Articles | Volume 34, issue 5
https://doi.org/10.5194/ejm-34-493-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/ejm-34-493-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
21 Oct 2022
Research article |
| 21 Oct 2022
| 21 Oct 2022
Weathering of stannite–kësterite [Cu2(Fe,Zn)SnS4] and the environmental mobility of the released elements
Patrick Haase
CORRESPONDING AUTHOR
Institute of Geosciences, Friedrich Schiller University, Jena, Germany
Stefan Kiefer
Institute of Geosciences, Friedrich Schiller University, Jena, Germany
Kilian Pollok
Institute of Geosciences, Friedrich Schiller University, Jena, Germany
Petr Drahota
Institute of Geochemistry, Mineralogy and Mineral Resources, Charles University, Prague, Czech Republic
Juraj Majzlan
Institute of Geosciences, Friedrich Schiller University, Jena, Germany
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Minerals formed by weathering of toxic materials, of either natural or human origin, act as storage containers for toxic elements. In this work, we investigated properties of common minerals which store and release arsenic in the environment. The data presented here will allow for improved modeling of the polluted sites and for better remediation strategies that could be applied to minimize the impact of the pollution on the environment.
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Minerals formed by weathering of toxic materials, of either natural or human origin, act as storage containers for toxic elements. In this work, we investigated properties of common minerals which store and release arsenic in the environment. The data presented here will allow for improved modeling of the polluted sites and for better remediation strategies that could be applied to minimize the impact of the pollution on the environment.
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Since As is detrimental to the environment, the As content of ores should be reduced before it is released into the atmosphere through a smelting process. Thus, Raman spectra of typical As minerals were investigated, and these can be used in the industrial removal of As-rich ores prior to the ore beneficiation. An additional objective of our study was an investigation of the secondary products of enargite weathering. They play a decisive role in the release or retainment of As in the waste form.
Juraj Majzlan, Alexandra Plumhoff, Martin Števko, Gwladys Steciuk, Jakub Plášil, Edgar Dachs, and Artur Benisek
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Eur. J. Mineral., 33, 357–371, https://doi.org/10.5194/ejm-33-357-2021, https://doi.org/10.5194/ejm-33-357-2021, 2021
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Dislocation and disclination densities in experimentally deformed polycrystalline olivine
Appearance, study and a possible correction for boron: a phenomenon in ultra-soft X-ray measurements using a synthetic multilayer crystal and the EPMA
The hierarchical internal structure of labradorite
Automatic element and mineral detection in thin sections using hyperspectral transmittance imaging microscopy (HyperTIM)
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Nobuyoshi Miyajima, Danielle Silva Souza, and Florian Heidelbach
Eur. J. Mineral., 36, 709–719, https://doi.org/10.5194/ejm-36-709-2024, https://doi.org/10.5194/ejm-36-709-2024, 2024
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Dauphiné twin (DT) domains in a deformed quartz were visualized for the first time by using orientation-optimized electron channelling contrast imaging under Bragg conditions of the rhombohedral planes. The different contrast of a pair of DT domains in the backscattered electron images originates not from a misorientation between the two domains but from different diffraction intensities between positive and negative rhombohedral planes in quartz.
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Labradorite displays various structural features which have received attention in science for a long time. In this paper an electron microscopy study was performed investigating the hierarchical structure and connecting its features over several orders of magnitude. In addition, the atomic structure was solved with three-dimensional electron diffraction, showing results comparable to X-ray diffraction data and demonstrating the potential of the method to solve complicated crystal structures.
Helge L. C. Daempfling, Christian Mielke, Nicole Koellner, Melanie Lorenz, Christian Rogass, Uwe Altenberger, Daniel E. Harlov, and Michael Knoper
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Vladimir V. Kovalevski and Igor A. Moshnikov
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Vanadium carbides in shungite are shown to be present in several forms, which reflects the distinctive conditions of their formation. An ordered carbon film revealed on the vanadium carbide particles could protect the particles from transformations for a long time. The parageneses of vanadium carbide and roscoelite occur, indicating that roscoelite in shungite rocks may be a secondary mineral formed upon vanadium carbide decomposition.
Ruggero Vigliaturo, Sabrina M. Elkassas, Giancarlo Della Ventura, Günther J. Redhammer, Francisco Ruiz-Zepeda, Michael J. O'Shea, Goran Dražić, and Reto Gieré
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Stephanie Pabich, Christian Vollmer, and Nikolaus Gussone
Eur. J. Mineral., 32, 613–622, https://doi.org/10.5194/ejm-32-613-2020, https://doi.org/10.5194/ejm-32-613-2020, 2020
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Electron backscatter diffraction (EBSD) is a powerful tool to visualize and differentiate between foraminiferal test structures, by providing information on crystal orientation and crystal sizes. This can be used to trace diagenetic recrystallization, altering geochemical proxy signals. The sediment samples from a core from the equatorial Pacific used here, spanning the last 45 Myr, showed no evidence for foraminiferal recrystallization, highlighting the suitability as geochemical proxy archive.
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Short summary
Stannite decomposition leads to the precipitation of an amorphous and metastable Sn–Fe–As-rich phase. With ageing, goethite and cassiterite crystallize from the precursor and mark the end of the weathering cycle. Other elements are lost in the initial stage of weathering (e.g. Zn, S) or after full oxidation of the sulfidic material (e.g. Cu, Ag). Electron microprobe (EMP) and transmission electron microscopy (TEM) analyses were performed to witness the mobility of the released elements.
Stannite decomposition leads to the precipitation of an amorphous and metastable Sn–Fe–As-rich...
