Hygric Transport Parameters of Several Kinds of Sandstones

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68407700%3A21110%2F14%3A00219141" target="_blank" >RIV/68407700:21110/14:00219141 - isvavai.cz</a>

Výsledek na webu

<a href="http://dx.doi.org/10.4028/www.scientific.net/AMM.621.24" target="_blank" >http://dx.doi.org/10.4028/www.scientific.net/AMM.621.24</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.4028/www.scientific.net/AMM.621.24" target="_blank" >10.4028/www.scientific.net/AMM.621.24</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Hygric Transport Parameters of Several Kinds of Sandstones

Popis výsledku v původním jazyce

Hygric transport properties belong to a group of important characteristics from a construction design point of view. Since a content of water (at whatever state) could lead to degradation processes of materials whether by phase changes or by chemical reaction (with any component of water contained), it is important to know an amount of water which can get into the pore structure of a material. Studied materials in this workwere sandstones. Several types of these clastic sedimentary rocks were chosen andexperimental determinations of basic physical properties as well as hygric transport parameters were performed. From the achieved results,it is obvious that the main influence on hygric transport characteristics has the open porosity, in particular thepore structure.The higher porosity is the higher amount of water can be transported through the sandstones.

Název v anglickém jazyce

Hygric Transport Parameters of Several Kinds of Sandstones

Popis výsledku anglicky

Hygric transport properties belong to a group of important characteristics from a construction design point of view. Since a content of water (at whatever state) could lead to degradation processes of materials whether by phase changes or by chemical reaction (with any component of water contained), it is important to know an amount of water which can get into the pore structure of a material. Studied materials in this workwere sandstones. Several types of these clastic sedimentary rocks were chosen andexperimental determinations of basic physical properties as well as hygric transport parameters were performed. From the achieved results,it is obvious that the main influence on hygric transport characteristics has the open porosity, in particular thepore structure.The higher porosity is the higher amount of water can be transported through the sandstones.

Druh

D - Stať ve sborníku

CEP obor

JN - Stavebnictví

OECD FORD obor

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Projekt

—

Návaznosti

S - Specificky vyzkum na vysokych skolach

Rok uplatnění

2014

Kód důvěrnosti údajů

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

Název statě ve sborníku

Applied Research in Materials and Mechanics Engineering

ISBN

978-3-03835-196-2

ISSN

1660-9336

e-ISSN

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Počet stran výsledku

6

Strana od-do

24-29

Název nakladatele

Trans Tech Publications

Místo vydání

Curich

Místo konání akce

London

Datum konání akce

21. 6. 2014

Typ akce podle státní příslušnosti

WRD - Celosvětová akce

Kód UT WoS článku

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