Wydział Chemii

Karol Kułacz

Kazimierz Orzechowski

Balázs Zsirka

János Kristóf

2022

Applied Clay Science

228

106637/1-106637/10

10.1016/j.clay.2022.106637

Naukowa

Angielski

Artykuł

Nontronite is a swelling clay mineral. Between the layers, it contains water and cations. Nontronite can be easily modified by intercalation. This work focuses on characterizing unmodified nontronite and nontronite intercalated with formamide. Thermal measurements, infrared spectroscopy, X–ray diffraction, and dielectric relaxation measurements were made to evaluate the interactions of the guest molecules with the host layers. A startling effect was observed in dielectric experiments: the low–frequency permittivity detected in nontronite was much larger than in the material intercalated with formamide, the molecule with a high dipole moment. To explain this effect, it was assumed that the low–frequency dielectric relaxation was associated with the movement of interlayer ions. Dehydration of nontronite, which is a stage of preparation for intercalation, can probably fix some ions in hexagonal cavities (privileged positions). Subsequent intercalation of nontronite by formamide does not bring back the mobility of ions, and the low–frequency electric permittivity remains relatively low. To achieve mobility of the cations, an expansion of the interlayer space is required, and ion–dipole interactions with guest molecules should be present.

Clay minerals, Smectites, Dielectric spectroscopy, Thermogravimetry, Infrared spectroscopy, Maxwell-Wagner effect

http://dx.doi.org/10.1016/j.clay.2022.106637

http://www.elsevier.com