Utilization of Olsi-Dranonin uranium deposit after mine closure

RAPANTOVÁ, Naďa, Arnošt GRMELA, Bedřich MICHÁLEK, Pavol ZÁBOJNÍK and Josef ZEMAN. Utilization of Olsi-Dranonin uranium deposit after mine closure. In Mine Water and the Environment PROCEEDINGS, 10th International Mine Water Association Congress, June 2-5. 2008, Karlovy Vary, Czech Republic. Ostrava: VŠB - Technical University of Ostrava, 2008, p. 221-224, 627 pp. ISBN 978-80-248-1767-5.

Basic information

• Original name: Utilization of Olsi-Dranonin uranium deposit after mine closure
• Name in Czech: Stratifikace důlních vod opuštěných dolů a její geochemický model
• Authors: RAPANTOVÁ, Naďa (203 Czech Republic), Arnošt GRMELA (203 Czech Republic), Bedřich MICHÁLEK (203 Czech Republic), Pavol ZÁBOJNÍK (203 Czech Republic) and Josef ZEMAN (203 Czech Republic, guarantor).
• Edition: Ostrava, Mine Water and the Environment PROCEEDINGS, 10th International Mine Water Association Congress, June 2-5. 2008, Karlovy Vary, Czech Republic, p. 221-224, 627 pp. 2008.
• Publisher: VŠB - Technical University of Ostrava

Other information

• Original language: English
• Type of outcome: Proceedings paper
• Field of Study: Geochemistry
• Country of publisher: Czech Republic
• Confidentiality degree: is not subject to a state or trade secret
• RIV identification code: RIV/00216224:14310/08:00036732
• Organization unit: Faculty of Science
• ISBN: 978-80-248-1767-5
• UT WoS: 000276841700054
• Keywords (in Czech): důlní voda; stratifikace; geochemický model; redox potenciál; zatopený důl
• Keywords in English: mine water; stratification; geochemical model; redox potential; mine flooded
• Tags: International impact, Reviewed

Abstract

Important factor which play main role at high concentrated mine water formation is stratification of mine water. The stratification of mine water body was observed on all studied ore and coal deposits (five) by in-depth resistivity and temperature logging, and mine water sampling. On Oslavany coal mine Jindřich II there can be identified three layers of stratified mine water. Sharp transition between layers and very distinctive concentrations of dissolved solids are characteristic. Stratification is stable despite of mine water discharge about 50 L/s. Detailed geochemical model of stratified layers formation and their time evolution is be presented.

Abstract (in Czech)

Important factor which play main role at high concentrated mine water formation is stratification of mine water. The stratification of mine water body was observed on all studied ore and coal deposits (five) by in-depth resistivity and temperature logging, and mine water sampling. On Oslavany coal mine Jindřich II there can be identified three layers of stratified mine water. Sharp transition between layers and very distinctive concentrations of dissolved solids are characteristic. Stratification is stable despite of mine water discharge about 50 L/s. Detailed geochemical model of stratified layers formation and their time evolution is be presented.

Links

• MSM0021622412, plan (intention): Name: Interakce mezi chemickými látkami, prostředím a biologickými systémy a jejich důsledky na globální, regionální a lokální úrovni (INCHEMBIOL) (Acronym: INCHEMBIOL)

Investor: Ministry of Education, Youth and Sports of the CR, Interactions among the chemicals, environment and biological systems and their consequences on the global, regional and local scales (INCHEMBIOL)