Saturated isotropic magnetostrictive strain

ID: saturated-isotropic-magnetostrictive-strain

Consider a mechanically free isotropic model of a saturated ferromagnet, at fixed temperature and fixed magnitude of magnetization. Let be a unit vector, where is the saturation magnetization. The magnetostrictive strain is an infinitesimal strain tensor, measured relative to a reference with randomly oriented magnetic domains. This reference convention matters: it sets the orientational average of the preferred strain to zero. Define , the saturation magnetostriction, as the longitudinal relative length change in this model.
Rotational symmetry permits a symmetric second-rank tensor made from of the form , where is the Kronecker delta. If we restrict attention to a change of shape with zero first-order volume change, its trace gives . Requiring the longitudinal component to equal gives . Hence
The tensor product is symmetric and unchanged under . It uses two copies of the magnetic direction, so the third-rank isotropic tensor obstruction in isotropic linear magnetostriction vanishes does not apply. More generally, a small-magnetization expansion can contain ; isotropy alone does not require its trace to vanish. The displayed saturated formula isolates the volume-preserving orientational contribution, rather than asserting that every material has zero volume magnetostriction.
Along a measuring unit vector , with , the fractional length change is
For a stipulated and reference length , alignment gives and a perpendicular orientation gives . Rotating from perpendicular to parallel therefore changes the length by , even though the saturated longitudinal value relative to the random reference is . A negative reverses these elongation and contraction signs.
The eigenvalues of this infinitesimal strain tensor are , so to first order. This is not exact finite incompressibility: using the illustrative deformation gradient gives
A finite-deformation law would need higher-order corrections if exact volume conservation were required.

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