2021
DOI: 10.1007/s11182-021-02301-w
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Modeling of Dielectric Relaxation in Clays at Negative and Positive Temperatures

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Cited by 4 publications
(3 citation statements)
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“…At low temperatures (24-30 o C), the intensity of the peaks where significantly low which indicate less adjustment between the frequency of applied field and the slow motion of the new charge carriers. Due to the steric effect of the intercalated organic molecule which somehow blocks the charge carrier movements, low temperatures could not provide enough energy to rotate or change the conformation of new organic substitution within bentonite layers to allow the charge carriers to have more freedom of motion [21]. However, at higher temperatures 40-60 o C, the intensities are noticeably higher due to higher energies provided by increasing the temperature and enough energy for rotating the organic conformation as well as reducing the constriction of charge carriers.…”
Section: Dielectric Permittivitymentioning
confidence: 99%
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“…At low temperatures (24-30 o C), the intensity of the peaks where significantly low which indicate less adjustment between the frequency of applied field and the slow motion of the new charge carriers. Due to the steric effect of the intercalated organic molecule which somehow blocks the charge carrier movements, low temperatures could not provide enough energy to rotate or change the conformation of new organic substitution within bentonite layers to allow the charge carriers to have more freedom of motion [21]. However, at higher temperatures 40-60 o C, the intensities are noticeably higher due to higher energies provided by increasing the temperature and enough energy for rotating the organic conformation as well as reducing the constriction of charge carriers.…”
Section: Dielectric Permittivitymentioning
confidence: 99%
“…Bore et al [24] used a high frequency dielectric relaxation spectroscopy to estimate the interfacial water molecules on the clay interlayers, whereas belyaeva et al [22] studied the saline soils by monitoring the complex dielectric permittivity at frequency 10 KHz to 8 GHz. Repin et al [21] proposed a modeling approach to calculate the dielectric relaxation of different clay mentals at various temperatures. The aim of this study is to investigate the effect of intercalating organic species, particularly Schiff base derivative, within the layer of montmorillonite clay minerals on the electrical and dielectric properties of the formed composite, as well as to estimate the activation energy of charge carriers and the relaxation time.…”
Section: Introductionmentioning
confidence: 99%
“…Many studies had been carried out to investigate the electrical behavior of clay minerals and its complexes with organic species. Bore et al [39] used a high frequency dielectric relaxation spectroscopy to estimate the interfacial water molecules on the clay interlayers, whereas belyaeva et al [40,41] proposed a modeling approach to calculate the dielectric relaxation of different clay mentals at various temperatures.…”
Section: Introductionmentioning
confidence: 99%