5 questions to test your understanding
An aluminum alloy is aged at 150°C. After 4 hours it reaches peak hardness. An engineer continues aging it for 24 hours to 'fully develop' the precipitates. What happens to the hardness?
During early aging (GP zone formation), what is the primary mechanism by which fine precipitates impede dislocation motion?
An alloy that has been overaged can be restored to near-peak hardness by re-solution treating above the solvus temperature followed by re-quenching and re-aging.
Larger precipitate particles are stronger barriers to dislocation motion than smaller ones at the same volume fraction.
Why does hardness first increase then decrease during aging at a fixed temperature, even though precipitates continue to grow throughout the entire aging period?