HIGH-RESOLUTION TRANSMISSION ELECTRON-MIC ROSCOPY OF PRECIPITATE MICROSTRUCTURES OF 2-STEP AGED AL-1.6-PERCENT-MG2SI ALLOY

Citation
K. Matsuda et al., HIGH-RESOLUTION TRANSMISSION ELECTRON-MIC ROSCOPY OF PRECIPITATE MICROSTRUCTURES OF 2-STEP AGED AL-1.6-PERCENT-MG2SI ALLOY, Nippon Kinzoku Gakkaishi, 62(2), 1998, pp. 133-139
Citations number
12
Categorie Soggetti
Metallurgy & Metallurigical Engineering
Journal title
ISSN journal
00214876
Volume
62
Issue
2
Year of publication
1998
Pages
133 - 139
Database
ISI
SICI code
0021-4876(1998)62:2<133:HTEROP>2.0.ZU;2-Q
Abstract
High resolution transmission electron microscopy (HRTEM) was performed on the micro-structure analyses of a two-step aged Al-1.6 mass%Mg2Si alloy in order to elucidate the characteristic two-step aging behavior of Al-Mg-Si alloys. The optimum conditions for the HRTEM observation of fine precipitates were determined, including accelerating voltage, defocus and crystallographic orientations. The alloy aged at 343 simil ar to 423 Ii for 60 ks was found to produce fine G.P. zones with mono layer or multi layer structures. When the specimens containing such G. P. zones are finally aged at 473 Ii up to their maximum hardness condi tions, a number of random-type precipitates, which are assumed to cont ain high concentration vacancies, are homogeneously formed. These prec ipitates result in the increased hardness, exhibiting so-called positi ve effect of the two-step aging. On the contrary, the alloy aged at 29 3 Ii for 60 lis, the primary G.P. zones with the diameter of similar t o 1 nm are formed with high number density. When this alloy is finally aged at 473 K up to a maximum hardness parallelogram-type precipitate s are preferentially formed. These parallelogram-type precipitates res ult in the decreased hardness, exhibiting negative effect of the two-s tep aging. Based on the microstructure analyses it is concluded that b oth the primary and mono layer G.P. zones almost dissolve into the mat rix at the beginning of 473 Ii aging, while multi layer G.P. zones con tinuously transform into random-type precipitate or act as effective n ucleation sites for the random-type precipitates.