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A longitudinal plane wave in the isotropic elastic model: dispersion check and strain energy at explicit parameters
Example
Take , , (The small-strain isotropic linear elastic constitutive law and its strain energy: here ). Let , and
Then is a longitudinal plane wave with speed , and the associated strain and stress satisfy the elastic momentum identity; the strain energy density at time equals both and the decomposition with the same value.
Facts & Assumptions
Given: The parameters ; the vectors , , ; the field .
Plane-wave dispersion: the momentum identity holds for this ansatz exactly when ; for this is (Exact plane-wave solutions of the isotropic linear elastic model, with longitudinal and transverse speeds).
Strain and stress: and ; here has the single entry with , so , (Exact plane-wave solutions of the isotropic linear elastic model, with longitudinal and transverse speeds, The small-strain isotropic linear elastic constitutive law and its strain energy, A total derivative computes every directional derivative, and its matrix is the Jacobian, Euclidean spatial calculus: gradient, divergence and material derivative, The trace as the sum of the diagonal entries, The vector space of by matrices over a field, with entrywise operations).
Strain-energy decomposition: with and (The isotropic elastic strain energy is , hence positive definite under , ); trigonometric values and derivatives as usual (The derivatives of sine and cosine are cosine and minus sine, Sine and cosine defined by their real power series, Parity and the Pythagorean identity for sine and cosine).
Verification
Check the dispersion relation: , , and ; the relation of [L1] holds, so the ansatz solves the elastic momentum equation at these parameters.
Compute the strain energy directly: from [L2], , so .
Compute the decomposition: , so ; also . Then , in agreement with step 2.1.
Remarks
- The example is a finite parametric check of the theorem and of the energy identity; it does not show that every elastic solution is such a wave, and no material is identified with these Lamé parameters.
Depends on
Exact plane-wave solutions of the isotropic linear elastic model, with longitudinal and transverse speeds
The small-strain isotropic linear elastic constitutive law and its strain energy
The isotropic elastic strain energy is , hence positive definite under ,
Euclidean spatial calculus: gradient, divergence and material derivative
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
Parity and the Pythagorean identity for sine and cosine
The Euclidean inner product on
The vector space of by matrices over a field, with entrywise operations
The trace as the sum of the diagonal entries
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 (linearized elasticity and strain energy)
- K. Likharev, Essential Graduate Physics, Classical Mechanics (September 1, 2026 complete volume), Section 7.7 (plane longitudinal and transverse elastic waves and their speeds)