Source release: Oxford examination archive release thread, Part C bundle pages 426–429. The cover identifies Solid Mechanics, Tuesday 7 June 2011, 9.30am–11.00am.
Answer availability checked on 28 October 2026: bounded searches of official Oxford sources by exact year, title, module and formal code found no advertised exact-paper answers. The 2020–21 Solid Mechanics course page lists an exam compilation covering 2011–2020, but does not advertise it as solutions; its linked resource could not be fetched in the bounded check. No later-year release policy was used to infer 2011 availability.
A homogeneous hyperelastic material has a strain energy density per unit reference volume depending on the deformation gradient, with no explicit dependence on the reference configuration. For orientation-preserving gradients , its first Piola-Kirchhoff stress tensor is the derivative:Equivalently the infinitesimal stored-energy change is . Reference and spatial indices are distinguished here by upper- and lowercase index letters.
The material symmetry group may be written . A volume-preserving relabelling convention restricts the candidate to ; the material isotropy criterion is the same. The material has material isotropy when , meaning for every proper rotation . If only rotational symmetries are included in the definition of the group, material isotropy means that group equals . This right-rotation invariance is distinct from material frame indifference, the left-rotation invariance .
The polar decomposition in continuum mechanics gives the unique factorizationswhere are positive-definite symmetric matrices. Their common positive eigenvalues are the principal stretches, equivalently the singular values of . They describe the local stretch magnitudes after separating out a rigid rotation.
Define the invariants by the characteristic polynomialBecause has positive eigenvalues , its invariants are the elementary symmetric functions in those eigenvalues:The Frobenius norm gives . Write . Since , its singular values are , soFinally . ThereforeThese identities also give and .
Take a singular value decomposition , with positive and . Such a choice is possible because . Left material frame indifference removes , and right material isotropy removes , giving .
Moreover is unchanged when the positive diagonal entries are permuted. Every permutation can be implemented by a signed permutation matrix of determinant one; the signs disappear in conjugating a diagonal matrix. Thus the energy depends only on the unordered principal stretches.
The three invariants determine precisely this unordered triple: the roots of are , and their positive square roots give the stretches. Consequently, on the set of admissible invariant triples, define to be . The preceding argument proves that this is well defined and thatNot every positive triple is realizable by three positive roots. Since the requested statement only asserts existence of a function on , extend arbitrarily on the nonrealizable triples; no choice there affects the formula for a deformation in continuum mechanics. Smooth invariant representations, where needed for differentiating the constitutive equation, are understood locally on the realizable set.
Retain the material frame indifference assumption used in part (c), in addition to material isotropy. Put , and . For this antiplane shear,The invariant identities give and . Hence the restriction of the strain energy density isAntiplane energy does not determine the full stress: the restriction gives one scalar energy along antiplane gradients. It does not determine the full stress derivative with respect to every entry of .
Indeed, using the isotropic hyperelastic stress invariant representation and differentiating the energy, with denoting the corresponding partial derivatives, givesUsing , the general objective isotropic Cauchy stress tensor isAll derivatives are evaluated at the current invariant triple. The extra terms generally remain nonzero on antiplane gradients, so the printed assertion that the full stress must be does not follow.
A stress-free, objective isotropic counterexample is the compressible neo-Hookean solid , with . Its derivative is , so on antiplane gradientsTake . Then but , whereas and . The diagonal entry would force , contradicting the shear entry. Thus this is not a matter of choosing the right scalar coefficient.
For the additional one-invariant constitutive assumption , the stronger formula does hold, withThis is a valid special case, rather than a consequence of material isotropy alone. For the general restricted energy, the shear entries are still fixed: and , since along . The full normal stress needs the constitutive information that the printed claim omits. If material isotropy alone is interpreted without material frame indifference, even the first reduction to needs that additional material frame indifference assumption.
In the classical smooth setting, a deformation in continuum mechanics is a sufficiently regular, injective map with . Injectivity excludes material interpenetration, and a positive determinant preserves orientation and local volume. We use regularity for these kinematics and additional differentiability where stress-divergence identities are applied.
Cauchy's stress theorem states that the contact force on an oriented surface element at a current point depends on the point and its unit normal, rather than on the shape of the chosen subbody. Thus the contact force on the boundary of a current subbody has the form . Static force balance, for a body force per unit current volume, isfor every subbody. A shrinking pillbox gives ; a shrinking tetrahedron then gives linear dependence on the normal, . Applying the divergence theorem and using arbitrary subbodies givesIf body force is specified per unit mass instead, replace by . Symmetry of follows additionally from conservation of angular momentum in the absence of body couples; it is not a consequence of force balance alone.
The surface element relation is Nanson's formula. The force on a corresponding pair of current and reference surface elements must agree:Therefore the first Piola-Kirchhoff stress tensor isIt measures force per reference area, with a current force direction and a reference normal direction.
In components, differentiate . The Piola identity says . One proof writes the cofactor matrix as ; differentiating in produces symmetric second derivatives contracted against antisymmetric epsilon symbols, hence zero. The chain rule consequently givessince . Thus, with the coordinate composition made explicit,The distinction between reference divergence and current divergence is essential to this identity.
For , and . Differentiating the spherically symmetric deformation givesFor an orientation-preserving spherically symmetric deformation with positive radius, and . The radial direction and its perpendicular plane are eigenspaces of this positive symmetric matrix, soAt a positive diagonal matrix , every diagonal rotation with two minus signs commutes with . The supplied equivariance relation therefore forces to be a diagonal matrix: each off-diagonal entry changes sign under one such rotation while stays fixed. Varying a positive diagonal entry shows that the diagonal entries of are . Permutation symmetry of implies when .
Choose a rotation whose first column is . Applying equivariance to now giveswith the derivatives evaluated at . Thus the stress has one radial and one repeated tangential principal value, independently of the choice of tangent basis.
The Green-Lagrange strain tensor has eigenvalues . Its Frobenius norm and trace are invariant under the orthogonal principal-axis change, soFor the homogeneous dilation , put . Then . Differentiating the energy through gives the second Piola-Kirchhoff stress tensor , and multiplication by gives the first Piola-Kirchhoff stress tensor. ThusThe normals of the reference and deformed spheres point in the same radial direction. As , the reference traction magnitude tends to zero, while the current traction magnitude tends to infinity, provided , as for physically stable Lamé parameters. The negative signs of the stress coefficients for indicate compression.
There is no contradiction: the current area is times the reference area, so the same force divided by the vanishing current area has the larger stress. Indeed . The limiting map at is not itself an admissible deformation in continuum mechanics; the statement concerns the approach through positive . A degenerate choice would not have the asserted growth without bound.
The displacement field is , and its gradient is . Linear elasticity expands about an undeformed stress-free reference state, taking with and external loads of the same small order. A rigid translation need not itself be small; it is the deformation gradient that controls the infinitesimal strain tensor.
For with , a Taylor series givesThe constant can be set to zero. The tensor is the elasticity tensor. Commutation of continuous mixed partial derivatives proves its major symmetry:Material frame indifference at a stress-free reference also makes the quadratic energy depend only on the infinitesimal strain tensor , leading to the usual minor symmetries after spatial and reference indices are identified.
In this scaling, an external force of order may be evaluated on the reference geometry: its change due to the order- displacement contributes only at order . Thus the leading forces are fixed dead loads. Likewise , and , so the Piola transformation gives . Hence Cauchy and first Piola stresses agree to linear order. This reasoning uses the usual small-load, stress-free linearization; an order-one prestress or leading follower-load effect requires a different expansion.
Let the boundary split into a displacement part and a traction part . The linearized stored elastic energy functional isIts corresponding total potential subtracts the work of fixed body and surface loads:The problem in the calculus of variations is to minimize among admissible displacements with on . For a stable quadratic elastic energy this is the usual energy minimization formulation. Its stationarity condition suffices to derive equilibrium.
Vary by , with on . Major symmetry combines the two differentiated quadratic terms, givingIntegration by parts, first with test functions compactly supported in the interior, gives . Then arbitrary traces on give the natural traction condition. The complete boundary value problem isFor a homogeneous hyperelastic material the elasticity tensor is constant. In isotropic linear elasticity the constitutive equation is , giving the familiar Navier-Cauchy equation .
Taking traces of the constitutive equation givesThe assumed finite limits of stress and strain make the right side bounded. Therefore , and the limiting strain satisfies . The permitted interchange of derivatives and limits gives . DefineThen the limit stress is . Passing to the limit in force balance and using givesThe pressure acts as the Lagrange multiplier enforcing the volume constraint. The differential equations determine it up to an additive constant, while a specified absolute limit stress can fix that constant.
Nonlinear elastic incompressibility is . Expanding the determinant for gives , so its first-order form is precisely . The volumetric energy term becomes increasingly expensive as grows, while the fixed positive leaves shear strain possible. Thus the infinite-bulk-stiffness limit is the incompressible limit of isotropic linear elasticity, with the same equilibrium operator as the steady Stokes equations.
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