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The microstructure of scale formed by oxynitriding of Ti and exhibiting significant apatite-forming ability

Published online by Cambridge University Press:  10 March 2016

Masami Hashimoto*
Affiliation:
Materials Research and Development Laboratory, Japan Fine Ceramics Center, 2-4-1 Mutsuno, Atsuta-ku, Nagoya 456-8587, Aichi, Japan
Satoshi Kitaoka
Affiliation:
Materials Research and Development Laboratory, Japan Fine Ceramics Center, 2-4-1 Mutsuno, Atsuta-ku, Nagoya 456-8587, Aichi, Japan
Shunsuke Muto
Affiliation:
Institute of Materials and Systems for Sustainability, Nagoya University, Furo-cho, Chikusa-ku, Nagoya 464-8603, Aichi, Japan
Kazuyoshi Tatsumi
Affiliation:
Institute of Materials and Systems for Sustainability, Nagoya University, Furo-cho, Chikusa-ku, Nagoya 464-8603, Aichi, Japan
Yoshihiro Obata
Affiliation:
Graduate School of Engineering, Nagoya University, Furo-cho, Chikusa-ku, Nagoya 464-8603, Aichi, Japan
*
a) Address all correspondence to this author. e-mail: masami@jfcc.or.jp

Abstract

A scale formed by heat treatment of Ti in a nitrogen atmosphere containing oxygen at an extremely low partial pressure exhibited an exceptional degree of hydroxyapatite (HAp) formation in a simulated body fluid. Scanning transmission electron microscopy and electron energy loss spectroscopy indicated that the subsurface of this scale was composed of nitrogen doped rutile-type TiO2. The N-K edge energy-loss near edge structure spectrum of this layer in conjunction with the theoretical spectra of possible compounds obtained using the augmented plane wave plus local orbital band method suggested that oxygen sites were replaced by two nitrogens, resulting in an effective charge of +2. The enhanced HAp forming ability of this scale is likely related to the positively charged surface induced by the presence of N. Conversely, the subsurface scale formed by heat treatment in air, in which N is not found, leads to much slower HAp coverage, believed to be related to the lack of surface charge.

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Type
Articles
Copyright
Copyright © Materials Research Society 2016 
Figure 0

FIG. 1. Cross-sectional TEM image (left) and N and O SIMS depth profiles (right) through the scale formed by treatment A. The SIMS intensities have been normalized to the Ti intensity.

Figure 1

FIG. 2. Cross-sectional TEM image (left) and N and O SIMS depth profiles (right) through the scale formed by treatment B. The SIMS intensities have been normalized to the Ti intensity.

Figure 2

FIG. 3. Depth-resolved (b) Ti, (c) O, and (d) N distributions in the scale formed by treatment A, obtained by scanning the framed area in (a) STEM image (5 nm/pixel).

Figure 3

FIG. 4. STEM image (left) and depth-resolved Ti-L2,3, O-K, and N-K edge ELNES spectra (right) of a cross-section of the scale formed by treatment A.

Figure 4

FIG. 5. Three component MCR analysis of the scale formed by treatment A: (a) STEM image of the scale, and spatial distribution maps from the framed area in (a) showing (b) phase I, (c) phase II, (d) phase III, and (e) the residual phase.

Figure 5

FIG. 6. (a) N-K, (b) Ti-L2,3, and (c) O-K edge ELNES spectra of the extracted spectral components of phases I, II, and III in the scale formed by treatment A. Each spectrum has been offset vertically to allow easier comparison.

Figure 6

FIG. 7. (a) Experimental and [(b)–(g)] theoretical N-K ELNES spectra obtained in the vicinity of the surface of the scale formed by treatment A. The effective charge is indicated on each theoretical spectrum.

Figure 7

FIG. 8. Two-component MCR analysis of the scale formed by treatment B: (a) STEM image of the scale, and spatial distribution maps from the framed area in (a) showing (b) phase I, (c) phase II and (d) the residual phase.

Figure 8

FIG. 9. (a) N-K, (b) Ti-L2,3, and (c) O-K edge ELNES spectra of the extracted spectral components of phases I and II in the subsurface scale formed by treatment B. Each spectrum has been offset vertically to allow easier comparison.