Jw. Cohron et al., Room-temperature mechanical behavior of FeAl: Effects of stoichiometry, environment, and boron addition, ACT MATER, 46(17), 1998, pp. 6245-6256
The intrinsic ductility of FeAl (in ultrahigh vacuum) decreases with increa
sing Al content, from around 16% in Fe-37A1 to zero in Fe-48A1. The sharpes
t decline occurs around the composition where the fracture mode changes fro
m transgranular to intergranular. Boron shifts this ductile-brittle transit
ion to higher Al levels by segregating to the grain boundaries and suppress
ing grain-boundary fracture. However, its effectiveness decreases with incr
easing Al concentration, even though the amount of B segregating to the gra
in boundaries remains the same, independent of alloy stoichiometry. Consequ
ently, even the B-doped alloys become brittle and fracture intergranularly
as the stoichiometric composition is approached. Low-pressure hydrogen embr
ittles FeAl, although not as severely as atmospheric moisture. Environmenta
l embrittlement is most noticeable in Fe-rich FeAl; with increasing Al conc
entration, the grain boundaries become intrinsically weak, and brittle frac
ture persists even after environmental effects are eliminated. (C) 1998 Act
a Metallurgica Inc. Published by Elsevier Science Ltd. All rights reserved.