![]() ![]() The latter term originated with the German mineralogist Rudolph Hermann, who coined it in 1844 to describe iron hydroxide specimens found near the Turginsk River in the Ural Mountains (Hermann, 1844). Hematite specimens that frequently display iridescence are described as “rainbow hematite” and “turgite” (figure 1). The authors propose that this periodic substructure results from arrested crystal growth by the oriented aggregation of hematite nanorods. The organized substructure is apparent on all freshly fractured surfaces, suggesting that it represents more than an exterior surface coating. The distances between adjacent parallel spindle-shaped particles within the same layer fall in the range of 280–400 nm, generating a diffraction grating for visible light. They are arranged in three orientations at 120º angles with respect to each other and stacked layer by layer to form the bulk crystal. The nanorods are 200–300 nm in length and 50–60 nm in width. The study revealed that the interference is produced by a highly periodic microstructure consisting of spindle-shaped hematite nanocrystals containing minor Al and P impurities. The authors investigated “rainbow” hematite from Minas Gerais, Brazil, using electron microscopy, atomic force microscopy, and synchrotron X-ray diffraction to determine the cause of its intense wide-angle iridescence. Rainbow hematite from the Andrade mine in João Monlevade, Minas Gerais, Brazil. Applied Jewelry Professional ™ Online Diplomaįigure 1.
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