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Wyszukujesz frazę "acid mine drainage" wg kryterium: Temat


Wyświetlanie 1-5 z 5
Tytuł:
Geomicrobiology of Acid Mine Drainage in the weathering zone of pyrite-bearing schists in the Rudawy Janowickie Mountains (Poland)
Autorzy:
Borkowski, A.
Parafiniuk, J.
Wolicka, D.
Kowalczyk, P.
Powiązania:
https://bibliotekanauki.pl/articles/2060320.pdf
Data publikacji:
2013
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Acid Mine Drainage
microbial communities
pyrite
weathering zone
Opis:
This paper presents the geomicrobiological analysis of acid water reservoirs and Acid Mine Drainage (AMD) developed in the weathering zone of pyrite-bearing schists near the closed-down pyrite mine in Wieściszowice (south-western Poland). The analysis was focused on two reservoirs characterized by different physical and chemical properties (pH, redox potential, content of sulphates and heavy metals). The study is the first thorough report on the geomicrobiological relationships taking place in the AMD setting in Wieściszowice and enables a description of the microbiological processes that significantly influence biogeochemical cycles of sulfur and iron in the analyzed water reservoirs. The reservoir water also harbors numerous big, organized microbial structures in the form of streamers. Samples of these structures were studied in detail using optical and electron microscopy, as well as microbiological cultivation and molecular methods. According to the obtained results, the slime streamers from the Wieściszowice mine are characterized by the co-occurrence of typical chemolithoautotrophic microorganisms oxidizing sulphur and iron together with sulphate reducing bacteria. The presence of these structures probably depends on the occurrence of iron (II) in the surrounding environment.
Źródło:
Geological Quarterly; 2013, 57, 4; 601--612
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Schwertmannite precipitated from acid mine drainage in theWestern Sudetes (SW Poland) and its arsenate sorption capacity
Autorzy:
Parafiniuk, J.
Siuda, R.
Powiązania:
https://bibliotekanauki.pl/articles/2059129.pdf
Data publikacji:
2006
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Western Sudetes
schwertmannite
ochre
acid mine drainage
arsenate sorption
Opis:
This paper contains XRD, Mössbauer and IR spectroscopy, chemical composition and thermal analysis results for the mineral schwertmannite present in the weathering zone developed in two abandoned sulphide mines in the Sudetes (SW Poland). In Wieściszowice a pyrite deposit was exploited, and in Radzimowice the deposit consisted of polymetallic mineralization with predominant arsenopyrite. In both localizations schwertmannite is developed as dripstones in underground workings and loose sediments precipitating from the acid mine drainage (AMD) waters. Schwertmannite forms tiny, needle-like crystals 2–3 m in size, usually grouped in botryoidal aggregations. The chemical composition of schwertmannite from Wieściszowice is typical for this mineral, and in Radzimowice the mineral contains up to 5.20 wt. % of As2O5. Due to highly developed specific surface and structural features, schwertmannite has the strongest sorption capabilities among the components of ochres, and takes up the largest amounts of arsenate oxyanion fromAMD, as well as considerable amounts of phosphates and heavymetals. About 71-87% of arsenate is sorbed on to the surface of the schwertmannite crystals and may readily be released into solution, 12–30% is bound into the structure of the mineral, and about 1% is an admixture of insoluble ferric arsenates.
Źródło:
Geological Quarterly; 2006, 50, 4; 475-486
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Origin of sulfates in the post-mining lakes in the eastern part of Muskau Arch (Polish-German borderland)
Autorzy:
Labus, K. M.
Skoczyńska-Gajda, S.
Powiązania:
https://bibliotekanauki.pl/articles/2060557.pdf
Data publikacji:
2013
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
acid mine drainage
post-mining lakes
stable isotope analyis
Muskau Arch
Opis:
Exploitation of lignites, carried out within glaciotectonic structures of Muskau Arch, led to formation of numerous post-minng lakes impacted by Acid Mine Drainage (AMD). . The isotopic analyses decribed in this paper allowed for identification of sources of the dissolved sulphates in the waters of two representative lakes. One of the sources of sulfur isotopes could be oxidation of sulphides (supplied in debris sliding from the slopes of waste dumps, which are surrounding the lakes) in the water column. The fraction of oxygen from water in forming the sulphates vary from about 5% to 25% in the first lake, while in the second it falls within the range 25%-85%. The research confirmed that the main source of sulfates in the lakes is the oxidation of pyrite.
Źródło:
Geological Quarterly; 2013, 57, 3; 561--566
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Pierwiastki ziem rzadkich w kwaśnych wodach kopalnianych : zarys problematyki
Rare earth elements in acid mine drainage waters : an outline of the issues
Autorzy:
Migaszewski, Zdzisław M.
Gałuszka, A.
Powiązania:
https://bibliotekanauki.pl/articles/2075910.pdf
Data publikacji:
2019
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
kwaśne wody kopalniane
pierwiastki ziem rzadkich
cechy
anomalie
występowanie
interakcje geochemiczne
acid mine drainage
rare earth elements
characteristics
anomalies
occurrence
geochemical interactions
Opis:
This paper presents the brief characteristics of rare earth elements (REE) and their occurrence in acid mine drainage (AMD) waters. The special emphasis is laid on REE classification, computation of shale-normalized coefficients and interpretation of REE anomalies. This paper also outlines the REE behavior in the environment, geochemical interactions and their potential application for assessing an impact of AMD on the environment.
Źródło:
Przegląd Geologiczny; 2019, 67, 2; 105--114
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Zmienność składu chemicznego kwaśnych wód spływu powierzchniowego z czynnej hałdy odpadów górniczych reprezentujących osady krakowskiej serii piaskowcowej Górnośląskiego Zagłębia Węglowego
Variability of chemical composition of acidic runoff waters from anactive spoil heap of mining wastes representing sediments of the Cracow Sandstone Series of the Upper Silesian Coal Basin
Autorzy:
Bauerek, A.
Bebek, M.
Frączek, R.
Paw, K.
Kasperkiewicz, W.
Powiązania:
https://bibliotekanauki.pl/articles/2075663.pdf
Data publikacji:
2017
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
kwaśne wody kopalniane
AMD
odpady górnicze
Górnośląskie Zagłębie Węglowe
metale ciężkie
siarczany
acid mine drainage
coal mining waste
Upper Silesian Coal Basin
heavy metals
sulphates
Opis:
Analysis of physical and chemical properties of water runoff samples collected in the vicinity of a spoil heap near the coal mine in Libiąż showed that they represented a classic example of acid mine drainage. For the first time in the Upper Silesian Coal Basin, it has been documented that rainwater in contact with a surface layer of waste containing pyrite (FeS2) and scarce carbonate phases, produces strongly acidified wastewater. This process is accompanied by a dramatic increase in the concentration of dissolved ions (eg. Cl-, SO , Fe, Al, Mn). Further geochemical changes occur in the ditch collecting water runoff at the base of the heap. At this stage, oxidation of pyrite catalyzed by bacteria, followed by hydrolysis of iron Fe3+ to form goethite (FeO(OH)) leads to conversion of the less acidic (pH 2.6-3.5), short-time retention runoff water into the aggressive stagnant runoff water (pH 2.1-2.8). Further disintegration of Carboniferous claystones occurs in the acidic stagnant water environment, leading to the decomposition of mineral phases containing heavy metals dispersed in the rock matrix and to mobilization of Zn, Ni, Cu, Cd, Co, and Cr.
Źródło:
Przegląd Geologiczny; 2017, 65, 7; 450--458
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
    Wyświetlanie 1-5 z 5

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