Study of local environment in quasicrystallineAl86Mn14by Mössbauer effect

Abstract
Mössbauer-effect measurements on Al86 (57 Fe0.02 Mn0. 98)>14 in the icosahedral phase indicate a distribution of quadrupole-splitting magnitudes at the iron sites. This distribution strongly indicates the existence of more than two inequivalent Mn sites. It can be fitted at least as well with a continuous distribution of sites of the form suggested by an amorphous analog as with a discrete set.