The process of water vapour adsorption is reversible in the case of zeolites because of their rigid microporous structure, but irreversible in the case of clay minerals because of swelling that takes place in their sheet structure. The Polanyi-Dubinin theory applicable for zeolites is also used for clay minerals in the region of homogeneous hydration and thermodynamic functions are calculated from the Dubinin-Astakhov plot.Simonot-Grange Marie-Hélène. Thermodynamic properties of adsorbed water in zeolites and comparison with clay minerals. In: Proceedings of the 9th international Clay Conference, Strasbourg, 1989. Vol III : Geochemistry of clays. Nuclear waste disposal. Strasbourg : Institut de Géologie – Université Louis-Pasteur, 1990. pp....
Many of the most important properties of the clay minerals are in reality properties of the complex ...
An investigation was carried out to determine the extent of relations between various structural pro...
The study of swelling in the presence of water vapor of two monoionic montmorillonites (Na+ and Ca++...
The process of water vapour adsorption is reversible in the case of zeolites because of their rigid ...
The sepiolite dehydration curve under vacuum shows that the externa] and zeolitic water are lost at ...
Methods are presented for determining partial and integral thermodynamic quantities for the change i...
Abstract The integral thermodynamic quantities of adsorbed water on Na- and Ca-montmorillonite have ...
Abstract--The application of the Frenkel-Halsey-Hiil (FHH) formalism to the water desorption iso-the...
The zeolites constitute a group of minerals of much interest from geological, mineralogical and tech...
We studied the mathematical model of interaction with water of two natural minerals – amorphous, unc...
In this work, four zeolite-bearing materials (three naturally occurring and one of synthetic origin)...
Deep disposal concepts are usually based on a multibarrier concept that may involve a physical conta...
The influence of decationization and dealumination on adsorption of water with rock from Transcarpat...
In this manuscript, the amount of water vapour uptakes on zeolites (types AQSOA-Z01, Z02 and Z05) un...
After recalling the results obtained for Ca++ saturated clay minerals, the author studies adsorption...
Many of the most important properties of the clay minerals are in reality properties of the complex ...
An investigation was carried out to determine the extent of relations between various structural pro...
The study of swelling in the presence of water vapor of two monoionic montmorillonites (Na+ and Ca++...
The process of water vapour adsorption is reversible in the case of zeolites because of their rigid ...
The sepiolite dehydration curve under vacuum shows that the externa] and zeolitic water are lost at ...
Methods are presented for determining partial and integral thermodynamic quantities for the change i...
Abstract The integral thermodynamic quantities of adsorbed water on Na- and Ca-montmorillonite have ...
Abstract--The application of the Frenkel-Halsey-Hiil (FHH) formalism to the water desorption iso-the...
The zeolites constitute a group of minerals of much interest from geological, mineralogical and tech...
We studied the mathematical model of interaction with water of two natural minerals – amorphous, unc...
In this work, four zeolite-bearing materials (three naturally occurring and one of synthetic origin)...
Deep disposal concepts are usually based on a multibarrier concept that may involve a physical conta...
The influence of decationization and dealumination on adsorption of water with rock from Transcarpat...
In this manuscript, the amount of water vapour uptakes on zeolites (types AQSOA-Z01, Z02 and Z05) un...
After recalling the results obtained for Ca++ saturated clay minerals, the author studies adsorption...
Many of the most important properties of the clay minerals are in reality properties of the complex ...
An investigation was carried out to determine the extent of relations between various structural pro...
The study of swelling in the presence of water vapor of two monoionic montmorillonites (Na+ and Ca++...