Abstract
Deformation twins have been observed in polycrystalline Al-4.8 wt% Mg shock-loaded at -180°C to 13 GPa. Selected area diffraction confirms the twinning plane to be the {111}, similar to deformation twinning in other face-centered cubic (f.c.c.) metals. Transmission electron microscope (TEM) observations indicate that twins form preferentially near grain boundaries. A qualitative estimate of twin boundary velocity based on TEM observations suggests that twins in Al-4.8 wt% Mg form at speeds just below the shear wave velocity. Similarly shock-loaded experiments on 99.99 Al and 6061-T6 exhibited no evidence of deformation twinning. Substructure evolution and twin formation and/or lack of deformation twinning in the three aluminum alloys studied are discussed in terms of deformation twinning mechanisms.
| Original language | English |
|---|---|
| Pages (from-to) | 1745-1754 |
| Number of pages | 10 |
| Journal | Acta Metallurgica |
| Volume | 36 |
| Issue number | 7 |
| DOIs | |
| State | Published - Jul 1988 |
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