The effect of iron and manganese mine waters on stream biota,
Part I: Seasonal and long term trends in mine water
geochemistry.

D 2002

The effect of iron and manganese mine waters on stream biota, Part I: Seasonal and long term trends in mine water geochemistry.

ZEMAN, Josef

Základní údaje

Originální název

The effect of iron and manganese mine waters on stream biota, Part I: Seasonal and long term trends in mine water geochemistry.

Autoři

ZEMAN, Josef (203 Česká republika, garant)

Vydání

Brno, Secotox 2002: Trends and advances in environmental chemistry and ecotoxicology, s. 107-107, 2002

Nakladatel

Recetox

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/00216224:14310/02:00007197

Organizační jednotka

Přírodovědecká fakulta

ISBN

80-210-2971-4

Klíčová slova anglicky

iron; manganese; mine water; geochemistry; trend

Štítky

geochemistry, Iron, manganese, Mine water, trend

Změněno: 13. 7. 2005 07:53, doc. RNDr. Josef Zeman, CSc.

Anotace

V originále

Olší mine (Dolní Rožínka, Czech Republic) was exploited in the years 1958-1989, uranium mineralization is mainly represented by uraninite and coffinite. Uranium mine Olší was closed in 1989. The regulated flooding of the mine continued till autumn 1995 when mine waters reached the surface. During flooding period, the concentration of total dissolved species varied around 650 mg/l, sulphate ions around 200 mg/l, Fe 1 mg/l, Mn 0.2 mg/l, uranium 0.2 mg/l, and 226Ra 50 mBq/l. These concentrations were almost the same as the concentrations characteristic for water in geochemical background. It was assumed that the concentration of TDS and all dissolved species in mine water would gradually decrease during the mine flooding and by the time water reached surface there would be no need to clean or the otherwise process the mine water. It was planned to leak mine water directly to surface into Hadůvka creek. Seasonal and long term trends in natural geochemical evolution of Olší mine water and Hadůvka creek water was presented.

Návaznosti

MSM 143100004, záměr

Název: Geologické procesy a jejich environmentální vyústění - styk variscid a alpid

Investor: Ministerstvo školství, mládeže a tělovýchovy ČR, Geologické procesy a jejich environmentální vyústění - styk variscid a alpid

Citovat

ZEMAN, Josef. The effect of iron and manganese mine waters on stream biota, Part I: Seasonal and long term trends in mine water geochemistry. In Secotox 2002: Trends and advances in environmental chemistry and ecotoxicology. Brno: Recetox, 2002, s. 107. ISBN 80-210-2971-4.

@inproceedings{483195,
   author = {Zeman, Josef},
   address = {Brno},
   booktitle = {Secotox 2002: Trends and advances in environmental chemistry and ecotoxicology},
   keywords = {iron; manganese; mine water; geochemistry; trend},
   language = {eng},
   location = {Brno},
   isbn = {80-210-2971-4},
   pages = {107-107},
   publisher = {Recetox},
   title = {The effect of iron and manganese mine waters on stream biota, Part I: Seasonal and long term trends in mine water geochemistry.},
   year = {2002}
}

TY  - JOUR
ID  - 483195
AU  - Zeman, Josef
PY  - 2002
TI  - The effect of iron and manganese mine waters on stream biota, Part I: Seasonal and long term trends in mine water geochemistry.
PB  - Recetox
CY  - Brno
SN  - 8021029714
KW  - iron
KW  - manganese
KW  - mine water
KW  - geochemistry
KW  - trend
N2  - Olší mine (Dolní Rožínka, Czech Republic) was exploited in the years 1958-1989, uranium mineralization is mainly represented by uraninite and coffinite. Uranium mine Olší was closed in 1989. The regulated flooding of the mine continued till autumn 1995 when mine waters reached the surface. During flooding period, the concentration of total dissolved species varied around 650 mg/l, sulphate ions around 200 mg/l, Fe 1 mg/l, Mn 0.2 mg/l, uranium 0.2 mg/l, and 226Ra 50 mBq/l. These concentrations were almost the same as the concentrations characteristic for water in geochemical background. It was assumed that the concentration of TDS and all dissolved species in mine water would gradually decrease during the mine flooding and by the time water reached surface there would be no need to clean or the otherwise process the mine water. It was planned to leak mine water directly to surface into Hadůvka creek. Seasonal and long term trends in natural geochemical evolution of Olší mine water and Hadůvka creek water was presented.
ER  -

ZEMAN, Josef. The effect of iron and manganese mine waters on stream biota, Part I: Seasonal and long term trends in mine water geochemistry. In \textit{Secotox 2002: Trends and advances in environmental chemistry and ecotoxicology}. Brno: Recetox, 2002, s.~107. ISBN~80-210-2971-4.

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