The smectites were modified with different types of alkylammonium cations. The X-ray powder diffraction was used to calculate the values of the basal space of the modified smectites to confirm the intercalation of cations into the structure. The montmorillonites were also characterized by means of FTIR spectroscopy, which proved sorption or intercalation of the alkylammonium cations too. Thermal behaviour of the smectites was investigated by simultaneous thermogravimetry and differential thermal analysis. The temperatures of dehydratation and dehydroxylation and the temperatures related to total melting and recrystallization generally changed. Study of temperatures changes together with determination of kinetic parameters helped to obtained...
Clays are involved in a variety of natural and managed processes, and calculation of their stability...
International audienceThe aim of the present study was to investigate the detailed evolution of the ...
Smectites are one of the most important groups of phyllosilicates found in soils and sediments, and ...
The clay minerals were modified by two alkylammonium cations under sorption procedure. T X-ray powde...
Due to their special features smectites, dioctahedral smectites in particular, are widely used in a ...
The thermal dehydration of a series of smectites has been investigated by X-ray methods. It has been...
The present investigation was undertaken to obtain information about the structural, thermal, morpho...
Abstract- A series of organic ammonium ions were exchanged onto clay minerals montmorillonite and he...
The decomposition mechanism of intercalated montmorillonites at a particular temperature region and ...
High resolution thermogravimetric analysis has been used to study the thermal decomposition of montm...
Three n-alkylammonium salts of varying alkyl chain length were ion exchanged with montmorillonites (...
International audienceThe hydrothermal reactivity of the <1 μm fraction, K-saturated SWy-2 Wyoming l...
Emanation thermal analysis (ETA) and thermogravimetry measured in the range 20-1000 degrees C was us...
The swelling property of smectite is dominated by the hydration of exchangeable cations in the inter...
Abstract--Smectites are one of the most important groups of phyllositicates found in soils and sedim...
Clays are involved in a variety of natural and managed processes, and calculation of their stability...
International audienceThe aim of the present study was to investigate the detailed evolution of the ...
Smectites are one of the most important groups of phyllosilicates found in soils and sediments, and ...
The clay minerals were modified by two alkylammonium cations under sorption procedure. T X-ray powde...
Due to their special features smectites, dioctahedral smectites in particular, are widely used in a ...
The thermal dehydration of a series of smectites has been investigated by X-ray methods. It has been...
The present investigation was undertaken to obtain information about the structural, thermal, morpho...
Abstract- A series of organic ammonium ions were exchanged onto clay minerals montmorillonite and he...
The decomposition mechanism of intercalated montmorillonites at a particular temperature region and ...
High resolution thermogravimetric analysis has been used to study the thermal decomposition of montm...
Three n-alkylammonium salts of varying alkyl chain length were ion exchanged with montmorillonites (...
International audienceThe hydrothermal reactivity of the <1 μm fraction, K-saturated SWy-2 Wyoming l...
Emanation thermal analysis (ETA) and thermogravimetry measured in the range 20-1000 degrees C was us...
The swelling property of smectite is dominated by the hydration of exchangeable cations in the inter...
Abstract--Smectites are one of the most important groups of phyllositicates found in soils and sedim...
Clays are involved in a variety of natural and managed processes, and calculation of their stability...
International audienceThe aim of the present study was to investigate the detailed evolution of the ...
Smectites are one of the most important groups of phyllosilicates found in soils and sediments, and ...