The crystal structure of the alloy Fe3Ga has four inequivalent crystallogra
phic iron sites. Mossbauer spectra recorded at 4.2 K were able to be fined
with four sextets corresponding to these sites. Measurement of the hyperfin
e fields B-hf gave values 271 kG, 191 kG, 152 kG and 195 kG respectively Fo
r the series (Fe1-xTix)(3)Ga-4 spectra were recorded at 4.2 and 300 K for x
= 0.05, x = 0.10 and x = 0.15. These spectra were fitted to five sextets,
each associated with a distinct iron site. The magnetic ordering temperatur
e Te was observed to be essentially unchanged for 0 less than or equal to x
less than or equal to 0.15. Site preference for Ti atoms was observed for
x = 0.10 and x = 0.15 causing a large change in hyperfine held values at a
neighbouring site.
Similar Mossbauer studies were made on the series (Fe1-yCry)(3)Ga-4(0 less
than or equal to y less than or equal to 0.20). Spectra at 4.2 K could be f
itted with four sextets but continuous reductions in hyperfine field values
and ordering temperature T-C were observed with increasing y. The contrast
in the magnetic behaviour of the two series is associated with different p
atterns of substitutional site preference.