Growth‐Induced Anisotropy in Bubble Garnet Films Containing Calcium

Abstract
The growth‐induced anisotropy, Ku measured on (111) LPE films of Eu3−xCaxSix Fe5−xO12 grown on Sm3Ga5O12 substrates is large and positive (Ku = 4.0 to 8.1×104ergs/cm3 for x = 0.5 ). Many experiments have shown that Ku in Eu3−xYxFe5−yGayO12 films is also positive. In films of compositions (YSmCa)3 (GeFe)5O12 , the effects of Ca and of Y on the growth‐induced anisotropy are the same in sign and similar in magnitude. Since Ca2+ is larger in ionic radius than Eu3+ or Sm3+, whereas Y3+ is smaller, the simple site selectivity model of growth‐induced anisotropy would predict opposite signs of Ku for the Ca and Y additions. This contradiction shows that ionic radius is not the only relevant parameter which determines growth‐induced anisotropy in garnets, although size differences have been shown to account for the observed effects within the rare earth series. The charge difference between the Ca2+ ions and the rare earth ions, or the pairing of Ca2+ and Ge4+ or Si4+ ions during crystal growth may influence the site preference of the Ca ions and the resulting anisotropy. The growth‐induced anisotropy of the Eu2.5Ca0.5Si0.5Fe4.5O12 film, grown at 835°C at a rate of 2 μm/min, annealed out after several hours at 900°C in oxygen. This temperature is much lower than the usual annealing temperatures of 1200°C to 1300°C in O2 which are required to reduce Ku in other bubble garnets. This is attributed to a high concentration of defects due to an imbalance in the Ca‐Si concentrations in films grown at low temperatures and large growth rates.