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Geochemistry of Sulfur and Hazardous Elements in Late Paleozoic Coals and Partings from Taozao Coalfield, Shandong Province, China
作者姓名:Huang Wenhui  Che Yao  Yang Qi  Tang Dazhen  Energy Resource
作者单位:Huang Wenhui Che Yao Yang Qi Tang Dazhen Energy Resource Department,China University of Geosciences,Beijing 100083,China Zhao Zhigen Tang Xiuyi Anhui University of Science and Technology,Huainan 232001,China
摘    要:Intermsoftheharmfulmattersincoalandcoalminingwastes,thefirstisabouthazardouselements ,theotherin cludessulfurandhazardousorganicmatter.Muchresearchontracetoxicelementsandtheirimpactsonenvironmenthasbeeninvestigatedinmanycountries (Goodarzi,1995 ;Finkelman ,1994 ;Chouetal.,1982 ) .Althoughthere searchconcerningthisaspectwasstartedmuchlaterinChi na ,manystudieshavebeenstrengthenedsince 1980 ,andmuchprogresshasbeenmade ,alargenumberofdatahavebeencollected ,andthecomparisonshavebeenmadeforthedata…

关 键 词:地球化学  硫磺  硫铁矿  电子探针  仪器中子活化分析  晚古生代  煤田  地质学

Geochemistry of Sulfur and Hazardous Elements in Late Paleozoic Coals and Partings from Taozao Coalfield, Shandong Province, China
Huang Wenhui,Che Yao,Yang Qi,Tang Dazhen,Energy Resource.Geochemistry of Sulfur and Hazardous Elements in Late Paleozoic Coals and Partings from Taozao Coalfield, Shandong Province, China[J].Journal of China University of Geosciences,2004,15(1):15-22.
Authors:HUANG Wenhui  Che Yao  Yang Qi  TANG Dazhen  Zhao Zhigen  Tang Xiuyi
Abstract:The analyses of different sulfur forms, the trace elements in pyrites using electron microprobe and the trace elements in coal using INAA (instrumental neutron activation analysis) of the Late Paleozoic coals from the Taozao coalfield in Shandong Province, China, conclude that most sulfur (>75 %) in high-sulfur coal of Taiyuan Formation occurred as pyrite, in which many hazardous elements co-existed and their concentrations varied with their geological origin. The concentrations of hazardous elements in high-sulfur coals from Taiyuan Formation, composing mainly of Cu, As, U, Pb, Mo and Co, are much higher than those in the low-sulfur coals from Shanxi Formation and Shihezi Formation, because the influence of seawater during and after coal accumulation in Taiyuan Formation is stronger than those in Shanxi and Shihezi formations. Moreover, the element As is related to Fe, and both elements exist mainly in the form of pyrite. The element U is richer in the coal influenced by seawater. In addition, the coal affected by the magmatism contains more U, too. When high-sulfur coals are processed with heavy media washing to remove sulfur and minerals, the majority of hazardous elements will also be removed from the coals.
Keywords:Late Paleozoic coals  partings  geochemistry  hazardous elements  Shandong Province
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