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New imformations about the building of calcite straw stalactites

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F04%3A00011765" target="_blank" >RIV/00216224:14310/04:00011765 - isvavai.cz</a>

  • Alternative codes found

    RIV/61989592:15310/04:00002451

  • Result on the web

  • DOI - Digital Object Identifier

Alternative languages

  • Result language

    čeština

  • Original language name

    Nové poznatky o stavbě a vývoji kalcitových brček

  • Original language description

    Based on the hypothesis that the destruction of calcite speleothems in the Moravian Karst caves could be consequence of chemical corrosion, detail mineralogical study of straw stalactites was accomplished. In stalactite wall, calcite was recognized as asingle phase. The stalactite wall was built by three layers: (1) outer one (porous, finely grained, to 0.1 mm thick), (2) middle one (mono-crystalline, to 0.6 mm thick), and (3) inner one (to 1 mm thick, composed from many single crystals, chaotically distributed, 0-0.3 in diameter). The mono-crystalline layers werw typically cracked due to calcite excellent fissionability along rhombohedron. An ocassionally observed crack widening could be induced by corrosion. Majority of stalactite corruption, however, resulted from mechanical breakages in the direction of the fissile cracks. Zhe chemical corrosion impacts were positively identified only on the outside wall of stalactite.

  • Czech name

    Nové poznatky o stavbě a vývoji kalcitových brček

  • Czech description

    Based on the hypothesis that the destruction of calcite speleothems in the Moravian Karst caves could be consequence of chemical corrosion, detail mineralogical study of straw stalactites was accomplished. In stalactite wall, calcite was recognized as asingle phase. The stalactite wall was built by three layers: (1) outer one (porous, finely grained, to 0.1 mm thick), (2) middle one (mono-crystalline, to 0.6 mm thick), and (3) inner one (to 1 mm thick, composed from many single crystals, chaotically distributed, 0-0.3 in diameter). The mono-crystalline layers werw typically cracked due to calcite excellent fissionability along rhombohedron. An ocassionally observed crack widening could be induced by corrosion. Majority of stalactite corruption, however, resulted from mechanical breakages in the direction of the fissile cracks. Zhe chemical corrosion impacts were positively identified only on the outside wall of stalactite.

Classification

  • Type

    D - Article in proceedings

  • CEP classification

    DB - Geology and mineralogy

  • OECD FORD branch

Result continuities

  • Project

    <a href="/en/project/GA205%2F03%2F1128" target="_blank" >GA205/03/1128: Recent karst processes: speleothem destruction</a><br>

  • Continuities

    P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Others

  • Publication year

    2004

  • Confidentiality

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

Data specific for result type

  • Article name in the collection

    Sborník IV. vědecké konference s mezinárodní účastí "Výskum, využívanie a ochrana jaskýň"

  • ISBN

    80-8064-201-X

  • ISSN

  • e-ISSN

  • Number of pages

    3

  • Pages from-to

    75-77

  • Publisher name

    Správa slovenských jaskýň

  • Place of publication

    Liptovský Mikuláš-Žilina

  • Event location

    Tále

  • Event date

    Oct 5, 2003

  • Type of event by nationality

    EUR - Evropská akce

  • UT code for WoS article