Precipitation sequence in an Al-1.6 mass%Mg2Si alloy was investigated by DS
C measurement and HRTEM observation, Four exothermic peaks (A, C, D and E)
and one endothermic peak (B) were obtained when samples were heated at 10 K
/min. Precipitates were confirmed when samples aged to the temperature of e
ach peak were observed using HRTEM, and were classified into several types.
Products in the region between peaks A and B were classified as GP zones.
Precipitates between peaks B and C were classified as the random-type preci
pitates. Precipitates at peak C were classified as the parallelogram-type p
recipitates. Precipitates at peak D were classified as metastable phase bet
a '. Precipitates at peak E were classified as equilibrium phase beta. Alth
ough there have been many reports that the beta " phase is formed at peak C
, this was not observed in the present study, rather random-type precipitat
es were observed. The hardness of samples heated to various temperatures wa
s measured. The temperature that resulted in maximum hardness corresponded
to the temperature that yielded the maximum amount of random-type precipita
tes.