D
2008
Utilization of Olsi-Dranonin uranium deposit after mine closure
RAPANTOVÁ, Naďa, Arnošt GRMELA, Bedřich MICHÁLEK, Pavol ZÁBOJNÍK, Josef ZEMAN et. al.
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
Type of outcome
Stať ve sborníku
Field of Study
Geochemistry
Country of publisher
Czech Republic
Confidentiality degree
není předmětem státního či obchodního tajemství
RIV identification code
RIV/00216224:14310/08:00036732
Organization unit
Faculty of Science
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
V originále
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.
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) |
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Displayed: 5/11/2024 20:20