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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.

About the Authors

Asiyat A Iyakhmaeva
Ioffe Institute
Russian Federation


Ekaterina K Khrapova
Ioffe Institute
Russian Federation


Lev A Lebedev
Ioffe Institute
Russian Federation


Nadezhda V Glebova
Ioffe Institute


Valentin G Semenov
Saint Petersburg State University
Russian Federation


Andrey A Kopylov
RITVERC JSC
Russian Federation


Andrei A Krasilin
Ioffe Institute
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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ISSN 2220-8054 (Print)
ISSN 2305-7971 (Online)