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Lithium extraction from the mineral zinnwaldite: Part I: Effect of thermal treatment on properties and structure of zinnwaldite
•The dehydroxylation mechanism of zinnwaldite was studied.•27Al-NMR, F-NMR, Li-NMR, Mössbauer, IR spectroscopy were applied.•The crystal structure of tempered zinnwaldite at 700°C was resolved.•β-spodumene, leucite, hematite and magnetite are the main decomposition products. Lithium has become an en...
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Published in: | Minerals engineering 2017-09, Vol.111, p.55-67 |
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Main Authors: | , , , , , , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
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Summary: | •The dehydroxylation mechanism of zinnwaldite was studied.•27Al-NMR, F-NMR, Li-NMR, Mössbauer, IR spectroscopy were applied.•The crystal structure of tempered zinnwaldite at 700°C was resolved.•β-spodumene, leucite, hematite and magnetite are the main decomposition products.
Lithium has become an energy critical element and thus the security of supply is of great importance. As a local German resource, attention was directed towards the mica-type mineral zinnwaldite. It represents a lithium-rich siderophyllite and corresponds to an intermediate polylithionite–siderophyllite solid solution with high contents of fluoride. Mineral samples from the deposit Zinnwald/Cínovec at the German/Czech border were analyzed and characterized by a variety of methods, particularly concerning its thermal behavior. Understanding the thermal behavior of the mica gives the opportunity to develop new and cost-efficient methods for lithium extraction.
Investigations with different spectroscopic methods revealed the decomposition mechanisms. Starting at 300°C, oxidation of Fe2+ catalyzed the dehydroxylation of the mica by dehydrogenation. This is followed by a dehydroxylation similar to the mechanism of dioctahedral micas. At higher temperatures, the release of HF was detected. At about 800°C the precipitation of hematite was observed. The complete decomposition of Zinnwaldite takes place at 900°C, it is accompanied by the liberation of SiF4 and leads to the formation of several solid decomposition products.
By means of single-crystal diffraction using X-rays and neutrons the structural changes could be identified after annealing at 700°C. The results point to a transformation into a polylithionite-like structure, the end member of the solid solution series. |
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ISSN: | 0892-6875 1872-9444 |
DOI: | 10.1016/j.mineng.2017.05.006 |