Water Vapor Diffusion and Adsorption of Sandstones: Influence of Rock Texture and Composition
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68407700%3A21110%2F16%3A00301169" target="_blank" >RIV/68407700:21110/16:00301169 - isvavai.cz</a>
Výsledek na webu
<a href="http://dx.doi.org/10.1155/2016/8039748" target="_blank" >http://dx.doi.org/10.1155/2016/8039748</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1155/2016/8039748" target="_blank" >10.1155/2016/8039748</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Water Vapor Diffusion and Adsorption of Sandstones: Influence of Rock Texture and Composition
Popis výsledku v původním jazyce
Thetermsandstone is used for wide range of rocks containing quartz clastswhich 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 ofwater vapor diffusion, as well as the vapor sorption isotherm, was determined for range of sandstone types.The diffusion resistance factorwas 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.
Název v anglickém jazyce
Water Vapor Diffusion and Adsorption of Sandstones: Influence of Rock Texture and Composition
Popis výsledku anglicky
Thetermsandstone is used for wide range of rocks containing quartz clastswhich 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 ofwater vapor diffusion, as well as the vapor sorption isotherm, was determined for range of sandstone types.The diffusion resistance factorwas 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.
Klasifikace
Druh
J<sub>x</sub> - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
CEP obor
JN - Stavebnictví
OECD FORD obor
—
Návaznosti výsledku
Projekt
<a href="/cs/project/GA14-17207S" target="_blank" >GA14-17207S: Transportní parametry a trvanlivost porézních hornin</a><br>
Návaznosti
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)
Ostatní
Rok uplatnění
2016
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Advances in Materials Science and Engineering
ISSN
1687-8434
e-ISSN
—
Svazek periodika
2016
Číslo periodika v rámci svazku
8039748
Stát vydavatele periodika
US - Spojené státy americké
Počet stran výsledku
7
Strana od-do
—
Kód UT WoS článku
000379869300001
EID výsledku v databázi Scopus
2-s2.0-84978945315