Hygric Properties of Sandstones as a Function of Porosity

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68407700%3A21110%2F15%3A00230384" target="_blank" >RIV/68407700:21110/15:00230384 - isvavai.cz</a>

Výsledek na webu

<a href="http://dx.doi.org/10.1063/1.4912638" target="_blank" >http://dx.doi.org/10.1063/1.4912638</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1063/1.4912638" target="_blank" >10.1063/1.4912638</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Hygric Properties of Sandstones as a Function of Porosity

Popis výsledku v původním jazyce

Sandstones, clastic sedimentary rocks, were used as load-bearing materials for centuries. Even though nowadays these natural materials are usually used as decorative or facing materials, sandstones still belong to the group of building materials. Rocks,which can be called sandstones (from a geological point of view), vary widely. All properties depend mainly on the mineralogical composition, granularity and pore system of an individual material. Because the aim of this study was to find out the relationship between hygric properties and pore size distribution, selected materials differ mainly in their porosity. Mostly quartzose sandstones with an irregular granularity, which are quarried in the Czech Republic, were chosen and experimentally characterised for the purpose of this study. The dependencies of water vapour transport properties on the porosity of quartzose sandstones were found in a form of a power function, while in the case of liquid water transport exponential function fi

Název v anglickém jazyce

Hygric Properties of Sandstones as a Function of Porosity

Popis výsledku anglicky

Sandstones, clastic sedimentary rocks, were used as load-bearing materials for centuries. Even though nowadays these natural materials are usually used as decorative or facing materials, sandstones still belong to the group of building materials. Rocks,which can be called sandstones (from a geological point of view), vary widely. All properties depend mainly on the mineralogical composition, granularity and pore system of an individual material. Because the aim of this study was to find out the relationship between hygric properties and pore size distribution, selected materials differ mainly in their porosity. Mostly quartzose sandstones with an irregular granularity, which are quarried in the Czech Republic, were chosen and experimentally characterised for the purpose of this study. The dependencies of water vapour transport properties on the porosity of quartzose sandstones were found in a form of a power function, while in the case of liquid water transport exponential function fi

Druh

D - Stať ve sborníku

CEP obor

JJ - Ostatní materiály

OECD FORD obor

—

Projekt

—

Návaznosti

S - Specificky vyzkum na vysokych skolach

Rok uplatnění

2015

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název statě ve sborníku

PROCEEDINGS OF THE INTERNATIONAL CONFERENCE ON NUMERICAL ANALYSIS AND APPLIED MATHEMATICS 2014 (ICNAAM-2014)

ISBN

978-0-7354-1287-3

ISSN

0094-243X

e-ISSN

—

Počet stran výsledku

5

Strana od-do

"410009-1"-"410009-4"

Název nakladatele

AIP Conference Proceedings

Místo vydání

New York

Místo konání akce

Rhodes, Greece

Datum konání akce

22. 9. 2014

Typ akce podle státní příslušnosti

WRD - Celosvětová akce

Kód UT WoS článku

000355339702053