Formation of 2:1 Li-Fe-phyllosilicate with montmorillonite-like structure in hydrothermal conditions
Abstract
Here, we report on hydrothermal synthesis and structural characterization of Li-Fe-montmorillonite (MMT). To date, this 2:1 type phyllosilicate attracts attention due to such properties as high ion mobility, hydrophilicity, electrical and thermal resistance. Due to that, various MMTs may serve as perspective components of Li-ion batteries (electrolyte and separator fillers, as well as protective buffer layer on top of Li metal anode). Scarce data on synthetic Li-Fe3+-MMTs motivated us to investigate formation process and structure features of such phyllosilicate by X-ray diffraction, UV-visible and Mössbauer spectroscopy, and other methods. We established critical Fe3+ content and temperature range needed for almost single-phase MMTs formation. Around 20% of total Fe may occupy tetrahedral site of MMT layer. Thermal behavior of Li-Fe-MMT strongly depends on hydrothermal synthesis conditions because of different Li+ amount present in the interlayer space and in the layer vacancies.
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About the Authors
Asiyat A IyakhmaevaRussian Federation
Ekaterina K Khrapova
Russian Federation
Lev A Lebedev
Russian Federation
Nadezhda V Glebova
Valentin G Semenov
Russian Federation
Andrey A Kopylov
Russian Federation
Andrei A Krasilin
Russian Federation
Review
For citations:
Iyakhmaeva A.A., Khrapova E.K., Lebedev L.A., Glebova N.V., Semenov V.G., Kopylov A.A., Krasilin A.A. Formation of 2:1 Li-Fe-phyllosilicate with montmorillonite-like structure in hydrothermal conditions. Nanosystems: Physics, Chemistry, Mathematics. 2025;16(6).
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