Articles | Volume 37, issue 1
https://doi.org/10.5194/ejm-37-101-2025
https://doi.org/10.5194/ejm-37-101-2025
Research article
 | 
25 Feb 2025
Research article |  | 25 Feb 2025

Incorporation of W6+ into hematite (α-Fe2O3) in the form of ferberite nanolamellae

Juraj Majzlan, Ralph Bolanz, Jörg Göttlicher, Martin Števko, Tomáš Mikuš, Mária Čaplovičová, Jan Filip, Jiří Tuček, Christiane Rößler, and Christian Matthes

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Short summary
Many chemical elements occur in rocks, in ore deposits, and in the environment in trace amounts. One of them is the element tungsten. It is not clear, however, where the trace amounts of tungsten reside and how they move around. In this work, we found that the element tungsten can be carried by a common iron oxide mineral, hematite. It can be transported in hematite and released under appropriate conditions, for example in reducing environments.
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