Heated goethite and natural hematite: Can Raman spectroscopy be used to differentiate them?

By D. Faria, F. Lopes. 2007

406 citations recorded by the source corpus.

Subfields: Archeology, Geochemistry and Petrology, Renewable Energy, Sustainability and the Environment

View Paper: https://www.semanticscholar.org/paper/e6805a683736d91288d692bb970b142182f0e364

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1. Albert G. Nasibulin
2. H. Jiang
3. Esko I. Kauppinen
4. Ying Tian
5. S. Shandakov
6. Larisa I. Nasibulina
7. P. R. Mudimela
8. S. Račkauskas

Citations in the corpus

• Simple and rapid synthesis of α-Fe2O3 nanowires under ambient conditions (2009, background): “Figure 3 XPS spectra of α-Fe2O3 NWs: (a) wide range spectrum; (b) Fe 2p spectrum; (c) O 1s spectrum In addition to Raman peaks corresponding to α-Fe2O3 (at 225, 245, 292, 411, 498, 611, and 1323 cm (1)), a very weak peak of Fe3O4 at 663 cm 1 [27, 28] was also detected in the surface layer of the oxi”
• On the goethite to hematite phase transformation (2010, neutral): “[23, 24].”