Mercury distribution in coals influenced by magmatic intrusions, and surface waters from the Huaibei Coal Mining District, Anhui, China

•Hg concentrations in coal and surface water samples were determined.•Hg is enriched in the Huaibei coals.•Magmatic activities imparted influences on Hg content and distribution.•Hg contents in surface waters are relative low at the present status. The Hg concentrations in 108 samples, comprising 81...

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Published inApplied geochemistry Vol. 33; pp. 298 - 305
Main Authors Yan, Zhicao, Liu, Guijian, Sun, Ruoyu, Wu, Dun, Wu, Bin, Zhou, Chuncai
Format Journal Article
LanguageEnglish
Published Kidlington Elsevier Ltd 01.06.2013
Elsevier
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Summary:•Hg concentrations in coal and surface water samples were determined.•Hg is enriched in the Huaibei coals.•Magmatic activities imparted influences on Hg content and distribution.•Hg contents in surface waters are relative low at the present status. The Hg concentrations in 108 samples, comprising 81 coal samples, 1 igneous rock, 2 parting rock samples and 24 water samples from the Huaibei Coal Mining District, China, were determined by cold-vapor atomic fluorescence spectrometry. The abundance and distribution of Hg in different coal mines and coal seams were studied. The weighted average Hg concentration for all coal samples in the Huaibei Coalfield is 0.42mg/kg, which is about twice that of average Chinese coals. From southwestern to northeastern coalfield, Hg concentration shows a decreasing trend, which is presumably related to magmatic activity and fault structures. The relatively high Hg levels are observed in coal seams Nos. 6, 7 and 10 in the southwestern coal mines. Correlation analysis indicates that Hg in the southwestern and southernmost coals with high Hg concentrations is associated with pyrite. The Hg concentrations in surface waters in the Huaibei Coal Mining District range from 10 to 60ng/L, and display a decreasing trend with distance from a coal waste pile but are lower than the regulated levels for Hg in drinking water.
Bibliography:http://dx.doi.org/10.1016/j.apgeochem.2013.02.024
ObjectType-Article-1
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content type line 23
ISSN:0883-2927
1872-9134
DOI:10.1016/j.apgeochem.2013.02.024