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A preliminary study on the enrichment mechanism and occurrence of hazardous trace elements in the Tertiary lignite from the Shenbei coalfield, China

机译:神北煤田三次褐煤富集机理及有害微量元素赋存的初步研究

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The Cr and Ni contents are high in the Eocene lignite of the Shenbei coalfield, which is a small intracontinental basin located in Liaoning Province, China. In this paper, we studied the distribution, origin and occurrence of Cr, Ni and other hazardous trace elements in the Shenbei lignite on the basis of coal petrology, and geochemistry of the lignite and combustion products. The following conclusions on the Shenbei lignite can be drawn: (1) The dominant maceral group in the Shenbei coal is huminite (humodetrinite), accounting for 96%-99% of the total maceral. Inertinite content is less than 1%. Liptinite content (sporinite and cutinite) is 0.2-1.6%. Common minerals in the Shenbei lignite include clay minerals (kaolinite), pyrite and quartz, and calcite and siderite. Chromite is not present in the lignite. (2) Potentially hazardous trace elements such as Co (22 μg/g), Cr (79 μg/g), Cu (63 μg/g), Zn (93 μg/g), V (88 μg/g) and Ni (75 μg/g) are strongly enriched in the Shenbei lignite compared with average concentration of trace elements in the Chinese coal and worldwide lignite. These elements are mainly associated with fulvic acid (FA) and/or coal organic macromolecular compounds in most of the studied lignite samples, indicating an organic association and enrichment of these elements in the Shenbei lignite. (3) Unusually high trace elements contents in the Shenbei lignite are derived mainly from the olivine basalt (country rock of coal basin) that consists of 52.7% plagioclase, 17.8% pyroxene, 14% olivine and 15.5% Ti-Fe oxide minerals. These olivine basalts have higher Cr, Ni, Pb and Zn contents than other types of rock and worldwide basalts do. (4) Fly ash of the Shenbei lignite, with 90% 1-50 μm amorphous particles and 8% 1-10 μm cenosphere, has high contents of Zn (23,707 μg/g), Be (12 μg/g), Sr (1574 μg/g), Pb (486 μg/g) and Cr (349 μg/ g). In particular, the ferruginous micro-cenoshperes contain 1-12.79% Zn. Fine bottom ash (<0.031mm) of the Shenbei lignite has higher contents for most of the elements with the exception of Mo, Sn and Zn. Therefore, the potentially environmental and health impact of the fly ash and fine bottom ash should constitute a major concern.
机译:深北煤田始新世褐煤中的Cr和Ni含量较高,这是位于中国辽宁省的一个小型洲际盆地。本文根据煤的岩石学,褐煤和燃烧产物的地球化学,研究了深北褐煤中Cr,Ni等有害微量元素的分布,成因和赋存状态。关于深北褐煤,可以得出以下结论:(1)深北煤中占主导地位的黄铁矿基团是腐殖质(humodetrinite),占总黄石的96%-99%。惰质含量小于1%。锂皂石的含量(亚硫酸钙钙石和角质钙石)为0.2-1.6%。神北褐煤中常见的矿物包括粘土矿物(高岭石),黄铁矿和石英以及方解石和菱铁矿。褐煤中不存在铬铁矿。 (2)潜在有害的微量元素,例如Co(22μg/ g),Cr(79μg/ g),Cu(63μg/ g),Zn(93μg/ g),V(88μg/ g)和Ni与中国煤炭和全球褐煤中痕量元素的平均浓度相比,深北褐煤中(75μg/ g)的含量很高。在大多数研究的褐煤样品中,这些元素主要与黄腐酸(FA)和/或煤有机大分子化合物有关,表明这些元素在神北褐煤中具有有机缔合和富集作用。 (3)陕北褐煤中微量元素含量异常高,主要来源于斜长石52.7%,辉石17.8%辉石,橄榄石14%和Ti-Fe氧化物矿物15.5%组成的橄榄石玄武岩。这些橄榄石玄武岩比其他类型的岩石和全世界的玄武岩具有更高的Cr,Ni,Pb和Zn含量。 (4)沉北褐煤的粉煤灰中90%的1-50μm无定形颗粒和8%1-10μm的中空层,具有较高的Zn(23,707μg/ g),Be(12μg/ g),Sr( 1574微克/克),铅(486微克/克)和铬(349微克/克)。尤其是,铁质微松柏含有1-12.79%的Zn。陕北褐煤的细末灰(<0.031mm)除钼,锡和锌外,大多数元素含量较高。因此,粉煤灰和细粉底灰对环境和健康的潜在影响应成为主要关注的问题。

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