Detailed Information on Publication Record
2008
Mine Water Stratification at Abandoned Mines and its Geochemical Model
ZEMAN, Josef, Irena ŠUPÍKOVÁ and Miroslav ČERNÍKBasic information
Original name
Mine Water Stratification at Abandoned Mines and its Geochemical Model
Name in Czech
Stratifikace důlních vod opuštěných dolů a její geochemický model
Authors
ZEMAN, Josef (203 Czech Republic, guarantor), Irena ŠUPÍKOVÁ (203 Czech Republic) and Miroslav ČERNÍK (203 Czech Republic)
Edition
Ostrava, Mine Water and the Environment PROCEEDINGS, 10th International Mine Water Association Congress, June 2-5. 2008, Karlovy Vary, Czech Republic, p. 183-186, 627 pp. 2008
Publisher
VŠB - Technical University of Ostrava
Other information
Language
English
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/00216224:14310/08:00036731
Organization unit
Faculty of Science
ISBN
978-80-248-1767-5
UT WoS
000276841700045
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
Změněno: 1/10/2009 06:47, doc. RNDr. Josef Zeman, CSc.
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
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