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Exact plane-wave solutions of the isotropic linear elastic model, with longitudinal and transverse speeds
Statement
Let and Lam'e parameters with and , let and , and define the plane wave
with the Euclidean inner product (The Euclidean inner product on ). For each fixed , the spatial displacement map is . Define the strain and stress fields using the spatial derivative at fixed time:
These are the pointwise constitutive formulas of the isotropic linear elastic model (The small-strain isotropic linear elastic constitutive law and its strain energy); in particular is the total derivative of , not the derivative of the full spacetime map.
Then the componentwise identity
holds on all of if and only if
When (D) holds and are nonzero, define the phase speed by . If for some (longitudinal polarization), then and . If (transverse polarization), then and . The constitutive positivity hypotheses imply and , so both branch phase speeds are real and positive. (When , (D) has no solution with and .)
Facts & Assumptions
Given: The parameters , the vectors , the frequency , and the field as constructed.
Sine and cosine have the usual derivatives, , , and , ; compositions with affine maps are differentiable by the chain rule (The derivatives of sine and cosine are cosine and minus sine, Sine and cosine defined by their real power series, The chain rule for total derivatives: , Sums, scalar multiples, products and quotients: , , , and when , A total derivative computes every directional derivative, and its matrix is the Jacobian, Euclidean maps and diffeomorphisms).
The strain and stress are computed from the partial derivatives of as in the constitutive definition; and the identity matrix are those of The trace as the sum of the diagonal entries and Rectangular matrix multiplication and the identity matrix , including zero-sized shapes (The small-strain isotropic linear elastic constitutive law and its strain energy, The vector space of by matrices over a field, with entrywise operations).
Proof
Put . Then and , so by [F1] and the chain rule
From step 1.1, and . Hence
Differentiate step 2.1 and use [F1]: where , and .
The identity for all reads, by steps 1.1 and 3.1, for all . Choosing , gives , so the bracket vanishes; conversely vanishing of the bracket makes the identity hold everywhere. This is exactly (D).
Assume (D) and . If with , then (D) reads , so . If , then (D) reads , so . Dividing by gives the phase-speed formulas. Positivity follows from and .
Remarks
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The theorem verifies exact solutions of the adopted constant-coefficient PDE; it does not assert that every solution of the elastic model is a plane wave, that a wave packet propagates unchanged, or that any material realises the model. General initial-value problems for the elastic system are not solved here.
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The identity (D) is the dispersion relation of the plane-wave ansatz. The two eigenvalue branches computed in the last step are the longitudinal and transverse speeds; they require and respectively, and no claim is made about alone.
Depends on
The small-strain isotropic linear elastic constitutive law and its strain energy
Euclidean spatial calculus: gradient, divergence and material derivative
Euclidean maps and diffeomorphisms
The Euclidean inner product on
A total derivative computes every directional derivative, and its matrix is the Jacobian
Sums, scalar multiples, products and quotients: , , , and when
The derivatives of sine and cosine are cosine and minus sine
Sine and cosine defined by their real power series
The vector space of by matrices over a field, with entrywise operations
Rectangular matrix multiplication and the identity matrix , including zero-sized shapes
The trace as the sum of the diagonal entries
The chain rule for total derivatives:
Dependency tree · 2 levels
Sources
- R. Abeyaratne, Continuum Mechanics, Volume II of Lecture Notes on the Mechanics of Solids (MIT, 1988, revised 2020), Section 11.2 (the isotropic linearized elastic field equations)
- K. Likharev, Essential Graduate Physics, Classical Mechanics (September 1, 2026 complete volume), Section 7.7 (3D acoustic waves: plane longitudinal and transverse waves and their speeds)