The
magnetostriction \lambda characterizes the shape change of a
ferromagnetic material during magnetization, whereas the inverse magnetostrictive effect characterizes the change of sample magnetization M(for given magnetizing field strength H) when mechanical stresses \sigma are applied to the sample.
Qualitative explanation of magnetoelastic effect Under a given uni-axial mechanical stress \sigma, the flux density B for a given magnetizing field strength H may increase or decrease. The way in which a material responds to stresses depends on its saturation magnetostriction \lambda_s. For this analysis, compressive stresses \sigma are considered as negative, whereas tensile stresses are positive. According to
Le Chatelier's principle: \left(\frac{d\lambda}{dH}\right)_{\sigma}=\left(\frac{dB}{d\sigma}\right)_{H} This means, that when the product \sigma \lambda_s is positive, the flux density B increases under stress. On the other hand, when the product \sigma \lambda_s is negative, the flux density B decreases under stress. This effect was confirmed experimentally.
Quantitative explanation of magnetoelastic effect In the case of a single stress \sigma acting upon a single magnetic domain, the magnetic strain energy density E_\sigma can be expressed as: E_\sigma = \frac{3}{2} \lambda_s \sigma \sin^2(\theta) where \lambda_s is the magnetostrictive expansion at saturation, and \theta is the angle between the saturation magnetization and the stress's direction. When \lambda_s and \sigma are both positive (like in iron under tension), the energy is minimum for \theta = 0, i.e. when tension is aligned with the saturation magnetization. Consequently, the magnetization is increased by tension.
Magnetoelastic effect in a single crystal In fact, magnetostriction is more complex and depends on the direction of the crystal axes. In
iron, the [100] axes are the directions of easy magnetization, while there is little magnetization along the [111] directions (unless the magnetization becomes close to the saturation magnetization, leading to the change of the domain orientation from [111] to [100]). This
magnetic anisotropy pushed authors to define two independent longitudinal magnetostrictions \lambda_{100} and \lambda_{111}. • In
cubic materials, the magnetostriction along any axis can be defined by a known
linear combination of these two constants. For instance, the elongation along [110] is a linear combination of \lambda_{100} and \lambda_{111}. • Under assumptions of
isotropic magnetostriction (i.e.
domain magnetization is the same in any crystallographic directions), then \lambda_{100} = \lambda_{111} = \lambda and the linear dependence between the
elastic energy and the stress is conserved, E_\sigma = \frac{3}{2} \lambda \sigma (\alpha_1 \gamma_1 +\alpha_2 \gamma_2 + \alpha_3 \gamma_3)^2. Here, \alpha_1 , \alpha_2 and \alpha_3 are the direction cosines of the domain magnetization, and \gamma_1 , \gamma_2 , \gamma_3 those of the bond directions, towards the crystallographic directions. == Method of testing the magnetoelastic properties of magnetic materials ==