宋党育, 李春辉, 宋播艺, 杨存备. 新密煤田裴沟矿二1煤中环境敏感元素地球化学特征[J]. 煤田地质与勘探, 2016, 44(5): 28-36. DOI: 10.3969/j.issn.1001-1986.2016.05.005
引用本文: 宋党育, 李春辉, 宋播艺, 杨存备. 新密煤田裴沟矿二1煤中环境敏感元素地球化学特征[J]. 煤田地质与勘探, 2016, 44(5): 28-36. DOI: 10.3969/j.issn.1001-1986.2016.05.005
SONG Dangyu, LI Chunhui, SONG Boyi, YANG Cunbei. Geochemistry of environment sensitive elements in the No.2-1 coal from Peigou mine, Xinmi coalfield[J]. COAL GEOLOGY & EXPLORATION, 2016, 44(5): 28-36. DOI: 10.3969/j.issn.1001-1986.2016.05.005
Citation: SONG Dangyu, LI Chunhui, SONG Boyi, YANG Cunbei. Geochemistry of environment sensitive elements in the No.2-1 coal from Peigou mine, Xinmi coalfield[J]. COAL GEOLOGY & EXPLORATION, 2016, 44(5): 28-36. DOI: 10.3969/j.issn.1001-1986.2016.05.005

新密煤田裴沟矿二1煤中环境敏感元素地球化学特征

Geochemistry of environment sensitive elements in the No.2-1 coal from Peigou mine, Xinmi coalfield

  • 摘要: 运用电感耦合等离子体质谱仪(ICP-MS)、X射线荧光光谱方法(XRF)和X射线衍射方法(XRD),对裴沟矿二1煤层中钒、铬、砷、硒、铅五种元素的地球化学特征进行研究。通过系统测定元素的含量、煤中无机元素和矿物组成,研究其地球化学特征及其与构造煤形成过程之间的内在联系。研究表明:裴沟矿二1煤层中As、V和Cr的含量明显偏高,Se与Pb属正常水平;除砷元素外,目标元素与煤中无机组分关系密切,主要赋存于黏土矿物中,如钒、铬主要赋存于黏土矿物高岭石、伊利石中,与硫酸盐、硫化物矿物也有联系;硒主要赋存于黏土矿物高岭石中,与金红石也有一定相关性;铅主要赋存于黏土矿物高岭石中。探讨了构造煤形成过程对环境敏感元素含量的影响,环境敏感元素含量在不同煤分层中含量差异性显著,构造煤形成过程中环境敏感元素在垂向上并无大规模的迁移和明显的均一化行为。

     

    Abstract: Geochemistry of vanadium, chromium, arsenic, selenium and lead in seam2-1 in Peigou mine was investigated using X ray fluorescence spectrometer (ARL Quant'X), X ray diffraction (XRD) and inductively couple-plasma mass spectrometry(ICP-MS). Concentration, distribution and occurrence and their relationship with tectonic movement were studied based on environment-sensitive elements content determination, minerals and minor elements composition. The results show that the average concentration of arsenic, vanadium, and chromium is obviously higher than their average concentration in other Chinese coal and American coal, the concentration of selenium and lead is generally normal; their occurrence is mainly related to the inorganic minerals except arsenic. Most of vanadium and chromium are mainly concentrated in kaolinite and illite, part of them may be associated with sulfide or sulfate. Selenium is mainly concentrated in kaolinite, and may be associated with rutile. Lead is mainly concentrated in kaolinite. The paper also discussed the effect of tectonic deformation of coal on environment-sensitive element concentration and their distribution. The content of elements in different layers varied greatly, that means there is no obviously migration or homogenization in tectonic deformation of coal.

     

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