Deformation of NiTiCu shape memory single crystals in compression

Citation
H. Sehitoglu et al., Deformation of NiTiCu shape memory single crystals in compression, MET MAT T A, 32(3), 2001, pp. 477-489
Citations number
16
Categorie Soggetti
Apllied Physucs/Condensed Matter/Materiales Science",Metallurgy
Journal title
METALLURGICAL AND MATERIALS TRANSACTIONS A-PHYSICAL METALLURGY AND MATERIALS SCIENCE
ISSN journal
10735623 → ACNP
Volume
32
Issue
3
Year of publication
2001
Pages
477 - 489
Database
ISI
SICI code
1073-5623(200103)32:3<477:DONSMS>2.0.ZU;2-U
Abstract
Single-crystal orientations of NiTi10Cu alloys were studied under increment al, cyclic compression conditions to establish the pseudoelastic and shape memory response of this class of alloys. This material exhibits a two-step transformation involving cubic to orthorhombic: martensite (B2 --> B19) fol lowed by orthorhombic to monoclinic martensite (B19 --> B19'). The transfor mation parameters (shear magnitudes and directions for habit and twin plane s) were determined associated with the B2 --> B19 transformation. The growt h of monoclinic martensite correspondent variant pairs (CVPs) emanating fro m the orthorhombic structure was also analyzed. The transformation strain f or the B2 --> B19 case was orientation dependent and lower than the B19 --> B19' transformation in compression for all orientations except those near the [001] pole. The experimental results show that the critical transformat ion stress is orientation dependent and is in the range 30 to 58 MPa. Orien tations that exhibit lower transformation stress (or high resolved shear st ress factors, [100] and [012]) produce higher recoverable strains las high as 4 pet), while other orientations ([011], [111], and [123]) with lower re solved shear stress factors result in recoverable strains less than 3 pet. At higher strains, inelastic deformation develops, limiting recoverability. The recoverable strains are lower than the theoretical values for two main reasons: the transformation is curtailed first by austenite slip and subse quently by martensite slip, and the orthorhombic structure does not fully t ransform to the monoclinic martensite.