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Bukov PVP underground research laboratory - geotechnical conditions of construction
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SYSNO ASEP 0460707 Document Type C - Proceedings Paper (int. conf.) R&D Document Type Conference Paper Title Bukov PVP underground research laboratory - geotechnical conditions of construction Author(s) Souček, Kamil (UGN-S) RID, ORCID
Vavro, Martin (UGN-S) RID, ORCID
Staš, Lubomír (UGN-S) RID, ORCID
Koníček, Petr (UGN-S) RID, ORCID
Ptáček, Jiří (UGN-S) RID
Waclawik, Petr (UGN-S) RID
Vavro, Leona (UGN-S) RID
Lednická, Markéta (UGN-S) RID, ORCID
Kaláb, Zdeněk (UGN-S) RID
Šňupárek, Richard (UGN-S) RID
Vondrovic, L. (CZ)Number of authors 11 Source Title Underground Construction Prague 2016, Eastern European Tunneling Conference (EETC 2016). - Praha : ITA-AITES, 2016 / Butovič A. ; Hilar M. - ISBN 978-80-906452-1-9 Number of pages 13 s. Publication form Medium - C Action International Conference Underground Construction Prague 2016 /13./, Eastern European Tunneling Conference (EETC 2016) /3./ Event date 23.05.2016 - 25.05.2016 VEvent location Praha Country CZ - Czech Republic Event type EUR Language eng - English Country CZ - Czech Republic Keywords Bukov URL ; rock mass ; radioactive waste Subject RIV DH - Mining, incl. Coal Mining Institutional support UGN-S - RVO:68145535 Annotation Bukov PVP Underground Research Laboratory (Bukov URL) is designed to be a test site for the evaluation of properties and behavior of the rock mass which is of similar type as selected candidate sites in the Czech Republic. It is situated at a depth corresponding to the proposed storage depth of the final locality for the national deep repository of high-level radioactive waste. The Bukov URL, the construction of which has begun in 2013, is situated in the southern part of the Rožná uranium deposit, at the northeastern periphery of the Strážek Moldanubicum close to its contact with the Svratka Unit. The rock mass is composed of relatively monotonous rock sequences primarily of a volcanosedimentary origin. They are currently represented, due to the subsequent tectonometa-morphic development, by migmatized biotite paragneisses up to stromatitic and/or oftalmitic migmatites, amphibole-biotite to biotite-amphibole gneisses, and amphibolites. The workings of the Bukov URL are situated on the level 12 of the Bukov-1 shaft, at the depth of about 600 m below the earth’s surface. The Bukov URL is still under construction and the research works by the consortium of several organizations – ÚJV Řež, a.s., Czech Geological Survey, Institute of Geonics of the CAS, v.v.i., and Arcadis CZ, a.s. - are carried out simultaneously. The research activities focus on a complex geological and geotechnical characterization of the rock mass of interest, which is vital for the realization of further research in situ. This paper briefly describes the technical solution of the Bukov URL and the process of its construction. Workplace Institute of Geonics Contact Lucie Gurková, lucie.gurkova@ugn.cas.cz, Tel.: 596 979 354 Year of Publishing 2017
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