , and transforms the infinitesimal strain tensor into . Components are even and are odd. Invariance of elastic energy excludes every coupling between these parity classes. In the engineering strain ordering , with corresponding stress ordering , the symmetric stiffness matrix has the form
Its symmetric even block has ten independent entries and its symmetric odd block has three. Hence a twofold axis leaves independent coefficients. No invariance under other rotation angles has been assumed.
Let be the solid exterior to the cavity, and choose outward from the solid, hence into the cavity on its boundary . Subtraction of the incident solution from the total solution gives the scattered displacement field equations
The traction-free cavity condition for the total field gives on . The scattered field has zero initial displacement and initial velocity before the pulse reaches the cavity and satisfies an outgoing radiation condition, excluding an additional incoming elastic wave. Equivalently one seeks the causal response to this prescribed boundary traction. Although the incident plane pulse extends across an infinite plane, the causal scattered field from the bounded cavity has finite propagation distance at each finite time.
To prove energy uniqueness for traction-driven elasticity, take the difference of two solutions with the same initial conditions, body force, boundary traction and outgoing condition. It satisfies
For a large enclosing ball , multiply by and integrate over . Integration by parts gives
Symmetry of stress replaces the last derivative by , and major symmetry of the elastic stiffness tensor makes that integral the derivative of the strain energy. Therefore
The cavity contribution is zero. On any fixed finite time interval choose beyond the causal support of the scattered difference; the outer contribution is then zero as well. This gives conservation of its nonnegative elastic energy. Positive mass density and positive strain energy imply that zero initial energy forces everywhere; the zero initial displacement field then gives . The same argument works for finite-energy outgoing solutions by taking the limit of enclosing surfaces and excluding incoming energy. Hence the causal scattered field is unique. Specifying the incident field and cavity traction alone without the initial and outgoing conditions would not establish uniqueness.
Use the material-first nominal stress tensor convention , whose reference-volume power is . At a regular constraint point, , all admissible deformation rates satisfy . Equality of mechanical power and the derivative of the strain energy density gives
for every vector in this eight-dimensional tangent hyperplane. Its orthogonal complement is the span of . Consequently the constraint reaction in hyperelastic stress is
The scalar Lagrange multiplier is not determined by the work identity: its contribution vanishes on every allowed rate. Regularity matters. For example, replacing a regular incompressibility constraint by would give zero gradient on the same admissible set and could not represent an arbitrary pressure reaction through that gradient.
For incompressibility use the regular function , with . Differentiating the alternating-tensor expression for gives
The first expression is the cofactor entry; contracting it with gives , proving the inverse formula. On this yields
With this plus-sign convention is the negative of the usual pressure multiplier.
For an equibiaxially stretched sheet, incompressibility requires the principal stretches . The printed sheet expression's is inconsistent with this constraint and must be ; the balloon expression later on the same PDF page has the correct exponent. Let denote the derivative with respect to principal stretch , evaluated on this constrained path. With no applied thickness-direction traction,
Isotropy gives at equal in-plane stretches. Hence
The equibiaxial nominal tension of an incompressible sheet is therefore
The two equal in-plane nominal tensions do work per reference volume; the thickness-direction nominal stress does no work because it is zero. That is exactly the constrained energy differential, explaining energy conservation. As a check that the printed exponent is a genuine error, a neo-Hookean solid gives , zero at the undeformed state. The derivative with the erroneous exponent would instead give at that state.
For the thin spherical balloon, use the leading reference shell volume . Its two tangential stretches are , while its thickness stretch is and its current thickness is . Define . Its total elastic energy at leading thin-shell order is
During a quasistatic increment , the enclosed volume changes by , and . Equating energy change to work of the internal excess pressure gives
This is the inflation pressure of a thin incompressible elastic balloon. The approximation neglects through-thickness variation and curvature corrections beyond leading order, and requires . It also agrees with membrane force balance: , , and . Here pressure is force per current area, while is force per reference area; confusing them would lose a factor of .
Retain , but normalize the complex potential as , so that . The Cauchy-Riemann equations give and . Since , the two stresses satisfy
Using the same unscaled from part (a) would instead put an additional on its derivative; the potential normalization matters.
Take the principal branch of , with its branch cut along the negative real axis and positive for . Write . For the antisymmetric crack-opening response, reflection gives on the faces. The prescribed equal face stress gives . Multiplication by the square-root factor converts this face condition to an additive jump. In fact, with and ,
The Sokhotski–Plemelj theorem applied to this jump gives
where is entire after imposing the usual finite-energy crack-tip regularity. This is the Hilbert problem for an antiplane crack, with the stress-potential phase chosen explicitly above.
For localized face loading with no additional remote loading, the far displacement is bounded and the weighted Cauchy transform decays. In particular, for compactly supported loading, at infinity and Liouville theorem sets . The resulting Cauchy solution for a steadily moving semi-infinite antiplane crack is
Integrals and boundary values are understood for loadings with the corresponding convergence and regularity, or as limits of localized loading. The reflection used above is the pure antiplane opening response: reflection with a sign change of displacement leaves both prescribed face stresses unchanged, and the usual no-extra-load uniqueness condition eliminates an unforced symmetric addition.
One can check the face stresses directly. Put . The Cauchy boundary limits give
Both have , verifying the prescribed traction and its sign on both faces. The opposite real parts also give the required reflection. Ahead of the tip, the integral is real and is purely imaginary, so the bonded line has zero tangential displacement gradient and the two halves match.
For , take in the boxed analytic solution. The ahead-of-tip stress is
No appears: at fixed co-moving position and the specified co-moving face loading, this stress is independent of the speed. The displacement, however, still scales with , so speed independence does not apply to the whole elastic field. If is finite, the near-tip stress is inverse-square-root with coefficient .
The far-field condition is a genuine uniqueness requirement. A homogeneous stress-intensity field of a semi-infinite antiplane crack has , for real . It adds no face traction but changes the stress ahead by . Although its stress tends to zero at infinity, its primitive is , which gives unbounded remote displacement and infinite total elastic energy. Thus only asking for stress to vanish at infinity would leave the homogeneous constant undetermined; excluding that added remote stress-intensity loading selects the displayed face-loaded solution. The ordinary inverse-square-root tip singularity itself has finite energy in a bounded neighbourhood and is not being excluded.
Use orthonormal cylindrical bases in the reference and deformed configurations. The radial coordinate remains , the angular coordinate becomes , and the axial coordinate is unchanged. Removing the rotation of the cylindrical basis, the deformation gradient is
It is a local simple shear with unit determinant. The squared principal stretches are the eigenvalues of
One principal stretch is one. The remaining squared principal stretches have product one and sum . Consequently they can be written and , where
For negative their ordering reverses, which is immaterial to the strain energy density of an isotropic material.
Let the reference length be . By material isotropy, the total elastic energy and end rotation are
For a quasistatic change, incompressibility makes the constraint reaction do no work. The velocity on an end section is its rigid rotational velocity; its traction power is the resultant torque times the angular velocity. Thus conservation of energy, or equivalently the torque and axial force of a twisted incompressible cylinder work identity, gives and
The radius is fixed in this derivative. This argument computes the required end torque along the prescribed deformation family; proving that a suitable end-only traction distribution sustains that family is unnecessary here.
For a neo-Hookean solid, the identity gives . Therefore
This is the signed torque in the twist direction; its magnitude is . For the positive twist convention the signed value equals the magnitude.
Put , the seismic impedance. In a uniform medium, define and . The field equations give
Thus and , with arbitrary independent profiles . Reconstruction gives
The two characteristic components therefore have , and , .
The kinetic plus elastic energy mass density is . Multiplying the equations by and yields . Hence the elastic-wave energy flux is . For a pure forward wave ; for a pure backward wave . In the mixture the cross terms cancel, giving . Strict sign holds for nonzero components.
If two harmonic solutions have the same body force and prescribed boundary traction, their difference has no body force and is traction-free. A nonzero difference would therefore be a free eigenfunction at that frequency. For any frequency outside the countable exceptional set found above, the difference must vanish, so the forced boundary-value solution, when it exists, is unique. At an eigenfrequency, a free eigenfunction can be added to any existing solution, and a resonant forcing may fail to admit a steady harmonic response. This distinguishes uniqueness from existence.
For the full time-dependent problem, let be the difference between two fields with identical forces, tractions and initial displacement field and velocity. It obeys , zero boundary traction, and zero initial data. Its energy uniqueness for traction-driven elasticity follows by direct integration:
Multiply the equation by and integrate by parts. Major symmetry turns the strain term into the derivative of elastic energy, giving . Stable elasticity makes , and gives . Thus equals its initial value zero. Even rigid zero-strain motions cannot survive these initial conditions.
The PDF correctly specifies zero initial displacement field and zero initial velocity; the TeX duplicates displacement field in the second condition. The complete causal displacement field is unique, including when its Fourier representation contains resonant modal contributions fixed by the initial data.
Put , the filament bending modulus in the easier bending direction; is the relevant second moment of area. Take filament tension as positive in extension. A cut at height supports the weight of the material above it, so its axial force is compressive:
The small transverse displacement induces a transverse tension force density , while bending produces . Their balance gives
The same result follows from elastic energy and gravitational energy. To quadratic order, local inextensibility shortens the height of the material point labelled by . Integrating its weight and interchanging the integrals gives the second-order potential energy
Two integration by parts steps in its first variation give
The clamped boundary conditions fix displacement and slope at the base, and the unconstrained tip must have zero bending moment and transverse end force. Thus the complete four conditions are
Since the filament tension vanishes at the tip, the last condition is . Integrate the ordinary differential equation once: is constant, and its tip value makes that constant zero. For the slope , it follows that
The other tip condition already follows from this equation for a regular solution; it is not a third independent condition on the second-order slope problem. Finally reconstruct to impose the base position.
Set , , and . Then and , so becomes
Substituting gives
This is the Bessel differential equation of order , whose two independent Bessel functions of the first kind give
The tip is . To decide which branch is admissible, retain both leading behaviours, not just the fact that stays finite:
Since and , the first branch has zero tip derivative, while the second has a nonzero tip derivative. The moment-free condition therefore sets , and it does not require the tip slope itself to vanish. The base condition now requires
Let be the first positive zero. The Bessel threshold for self-buckling of a vertical rod is
To identify this as the first loss of stability, write the quadratic energy in terms of the slope as . On functions with , its critical coefficient is the minimum Rayleigh quotient ; variation supplies the moment-free condition at the tip and the same Sturm-Liouville problem. The first zero gives the lowest eigenvalue, so the straight state is stable below this load, neutral at it, and unstable above it, with the easier direction buckling first.
For one small transverse displacement, the elastic energy of the elastic filament is
where is the filament bending modulus. Its first variation is
The clamped boundary conditions remove the left boundary terms. A force-free and torque-free tip permits independent and , so the natural boundary conditions for a free endpoint are : zero bending moment and transverse shear.
There is an important distinction between an energy minimum and a normal mode. The unloaded higher-order Euler-Lagrange equation is , whose only solution with these four boundary conditions is . A general fluctuating shape is a sum of modes, not one of the stated sinusoidal/hyperbolic functions. To obtain the clamped--free bending modes, extremize the bending Rayleigh quotient, or equivalently with a fixed norm. Its Euler-Lagrange equation is
This is the constrained variational characterization of bending modes. Its four characteristic roots are . Clamping gives and , hence
The free-tip conditions reduce to
Its determinant is , so nontrivial modes require
No zero mode exists, since a cubic satisfying the homogeneous clamp/free conditions is zero. The clamped-free bending spectrum starts with ; bisection or Newton iteration gives , so . Choosing and gives
The second boundary condition follows from the root equation, and is arbitrary until a normalization is chosen.
The bending operator with these boundary conditions is positive and self-adjoint. Twice integrating by parts gives
Symmetry implies orthogonality when . Expand and use . Then
by the equipartition theorem. The supplied endpoint identity therefore yields the thermal bending fluctuations of a clamped filament:
To evaluate the sum, apply a tip force and minimize . The modified free-end conditions are and , and in the interior. Integration gives , so the tip-force compliance of a cantilever is . On the other hand, minimizing the modal energy minus gives and hence
Comparison evaluates the fourth inverse-power sum of the cantilever spectrum without truncating the modes:
The boxed variance is for the specified single transverse direction. An independent equilibrium check follows by differentiating the Gaussian partition function with respect to : at zero load, reproducing the same result from the static compliance. Keeping only the first normal mode gives about , roughly of the exact variance. With two independent equivalent transverse directions, their summed variance is twice the boxed result. The small-slope model requires , or small compared with the usual three-dimensional persistence length .
The arclength element is . For uniformly small slopes, the Taylor expansion gives
Thus to quadratic order in the slopes the excess length is . This is the small-slope approximation used in the subsequent elastic energy.
Vary by , where the clamped endpoint conditions require at both endpoints. The first variation of the quadratic elastic energy is
Both integrations by parts have zero boundary terms. Since the variation is arbitrary in the interior, the fundamental lemma of the calculus of variations gives the Euler-Lagrange equation. Varying independently gives the second equation:
The clamped endpoint values accompany these equations. If or depends on , it must remain inside the derivatives.
With unit constant bending coefficients and unit length, the quadratic elastic energy is
To find the first loss of positivity, put . The clamped conditions give and . Extend periodically with period one. The sharp periodic Wirtinger inequality gives . For completeness, expand the mean-zero periodic in its Fourier series . Parseval identity gives
which proves the inequality and its equality condition. The same holds for . Consequently
For , the straight filament is the unique minimum. Equality in the periodic Wirtinger inequality has ; the endpoint value eliminates . Integration and the position boundary conditions therefore give the first buckling load and modes:
At this load every such pair has zero quadratic elastic energy and solves the Euler-Lagrange equations. For these modes give negative energy, signaling instability of the straight configuration. The quadratic small-slope model does not select a finite post-buckling amplitude; nonlinear terms would be needed for that. This is Euler buckling of an elastic filament.
A faceted, approximately equiaxed crystal is indicated. A truncated octahedron bounded by low-energy and facets is a plausible three-dimensional shape for an fcc metal particle; the hexagonal section alone does not uniquely distinguish it from other faceted polyhedra.
The Wulff construction minimizes at fixed particle volume. Place a plane with normal a distance from a common centre and take the inner envelope. Low-surface-energy orientations survive as large facets. Annealing permits diffusion toward this equilibrium morphology, provided the time is sufficient. For a supported or strained alloy, substrate adhesion and elastic energy modify this simple free-particle construction.
stress describes internal force per area. A cut with unit normal has traction ; its normal component is and its remainder is shear traction. force balance constrains the stress divergence, while ordinary local angular-momentum balance makes the Cauchy stress tensor symmetric in a medium without body couples.
strain describes deformation rather than force. For small displacement gradients,
The antisymmetric displacement-gradient part is a rigid rotation to first order and contributes no infinitesimal strain. Engineering shear strain is , so it must not be confused with the tensor component. stress has units of pressure; strain is dimensionless.
An isotropic linear elastic solid obeys
Two independent moduli are required. The shear modulus and bulk modulus must be positive for stability. Young's modulus and Poisson ratio satisfy
For a tensile specimen with free side faces, gives and . Pure shear gives ; hydrostatic loading gives . The incompressible limit has at finite shear stiffness, not vanishing shear resistance. Crystals can be anisotropic and need a fourth-rank elastic stiffness tensor instead of the isotropic two-constant law.
elastic deformation is recoverable on unloading; it need not remain linear at large strain. Beyond yield, irreversible rearrangements such as dislocation motion cause plastic strain, often followed by hardening. Ductile samples can neck before fracture; brittle failure has much less plastic deformation. Engineering stress uses initial area, while true stress uses the changing instantaneous area. A decreasing engineering stress during necking therefore need not mean that local true stress decreases. stress concentrations, flaws and loading geometry can determine failure before a uniform-material strength is reached. Viscoelastic materials also show rate dependence, creep and stress relaxation; their losses cannot be described by a static Hooke law alone.
A tensile test should measure force and gauge-length extension independently, correct machine compliance, align the grips, and control strain rate and temperature. Unloading distinguishes recoverable strain from a residual plastic extension. Separate shear or hydrostatic tests determine moduli that one axial measurement does not fix. Compression specimens need friction and buckling checks. Work per volume is ; the recoverable part is elastic energy, while a dissipative cycle produces a loss rather than creating energy. The original loading/unloading curve below is a chosen constitutive sketch, not measured material data.
Figure 1. . Small-strain geometry and illustrative unloading. Details.
The torque rises linearly with elastic twist, so the stored elastic energy is the work integral
Using the transmitted torque and end twist,
This is energy associated with deformation, distinct from the much larger kinetic energy of the whole spinning shaft.
For a slender elastic beam undergoing small bending, assume plane cross-sections remain plane and normal to the neutral axis. Fibres a signed distance from that axis have longitudinal strain , where is the local radius of curvature. Hooke's law gives stress , where is Young's modulus. Zero resultant axial force places the neutral axis through the section's centroid for a homogeneous beam.
The bending moment is the moment of this stress distribution. Its magnitude is
The second moment of area has units , and the bending stiffness has units . A rectangular section of width and depth has , so placing more material far from the neutral axis strongly resists bending. This is the purpose of an I-section.
For small deflection , the signed curvature is approximately . A consistent variational sign convention follows from the elastic energy and a transverse load :
For constant bending stiffness this is the Euler-Bernoulli beam equation . A clamped end fixes ; a simply supported end has and zero bending moment; an unloaded free end has zero moment and shear, for uniform . Endpoint loads replace the corresponding zero-force boundary conditions.
For a cantilever of length carrying a tip force , choose positive deflection along . The internal bending gives , with . Two integrations give
This approximation requires small slopes, elastic strains and a length large compared with section dimensions. Shear deformation, rotary inertia, plastic yielding and large rotations require extensions. Adding inertia gives flexural waves with for a uniform beam, where is mass per unit length.
An element with unperturbed coordinate length has mass and transverse speed squared . Its actual length is
At fixed tension the extra elastic energy to this order is . Subtracting it from the kinetic energy gives
Here prime means and dot means . The approximation retains quadratic transverse energy and neglects higher-order slope effects and longitudinal motion. The resulting field equations are for , with wave speed when .
Interpret as the small transverse displacement of the elastic beam. The first term is the positive kinetic energy density , with the mass per unit length. The Lagrangian density is kinetic minus potential energy, so the potential density encoded by the other two terms is
For a compressed rod, transverse deflection releases compression energy: the small-slope geometric change in length is proportional to , so the applied compressive load lowers the potential by . This explains the positive sign of the term in the Lagrangian. Tension would give the opposite sign and a restoring gradient term.
Bending costs elastic energy. At small slopes the curvature is , so positive bending stiffness gives potential , and hence a negative term in the Lagrangian. For a uniform slender beam is its flexural rigidity. The competition between destabilizing compression and stabilizing bending is responsible for Euler buckling of an elastic filament.
Effective stress and frictional strength generally increase with depth through the shallow crust undergoing brittle fracture. At , small overburden and often weak, fractured near-surface materials limit the shear stress and elastic energy that can accumulate. Some shallow materials also undergo stable sliding rather than unstable earthquake nucleation. Near , a locked fault prone to brittle fracture can sustain a much larger differential stress before frictional instability releases stored elastic energy.
This depth is plausibly near the lower, strong part of the seismogenic layer: below it, increasing temperature eventually promotes material creep across the brittle-ductile transition. Once nucleated at depth, a dynamic finite-source rupture can propagate into shallow regions that could not independently nucleate the same event. Depth alone does not determine the nucleation point: local pore pressure, frictional stability and stress heterogeneity also matter.