The tensile fracture behaviour of an Al-0.89 wt.% Mg2Si industrial alloy is
studied. It is found that the alloy deforms in a highly localised way only
in the underaged (UA) state. In the peak aged (PA) condition the hardening
precipitates are often by-passed by an Orowan mechanism, which predominate
s in the overaged (OA) state. in the UA condition, the stress concentration
is shown to be large enough to nucleate cracks at the particle interfaces
provided the sheer strain has reached the critical value for cutting the pr
ecipitates into pieces. In the PA and OA conditions, failure results from c
oalescence of voids nucleated at large AlFeSi and smaller (Mg + Si) particl
es. It is shown that none of these particles are responsible alone for frac
ture. In contrast. ductility and rupture surfaces are consistent with a dam
age mechanism whose nucleation step is the coalescence of voids nucleated a
t large AlFeSi and neighbouring (Mg + Si) particles. (C) 2001 Elsevier Scie
nce B.V. All rights reserved.