Neutron diffraction has been used to investigate the rare-earth effect
on the site occupations of Al and C atoms in the combined substitutio
nal-interstitial compounds, R2Fe15Al2Cy (R=P-r, Tb, Ho). All three sam
ples have the rhombohedral Th2Zn17-type structure. As the composition
changes from light rare-earth to heavy rare-earth, the site occupation
s of the substitutional Al atoms on the 6c and 18f increase while that
on the 18h site decreases. However, the 18h site still has the highes
t Al occupation for all samples. The site occupation of the C atoms on
the octahedral interstitial site (9e) is much higher in the heavy rar
e-earth (Ho) sample than in the light rare-earth (Pr) sample. However,
the tetrahedral interstitial 18g site shows a reverse behavior. This
18g site occupation of C atoms has not been observed before except in
gas phase interstitial compounds. The Al site occupation is determined
by the crystal environment, while the C site occupation appears to be
determined predominantly by site size. (C) 1997 American Institute of
Physics.