2008
Mine Water Stratification at Abandoned Mines and its Geochemical Model
ZEMAN, Josef; Irena ŠUPÍKOVÁ a Miroslav ČERNÍKZákladní údaje
Originální název
Mine Water Stratification at Abandoned Mines and its Geochemical Model
Název česky
Stratifikace důlních vod opuštěných dolů a její geochemický model
Autoři
ZEMAN, Josef (203 Česká republika, garant); Irena ŠUPÍKOVÁ (203 Česká republika) a Miroslav ČERNÍK (203 Česká republika)
Vydání
Ostrava, Mine Water and the Environment PROCEEDINGS, 10th International Mine Water Association Congress, June 2-5. 2008, Karlovy Vary, Czech Republic, od s. 183-186, 627 s. 2008
Nakladatel
VŠB - Technical University of Ostrava
Další údaje
Jazyk
angličtina
Typ výsledku
Stať ve sborníku
Obor
Geochemie
Stát vydavatele
Česká republika
Utajení
není předmětem státního či obchodního tajemství
Kód RIV
RIV/00216224:14310/08:00036731
Organizační jednotka
Přírodovědecká fakulta
ISBN
978-80-248-1767-5
UT WoS
000276841700045
Klíčová slova česky
důlní voda; stratifikace; geochemický model; redox potenciál; zatopený důl
Klíčová slova anglicky
mine water; stratification; geochemical model; redox potential; mine flooded
Příznaky
Mezinárodní význam, Recenzováno
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.
Česky
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.
Návaznosti
| MSM0021622412, záměr |
|