Journal
ACTA MATERIALIA
Volume 253, Issue -, Pages -Publisher
PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.actamat.2023.118957
Keywords
Titanium alloy; alpha p volume fraction; Fatigue crack initiation; Twist grain boundary; HR-DIC; Strain heterogeneity
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The present study investigates the effects of microstructural constituents on crack initiation in two-phase titanium alloys. It was found that basal (a) slip plays a crucial role in crack initiation, regardless of cracking mode. Increasing ap fraction resulted in a shift from transgranular to intergranular crack initiation. The high-resolution 2D strain mapping revealed that intergranular cracks initiated from (0001) twist grain boundaries.
The role of different microstructural constituents on crack initiation in two-phase titanium alloys is still an area of great controversy. The present study investigates the effects of primary a volume fraction and concomitant macrozones on two different fatigue crack initiation modes concurrently observed in a near-a titanium alloy. Statistically representative regions were monitored in quasi-in-situ studies by interrupting fatigue testing to detect slip trace formation leading to crack initiation. In addition, high-resolution 2D strain maps were generated to quantify in-plane shear strains of slip traces related to microstructural features. The detailed analysis demonstrates that at 90% of the proof stress basal (a) slip plays a crucial role in crack initiation, regardless of whether cracking is transgranular or intergranular. In addition, a distinct shift from transgranular to intergranular crack initiation was observed with increasing ap fraction driven by the increased number of a(p)/a(p) grain boundaries. The high-resolution 2D strain mapping suggest that these intergranular cracks initiated from a burst of basal (a) slip starting from (0001) twist grain boundaries but penetrating one side of the grain pair in case of a partial (0001) twist grain boundary. From these observations, a new criterion for intergranular cracking is proposed based on a geometrical grain boundary parameter and the preference of neighbouring a(p) grain pair well aligned for basal (a) slip. It was found that while (0001) twist grain boundaries increase with increasing a(p) fraction, macrozones do not further enhance their frequency. However, macrozones of hard orientated grains did enhance transgranular crack formation by potentially higher local stress and increasing slip length over clustered a(p) grains with low misorientation reducing the requirement for out-of-plane shear.
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