Published February 2025 | Published
Journal Article Open

Iridescent Iron Oxides

  • 1. ROR icon California Institute of Technology

Abstract

Iridescent iron oxides known as rainbow hematite and turgite are found in a variety of localities worldwide and display a variety of beautiful interference colors. Usually, there is a thin layer of nanocrystals containing aluminum and phosphorous coats, such as with hematite, although one example of aluminum with arsenic is presented. Infrared spectra of samples with thicker layers of these nanocrystals show absorption in the phosphate region. The thin films that range from tens to hundreds of nanometers thick are believed to cause the color. High-resolution secondary electron imaging shows that the thin film consists of nanocrystals arranged in three directions (120° apart). The rod-shaped crystals have a width from 5 to 35 nm and display the same morphology on all samples, irrespective of if they contain phosphorus or arsenic. The minute crystals have failed to produce either an X-ray powder diffraction pattern, an electron back-scatter diffraction pattern in SEM, or an electron diffraction ring pattern under TEM. Raman spectra are dominated by hematite features. Infrared ATR spectra of the bulk material show mostly hematite with occasional minor amounts of goethite and phosphate.

Copyright and License

© 2025 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (https://creativecommons.org/licenses/by/4.0/).
 

Acknowledgement

Rock H. Currier (Jewel Tunnel Imports) drew the authors’ attention to this problem and provided numerous research samples. Robert Housley, Benny Fenn, PA Schroeder and Paul M Adams provided additional samples. Mineracoes Brasileiras Reunidas S.A. is thanked for permission to collect samples at their mines.

Funding

Funding for this project was provided in part through the White Rose Foundation and the National Science Foundation, Grants EAR-9804871 and EAR-0337816. FE-SEM, EDS and EBSD analyses were done at the Caltech GPS analytical facility which is supported in part by the MRSEC Program of the NSF under DMR-0080065.

Contributions

G.R.R. conducted the spectroscopic and wet-chemistry experiments. C.M. conducted the electron-beam experiments. Both authors contributed figures and contributed to the drafting of the manuscript. All authors have read and agreed to the published version of the manuscript.

Data Availability

The authors confirm that the data supporting the findings of this study are available within the article. Additional spectra and electron microscope image are available from the authors.

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Additional details

Created:
January 30, 2025
Modified:
January 30, 2025