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Future water-rock interaction in deep repository of spent nuclear fuel

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F17%3A00097564" target="_blank" >RIV/00216224:14310/17:00097564 - isvavai.cz</a>

  • Result on the web

    <a href="https://www.sciencedirect.com/science/article/pii/S1878522016300455" target="_blank" >https://www.sciencedirect.com/science/article/pii/S1878522016300455</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1016/j.proeps.2016.12.013" target="_blank" >10.1016/j.proeps.2016.12.013</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Future water-rock interaction in deep repository of spent nuclear fuel

  • Original language description

    A deep geological repository of spent nuclear fuel has to be safe for at least 100 thousand years. During this time, water–rock interaction on surface as well as in the rock around the repository will progress. All exogenous processes will depend on future evolution of climate. Based on the research of Quaternary sediments, three limiting scenarios of future climate evolution are considered: Maximum cooling and drying in glacial periods; maximum warming and moistening in interglacial periods and climate evolution affected by elevated concentrations of CO2 in the atmosphere. Formation of permafrost, infiltration of melted water and oxidation will influence chemical composition of ground water. Two analogues of the changes are presented. They are ground waters in two mines in the Bohemian massive: (1) Mine “Svornost” in an abandoned historical uranium deposit Jáchymov Joachimstahl), (2) underground research facility of “Bukov” near the uranium deposit of Rožná. Ground water was sampled from surface to a depth of 1200 m. The water–rock interaction during the infiltration and flow of ground water is the cause of the observed stratification of the chemical composition. The chemical composition of the collected samples indicate a probable future composition of ground water within the repository.

  • Czech name

  • Czech description

Classification

  • Type

    D - Article in proceedings

  • CEP classification

  • OECD FORD branch

    10500 - Earth and related environmental sciences

Result continuities

  • Project

  • Continuities

    V - Vyzkumna aktivita podporovana z jinych verejnych zdroju

Others

  • Publication year

    2017

  • Confidentiality

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

Data specific for result type

  • Article name in the collection

    Procedia Earth and Planetary Science

  • ISBN

  • ISSN

    1878-5220

  • e-ISSN

  • Number of pages

    4

  • Pages from-to

    100-103

  • Publisher name

    ELSEVIER SCIENCE BV,

  • Place of publication

    Amsterdam

  • Event location

    Evora, Portugal

  • Event date

    Oct 16, 2016

  • Type of event by nationality

    WRD - Celosvětová akce

  • UT code for WoS article

    000398020400026