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Cation and anion ordering and clustering in the system Lithian muscovite, Trilithionite and Polylithionite

Subject Area Mineralogy, Petrology and Geochemistry
Term from 2018 to 2023
Project identifier Deutsche Forschungsgemeinschaft (DFG) - Project number 405948055
 
Final Report Year 2023

Final Report Abstract

A large number of lepidolites K(LixAl3-x)[Si2xAl4-2xO10](OH)yF2-y and Li-muscovites K(LixAl2-x/3□1-2x/3)[Si3AlO10](OH)yF2-y were synthesised by a gelling method in combination with hydrothermal syntheses at a pressure of 2 kbar and a temperature of 873 K. The nominal composition ranged between 0.0 ≤ x ≤ 2.0 and 0.0 ≤ y ≤ 2.0, i.e., from polylithionite K[Li2.0Al][Si4.0O10](OH)yF2-y over trilithionite K[Li1.5Al1.5][AlSi3.0O10](OH)yF2-y to muscovite K[Al2.0□][AlSi3.0O10](OH)yF2-y . 1H, 19F, 29Si, 27Al MAS NMR and 27Al MQMAS NMR spectroscopy has been performed to investigate the order/disorder state of Si and Al in the tetrahedral layers and of Li, Al, OH and F in the octahedral layer. The synthetic mica crystals are very small, ranging from 0.1 μm to 5 μm. Rietveld structure analyses on 12 samples showed that nearly all samples consist of two mica polytypes (1M and 2M1) of varying proportions. In the case of lepidolites, the 1M/2M1-ratio depends on the Li/Al ratio of the reaction mixture. The refinement of the occupancy factors of octahedral sites shows that lepidolites (1.5 ≤ x ≤ 2.0) represent a solid solution series with polylithionite and trilithionite as the endmembers. In the case of the Li-muscovites (0.0 ≤ x ≤ 1.5) the 1M/2M1-ratio depends on the amount of impurity phases like eucryptite or sanidine depleting the reaction mixture of Li or Al. There is no solid solution between trilithionite and muscovite, instead, the Li-muscovite crystals consist of domains differing in the relative proportions of muscovite and trilithionite. The overall composition of the synthesized micas which consist of two polytypes can be characterised by 29Si, 1H and 19F MAS NMR spectroscopy. The Si/Al ratio in the tetrahedral layers and thus the content of [4]Al was calculated by analysing the signal intensities of the 29Si MAS NMR experiments. The Li content xest was calculated from the measured tetrahedral Si/Al ratio of the 29Si MAS NMR signals. The calculated Li-contents xest of samples between polylithionite and trilithionite agree with the expected values. F-rich samples show slightly increased values and the OH-samples lower values. Lepidolites containing exclusively F (x = 1.5 – 2.0, y = 0.0) could be obtained, but no lepidolite with only OH (x = 1.5 - 2.0 and y = 2.0) was observed after synthesis. With decreasing Li-content, x ≤ 1.2, Li-muscovites containing mostly hydroxyl (y > 1.0) are formed. It was possible to synthesise fluorine containing micas with a Licontent as low as 0.3 and y = 0.2 - 1.8. The 19F and 1H MAS NMR experiments that F and OH are not distributed statistically but local structural preferences exist. F is attracted by Li-rich and OH by Al-rich environments.

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