Soapstone as a locally used and limited sculptural material in remote area of Northern Moravia (Czech Republic)
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60461446%3A52810%2F15%3A%230000198" target="_blank" >RIV/60461446:52810/15:#0000198 - isvavai.cz</a>
Nalezeny alternativní kódy
RIV/68145535:_____/15:00432637
Výsledek na webu
<a href="http://link.springer.com/article/10.1007%2Fs12665-014-3742-3" target="_blank" >http://link.springer.com/article/10.1007%2Fs12665-014-3742-3</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1007/s12665-014-3742-3" target="_blank" >10.1007/s12665-014-3742-3</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Soapstone as a locally used and limited sculptural material in remote area of Northern Moravia (Czech Republic)
Popis výsledku v původním jazyce
In contrast to Nordic countries, talc-rich rocks (massive and schistose talc-bearing rocks—talcite, magnesite-talc schists, chlorite-talc schists, and/or chloriteactinolite-talc schists often loosely classified as soapstone) represented practically an unknown natural building and sculptural stone in the Czech Republic. This extraordinary material was quarried and used in the only region of the Czech Republic where Sobotín amphibolite massif (Šumperk district, northern Moravia) outcrops. Metamorphosed basic igneous rocks contain small lenses of soapstone that were exploited in the past and used not only for refraktory purposes but also as a construction and sculptural material. Occurrences of "Sobotín" soapstone show distinct zone macrofabric marked by the occurrence of massive Soapstone in the core that gradually changes to talc-dominant schists, later to ctinolite/tremolite-rich schists and finally to chlorite schists at the contact with surrounding amphibolites. The most typical "Sobotín" soapstone exhibits high density (up to 2,900 kg m-3), low water uptake (maximum 0.68 wt %), favorable dynamic elastic properties (P-wave velocity 5,340–5,840 m s-1, S-wave velocity 2,900–3,300 m s-1), and mechanical properties (tensile splitting strength 5.2–6.9 MPa, uniaxial compressive strength 17.5–24.1 MPa). "Sobotín" soapstone is relatively resistant to weathering action although schistose varieties show typical delamination when exposed to frequent freeze/thaw cycling in harsh mountainous environment. Field survey of monuments, architectural and building artefacts made from "Sobotín" soapstone contributed to our knowledge on duration of exploitation of "Sobotín" Soapstone that was for sure utilised from the second half of seventeen century till the beginning of the twenty century. The most characteristic feature of "Sobotín" soapstone is its strict local use on the territory of about 20 villages surrounding previously exploited soapstone lenses.
Název v anglickém jazyce
Soapstone as a locally used and limited sculptural material in remote area of Northern Moravia (Czech Republic)
Popis výsledku anglicky
In contrast to Nordic countries, talc-rich rocks (massive and schistose talc-bearing rocks—talcite, magnesite-talc schists, chlorite-talc schists, and/or chloriteactinolite-talc schists often loosely classified as soapstone) represented practically an unknown natural building and sculptural stone in the Czech Republic. This extraordinary material was quarried and used in the only region of the Czech Republic where Sobotín amphibolite massif (Šumperk district, northern Moravia) outcrops. Metamorphosed basic igneous rocks contain small lenses of soapstone that were exploited in the past and used not only for refraktory purposes but also as a construction and sculptural material. Occurrences of "Sobotín" soapstone show distinct zone macrofabric marked by the occurrence of massive Soapstone in the core that gradually changes to talc-dominant schists, later to ctinolite/tremolite-rich schists and finally to chlorite schists at the contact with surrounding amphibolites. The most typical "Sobotín" soapstone exhibits high density (up to 2,900 kg m-3), low water uptake (maximum 0.68 wt %), favorable dynamic elastic properties (P-wave velocity 5,340–5,840 m s-1, S-wave velocity 2,900–3,300 m s-1), and mechanical properties (tensile splitting strength 5.2–6.9 MPa, uniaxial compressive strength 17.5–24.1 MPa). "Sobotín" soapstone is relatively resistant to weathering action although schistose varieties show typical delamination when exposed to frequent freeze/thaw cycling in harsh mountainous environment. Field survey of monuments, architectural and building artefacts made from "Sobotín" soapstone contributed to our knowledge on duration of exploitation of "Sobotín" Soapstone that was for sure utilised from the second half of seventeen century till the beginning of the twenty century. The most characteristic feature of "Sobotín" soapstone is its strict local use on the territory of about 20 villages surrounding previously exploited soapstone lenses.
Klasifikace
Druh
J<sub>x</sub> - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
CEP obor
DB - Geologie a mineralogie
OECD FORD obor
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Návaznosti výsledku
Projekt
<a href="/cs/project/DF13P01OVV008" target="_blank" >DF13P01OVV008: Přírodní kámen v sochařství a architektuře zemí koruny České – komplexní znalostní systém o zdrojích, vlastnostech, využití, trvanlivosti, historie využití, kompatibilitě a vzájemné zaměnitelnosti</a><br>
Návaznosti
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)
Ostatní
Rok uplatnění
2015
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Environmental Earth Sciences
ISSN
1866-6280
e-ISSN
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Svazek periodika
73
Číslo periodika v rámci svazku
8
Stát vydavatele periodika
DE - Spolková republika Německo
Počet stran výsledku
15
Strana od-do
4557-4571
Kód UT WoS článku
000351453600048
EID výsledku v databázi Scopus
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