Extreme enrichment of arsenic and rare earth elements in acid mine drainage: Case study of Wisniowka mining area (south-central Poland)

被引:67
|
作者
Migaszewski, Zdzislaw M. [1 ]
Galuszka, Agnieszka [1 ]
Dolegowska, Sabina [1 ]
机构
[1] Jan Kochanowski Univ, Inst Chem, Geochem & Environm Div, 15G Swietokrzyska St, PL-25406 Kielce, Poland
关键词
Acid mine drainage; Tailings pile; Strongly acidic pools; Arsenic; REE; HOLY CROSS MOUNTAINS; ISOTOPE GEOCHEMISTRY; PYRITE OXIDATION; SOIL POLLUTION; TRACE-ELEMENTS; IRON MOUNTAIN; STREAM WATERS; NEGATIVE PH; MINERALOGY; SULFUR;
D O I
10.1016/j.envpol.2018.10.106
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The Wisniowka rock strip mining area (south-central Poland) with quartzite quarries, acid water bodies and tailings piles is one of the most unique acid mine drainage (AMD) sites throughout the world. This is due to the occurrence of enormous amounts of pyrite unknown in sedimentary formations worldwide. Of the two mineralization zones, one that is the most abundant in arsenical pyrite occurs in the lowermost Upper Cambrian formation of the Podwisniowka quarry. The As-rich pyritiferous clastic rocks are exposed as a result of deep quartzite extraction during 2013-2014. In addition, the clayey-silty shale interbeds are enriched in rare earth element (REE) minerals. The mining operation left an acidic lake with a pH of about 2.4-2.6 and increased contents of sulfates, metal(loid)s and REE. The Podwisniowka pyrite rich waste material was stacked up in many places of the mining area giving rise to strongly acidic spills that jeopardized the neighboring environment. One of these unexplored tailings piles was a source of extremely sulfate- and metal(loid)-rich pools with unusual enrichments in As (up to 1548 mg L-1) and REE (up to 24.84 mg L-1). These distinctly exceeded those previously reported in the Wisniowka area. A broad scope of geochemical, mineralogical and petrographic methods was used to document these specific textural and mineralogical properties of pyrite facilitating its rapid oxidation. The pyrite oxidation products reacted with REE-bearing minerals releasing these elements into acid water bodies. Statistical methods were employed to connect the obtained tailings pool hydrogeochemical data with those derived from this and the previous studies of the Podwisniowka and Wisniowka Duza acid pit lakes. In contrast to metal(loid) profiles, the characteristic shale-normalized REE concentration patterns turned out to be more suitable for solving different AMD issues including provenance of mine waste material in the tailings pile examined. (C) 2018 Elsevier Ltd. All rights reserved.
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页码:898 / 906
页数:9
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