Publication details
Geochemický vývoj vod po uzavření a zatopení dolů.
| Title in English | Mine water geochemistry after mine closing and flooding |
|---|---|
| Authors | |
| Year of publication | 2002 |
| Type | Article in Proceedings |
| Conference | Geochémia 2002 |
| MU Faculty or unit | |
| Citation | |
| Field | Geochemistry |
| Keywords | mine water; geochemistry; flooding; uranium; iron; manganese |
| Description | Almost all mines were closed and flooded in ninetieth in Czech Republic. It invoked a range several environmental problems. The main characteristic of general geochemical evolution of mine waters was identified. Despite of deposit type and climate the main factors and features which determine geochemical evolution are as follows: (1) low concentrations of dissolved species during mining, (2) flooding is followed by sharp increase in TDS, (3) and smooth long term decrease in TDS, during the species are displaced in time and space. |
| Related projects: |