4.7 Article

Experimental evidence of concurrent compositional and structural instabilities leading to ω precipitation in titanium-molybdenum alloys

Journal

ACTA MATERIALIA
Volume 60, Issue 2, Pages 596-609

Publisher

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.actamat.2011.10.008

Keywords

Omega phase; Titanium alloy; Collapse of atomic planes; Phase separation; Atom probe tomography

Funding

  1. National Science Foundation, Division of Materials Research [6701956]
  2. Direct For Mathematical & Physical Scien
  3. Division Of Materials Research [1006487] Funding Source: National Science Foundation

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The omega phase is commonly observed in many commercial 13 or near-beta titanium alloys on rapidly cooling from the single 13 phase field and also during subsequent isothermal annealing. However, the crystallographic formation mechanism for the omega particles is hitherto unclear/under discussion. The present study primarily focuses on omega precipitation within the beta (body-centered cubic (bcc)) matrix of simple model binary titanium molybdenum (Ti-Mo) alloys. It provides direct experimental evidence of the formation of omega-like embryos from competing compositional and structural instabilities arising in the bcc lattice of Ti-Mo alloys during rapid cooling from the high-temperature single beta phase field. The displacive partial collapse of the {1 1 1} planes of the parent bcc structure within compositionally phase-separated regions containing several at.% less of Mo, forming omega-like embryos, has been conclusively shown by coupling aberration-corrected high-resolution scanning transmission electron microscopy with atom probe tomography observations. Growth and coarsening of these omega-like embryos take place during subsequent isothermal annealing, accompanied with both a completion of the collapse of the {1 1 1} beta planes leading to a fully developed omega structure as well as rejection of Mo from these precipitates, resulting in near-equilibrium compositions. (C) 2011 Acta Materialia Inc. Published by Elsevier Ltd. All rights reserved.

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