4.5 Article

The growth of the passive film on iron in 0.05 M NaOH studied in situ by Raman microspectroscopy and electrochemical polarization. Part II: In situ Raman spectra of the passive film surface during growth by electrochemical polarization

Journal

JOURNAL OF RAMAN SPECTROSCOPY
Volume 42, Issue 6, Pages 1353-1365

Publisher

WILEY-BLACKWELL
DOI: 10.1002/jrs.2842

Keywords

Raman Microspectroscopy; Passive film on iron; Passive film growth; MCR; Iron oxides

Categories

Funding

  1. National Research Foundation [2053306]
  2. University of the Witwatersrand
  3. DST/NRF Centre of Excellence in Strong Materials

Ask authors/readers for more resources

The composition of the passive film formed on iron in 0.05 M NaOH was analyzed in situ with Raman microspectroscopy with preresonance enhancement during its growth by cyclic potentiodynamic polarization. The surface comprised more than one iron oxide and oxyhydroxide compound whose composition changed during the anodic and cathodic sweeps within successive cycles leading to film growth. The relative amounts of the different iron compounds in the film at selected potentials were determined from the spectra using multivariate curve resolution (MCR) with alternating least squares analysis. Individual spectra of six different such compounds, comprising Fe3O4 (magnetite), gamma-Fe2O3 (maghemite), alpha-Fe2O3 (hematite), alpha-FeOOH (goethite), delta-FeOOH (feroxyhyte) and gamma-FeOOH (lepidocrocite), were used as pure component spectra for the MCR optimization. The results obtained over the first 15 cycles indicate that alpha-FeOOH, gamma-FeOOH, delta-FeOOH and gamma-Fe2O3 were present in the film at the beginning of the passive region of the anodic polarization. The amount ofwater in the film was also observed to increase at this potential range. Further into the passive region (atmore positive potentials), a decrease in the amount of water, which was accompanied by a decrease in alpha-FeOOH and gamma-FeOOH in favor of an increase in the amount of gamma-Fe2O3, was observed. Fe3O4 and alpha-Fe2O3 were not detected on the surface. With increasing number of cycles, the surface became increasingly amorphous or hydrated. Copyright (C) 2010 John Wiley & Sons, Ltd.

Authors

I am an author on this paper
Click your name to claim this paper and add it to your profile.

Reviews

Primary Rating

4.5
Not enough ratings

Secondary Ratings

Novelty
-
Significance
-
Scientific rigor
-
Rate this paper

Recommended

No Data Available
No Data Available