Abstract
Pyramidal I slip was observed to be the dominant slip mode in magnesium single crystals compressed quasi-statically along c-axis at room temperature. The slip trace angles resulted from pyramidal I and pyramidal II slips projected on (0 −1 1 0) and (2 −1 −1 0) surfaces were initially calculated, and then measured on 3% deformed magnesium single crystals. The measured angles indicate the prevalence of pyramidal I slip ({10–11}<11–23> with the critical resolve shear stress of 54MPa). The pyramidal slip traces are dense but very fine, suggesting limited <c+a> dislocation activities.
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