Water Vapor Diffusion and Adsorption of Sandstones: Influence of Rock Texture and Composition

The term sandstone is used for wide range of rocks containing quartz clasts which can be cemented by secondary precipitated quartz or calcite; moreover the space between clasts can be filled by matrix. These facts result in existence of numerous rocks having highly various properties. Sandstones hav...

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Main Authors: Martin Keppert, Jaromír Žumár, Monika Čáchová, Dana Koňáková, Petr Svora, Zbyšek Pavlík, Eva Vejmelková, Robert Černý
Format: Article
Language:English
Published: Wiley 2016-01-01
Series:Advances in Materials Science and Engineering
Online Access:http://dx.doi.org/10.1155/2016/8039748
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author Martin Keppert
Jaromír Žumár
Monika Čáchová
Dana Koňáková
Petr Svora
Zbyšek Pavlík
Eva Vejmelková
Robert Černý
author_facet Martin Keppert
Jaromír Žumár
Monika Čáchová
Dana Koňáková
Petr Svora
Zbyšek Pavlík
Eva Vejmelková
Robert Černý
author_sort Martin Keppert
collection DOAJ
description The term sandstone is used for wide range of rocks containing quartz clasts which can be cemented by secondary precipitated quartz or calcite; moreover the space between clasts can be filled by matrix. These facts result in existence of numerous rocks having highly various properties. Sandstones have been used as construction materials due to their good accessibility and workability. Since most of sandstones are porous, water vapor can penetrate through sandstone constructions. The rate of water vapor diffusion, as well as the vapor sorption isotherm, was determined for range of sandstone types. The diffusion resistance factor was found to be dependent on the total porosity of sandstone but the sorption behavior was strongly influenced by nature of the particular sandstone; the specific surface area of stone and presence of clay matrix are determining its sorption isotherm. The published data enable estimating (i) diffusion resistance factor of a sandstone via knowledge of its total porosity and (ii) the sorption isotherm via knowledge of the stone’s nature and specific surface area. This approach can significantly reduce the time necessary to acquire vapor-related properties of a sandstone.
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institution Kabale University
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series Advances in Materials Science and Engineering
spelling doaj-art-4f34921b1bc2406fa51b363ea2355e462025-02-03T05:47:33ZengWileyAdvances in Materials Science and Engineering1687-84341687-84422016-01-01201610.1155/2016/80397488039748Water Vapor Diffusion and Adsorption of Sandstones: Influence of Rock Texture and CompositionMartin Keppert0Jaromír Žumár1Monika Čáchová2Dana Koňáková3Petr Svora4Zbyšek Pavlík5Eva Vejmelková6Robert Černý7Department of Materials Engineering and Chemistry, Faculty of Civil Engineering, Czech Technical University in Prague, Thákurova 7, 166 29 Prague 6, Czech RepublicDepartment of Materials Engineering and Chemistry, Faculty of Civil Engineering, Czech Technical University in Prague, Thákurova 7, 166 29 Prague 6, Czech RepublicDepartment of Materials Engineering and Chemistry, Faculty of Civil Engineering, Czech Technical University in Prague, Thákurova 7, 166 29 Prague 6, Czech RepublicDepartment of Materials Engineering and Chemistry, Faculty of Civil Engineering, Czech Technical University in Prague, Thákurova 7, 166 29 Prague 6, Czech RepublicDepartment of Materials Engineering and Chemistry, Faculty of Civil Engineering, Czech Technical University in Prague, Thákurova 7, 166 29 Prague 6, Czech RepublicDepartment of Materials Engineering and Chemistry, Faculty of Civil Engineering, Czech Technical University in Prague, Thákurova 7, 166 29 Prague 6, Czech RepublicDepartment of Materials Engineering and Chemistry, Faculty of Civil Engineering, Czech Technical University in Prague, Thákurova 7, 166 29 Prague 6, Czech RepublicDepartment of Materials Engineering and Chemistry, Faculty of Civil Engineering, Czech Technical University in Prague, Thákurova 7, 166 29 Prague 6, Czech RepublicThe term sandstone is used for wide range of rocks containing quartz clasts which can be cemented by secondary precipitated quartz or calcite; moreover the space between clasts can be filled by matrix. These facts result in existence of numerous rocks having highly various properties. Sandstones have been used as construction materials due to their good accessibility and workability. Since most of sandstones are porous, water vapor can penetrate through sandstone constructions. The rate of water vapor diffusion, as well as the vapor sorption isotherm, was determined for range of sandstone types. The diffusion resistance factor was found to be dependent on the total porosity of sandstone but the sorption behavior was strongly influenced by nature of the particular sandstone; the specific surface area of stone and presence of clay matrix are determining its sorption isotherm. The published data enable estimating (i) diffusion resistance factor of a sandstone via knowledge of its total porosity and (ii) the sorption isotherm via knowledge of the stone’s nature and specific surface area. This approach can significantly reduce the time necessary to acquire vapor-related properties of a sandstone.http://dx.doi.org/10.1155/2016/8039748
spellingShingle Martin Keppert
Jaromír Žumár
Monika Čáchová
Dana Koňáková
Petr Svora
Zbyšek Pavlík
Eva Vejmelková
Robert Černý
Water Vapor Diffusion and Adsorption of Sandstones: Influence of Rock Texture and Composition
Advances in Materials Science and Engineering
title Water Vapor Diffusion and Adsorption of Sandstones: Influence of Rock Texture and Composition
title_full Water Vapor Diffusion and Adsorption of Sandstones: Influence of Rock Texture and Composition
title_fullStr Water Vapor Diffusion and Adsorption of Sandstones: Influence of Rock Texture and Composition
title_full_unstemmed Water Vapor Diffusion and Adsorption of Sandstones: Influence of Rock Texture and Composition
title_short Water Vapor Diffusion and Adsorption of Sandstones: Influence of Rock Texture and Composition
title_sort water vapor diffusion and adsorption of sandstones influence of rock texture and composition
url http://dx.doi.org/10.1155/2016/8039748
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