Abstract
An interpretation of the line-shape asymmetry for the Fe57 Mössbauer Zeeman spectrum in speromagnetically ordered amorphous yttrium iron garnet (a-YIG) at 4.2 K provides the first reported measurement of the distribution of electric-field-gradient (EFG) sign in an amorphous material. The number of iron sites with positive EFG (n+) is found to exceed those with negative EFG (n) in a-YIG in the ratio n+n1.16±0.04. This finding is in quantitative agreement with the prediction of a computer model of randomly packed spherical ions. Since n+n=0 for crystalline YIG, the possibility that a-YIG retains any vestige of its crystalline local environment in distorted form can therefore be completely excluded.