Abstract

The complex and intricate microstructure of B19′ martensite in shape memory nickel titanium alloys is generally explained with the Phenomenological Theory of Martensitic Crystallography (PTMC). Over the last decade, we have developed an alternative approach that supposes the existence of a “natural” parent–daughter orientation relationship (OR). As the previous TEM studies could not capture the global crystallographic characteristics of the B2→B19′ transformation required to discriminate the models, we used Electron BackScatter Diffraction (EBSD) and Transmission Kikuchi Diffraction (TKD) to investigate a polycrystalline NiTi alloy composed of B19′ martensite. The EBSD maps show the large martensite plates and reveal the coexistence of different ORs. The TKD maps permit us to image the “twins” and confirm the continuum of orientations suspected from EBSD. The results are interpreted with the alternative approach. The predominant OR in EBSD is the “natural” OR for which the dense directions and dense planes of B2 and B19′ phases are parallel—i.e., (010)B19′//(110)B2 and [101]B19′//[ 1 ¯ 11]B2. The natural OR was used to automatically reconstruct the prior parent B2 grains in the EBSD and TKD maps. From the distortion matrix associated with this OR, we calculated that the habit plane could be (1 1 ¯ 2)B2//(10 1 ¯ )B19′. The traces of these planes are in good agreement with the EBSD maps. We interpret the other ORs as “closing-gap” ORs derived from the natural OR to allow the compatibility between the distortion variants. Each of them restores a parent symmetry element between the variants that was lost by distortion but preserved by correspondence.

Highlights

  • Since no plane can be maintained fully invariant by the fcc-bcc distortion, we proposed that the habit plane could be a plane that is only unrotated by the lattice distortion

  • The Phenomenological Theory of Martensitic Crystallography (PTMC) calculations lead to solutions only if the stretch (Bain) distortion is such that one of its three eigenvalues is greater than 1 and another less than 1; in other words, part of the distortion should be an elongation along an axis and a contraction along another axis

  • In most of the maps, some small islands with a cubic structure are visible. When they have a facetted morphology, they are probably cubic precipitates misindexed as B2 phase, but in in some maps the zones indexed as B2 are really B2, because they form large equiaxed grains in a volume fraction that is far greater than that of B190 martensite, and they cannot be confused with precipitates

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Summary

Introduction

Since the morphology of martensite is often plate or lenticular, PTMC assumes that the habit plane (the plane of the plate or the mid-rib of the lenticle) is the plane of an “invariant plane strain”; that martensite results from an invariant plane strain deformation. This deformation mode is a composition of a simple shear along the habit plane (no volume change) and an extension or a contraction perpendicularly to the habit plane (that gives the volume change of the transformation). These lattice distortions can be expressed in the form of a rotation composed with a Crystals 2020, 10, 562; doi:10.3390/cryst10070562 www.mdpi.com/journal/crystals

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