The magnetostriction and magnetic induction calculated by a continuous
, anisotropic, anhysteric, magnetization model are compared with magne
tostriction and magnetic induction measurements on burst and nonburst
magnetostrictive Tb0.3Dy0.7Fe1.9 twinned single crystal rods. The mode
l shows that the magnetostriction and permeability suppression occurri
ng at low applied field is the result of the rotation,and subsequent c
apture, of initial field antiparallel magnetization into field transve
rse [11 (1) over bar] or [<(11)over bar>1] local magnetoelastic energy
minima. The model further shows that the interval of high magnetostri
ction applied field derivative, d lambda/dH, characteristic of burst m
agnetostrictive material, is the result of the rotation of field trans
verse [11(1) over bar] or [<(11)over bar>1] oriented magnetization int
o the [111] near field magnetocrystalline minima. The occurrence of bu
rst magnetostriction is therefore contingent on obtaining sufficient m
agnetocrystalline anisotropy and sufficiently tight magnetization ener
gy distribution in experimental Tb0.3Dy0.7Fe1.9 twinned single crystal
rods so as to minimize the applied field interval over which this mag
netization rotation process occurs. A final analysis shows that the pr
esent model is able to correctly approximate the applied field depende
nce of the burst magnetostriction response and the applied field depen
dence of the simultaneous magnetostriction and permeability suppressio
n with a single set of parameters for a range of constant [112] applie
d compressive stresses. The model additionally exhibits approximately
correct saturation magnetostrictions for a range of experimentally app
lied compressive stresses. However, the model fails to match the exper
imental behavior above a simultaneous d lambda/dH, permeability and fi
eld hysteresis transition, located approximately 1000 microstrain from
the saturation magnetostriction, The experimental transition clearly
indicates a change in magnetization mechanism not accommodated by the
present model. (C) 1997 American Institute of Physics.