4.7 Article

Morphological and chemical characteristics of oxide scales formed on δ-Phase plutonium metal alloys I: 3.5 at% ga

Journal

JOURNAL OF NUCLEAR MATERIALS
Volume 547, Issue -, Pages -

Publisher

ELSEVIER
DOI: 10.1016/j.jnucmat.2021.152815

Keywords

Nuclear forensics; Plutonium; Focused ion-beam scanning electron microscopy (FIB-SEM); Auger electron spectroscopy (AES)

Funding

  1. U.S. Department of Energy by Lawrence Livermore National Laboratory [DE-AC52-07NA27344]
  2. Office of Defense Nuclear Nonproliferation Research and Development within the U.S. Department of Energy's National Nuclear Security Administration [FY16LL-NDD3BA-P28]

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By using FIB-SEM and 3D microscopy to characterize the morphological features of oxide scales, the study found variations in the oxide surface under different environmental conditions. The oxide scale retained its original structure and chemical characteristics after exposure to dry air environments, but became thinner and without internal microcracking after exposure to moist air environments.
Focused ion-beam scanning electron microscopy (FIB-SEM) and three-dimensional (3D) microscopy were applied to characterize the subsurface morphological features of oxide scales formed on an similar to 3.5 at.% Ga plutonium (Pu) metal alloy. Using the FIB-SEM technique, a number of morphological features formed in the interior of the oxide scale from Pu metal's environmental exposure were observed and identified. Auger electron spectroscopy (AES) was utilized to characterize the cross-sectional composition and chemistry of the oxide scale. The oxide scale formed during inert storage and operational environments has a characteristic internal scale structure that includes a relatively dense oxide layer with some lateral and transverse cracking. Generally, after subsequent exposure to dry air environment, the oxide scale retained most of the original structural and chemical characteristics. However, after aging in a moist air environment, while the oxide scale was found to maintain the chemical characteristics of the source oxide, the scale was found to be on average thinner and without the previously observed internal microcracking, likely the result of spallation of the source scale during exposure to the new environment. (C) 2021 Elsevier B.V. All rights reserved.

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