Abstract

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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