Iridescent Hematite


George R. Rossman , Chi Ma

Division of Geological and Planetary Sciences California Institute of Technology Pasadena, CA 91125-2500, USA

Abstract

Iridescent iron oxides known as rainbow hematite and turgite are found in a variety of localities worldwide, displays a variety of beautiful interference colors. Usually, a thin layer of nanocrystals containing aluminum and phosphous coats such as with hematite, although one example of a coating with aluminum arsenate is presented. Infrared spectra of samples with thicker layers of those 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 (120º apart). The rod-shaped crystals have a width from 5 to 35 nm and display the same morphology on all samples irrespective if they are phosphate or arsenate. 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.


raiinbiw hematite    SEM
Rainbow hematite from Brazil                                                                                   SEM  image of the thin film