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作 者:代世峰[1] 唐跃刚[1] 常春祥 张义忠 李薇薇[1]
机构地区:[1]中国矿业大学煤炭资源教育部重点实验室 [2]开滦矿务局煤炭质量检测中心,河北开滦063018
出 处:《燃料化学学报》2005年第4期416-420,共5页Journal of Fuel Chemistry and Technology
基 金:国家自然科学基金(40472083);国家重点基础研究发展规划(973计划;2003CB214607);国家教育部科技研究重点项目(105020)~~
摘 要:以河北开滦矿区晚古生代煤及其洗选产品为研究对象,运用电感耦合等离子体质谱(ICPMS)和逐级化学提取的方法,对稀土元素的质量分数及其在洗选过程中的迁移和分配特征进行了研究。结果表明,开滦矿区煤中稀土元素没有明显富集;稀土元素在入洗原煤及其洗选产品中,以煤泥中质量分数最高,尾煤次之,在尾煤和煤泥中均相对富集;稀土元素在精煤中的质量分数最低;同原煤相比,中煤的稀土元素质量分数没有明显变化。原煤及其洗选的4种产品中的稀土元素分配模式基本相同,主要差别是质量分数的不同。稀土元素在洗选过程中的分配行为和赋存状态主要受控于黏土矿物,其次是有机质。On the basis of coal geochemistry and coal petrology, the content, migration, and distribution of rare earth elements (REEs) in the Paleozoic coals and their washing products were determined using inductively coupled-plasma mass spectrometry (ICP-MS), sequential chemical extraction procedure, and optical microscope.The contents of REEs in 47 coal channel samples from 10 mines of Kailuan Coalfield were determined. The results show that the REEs are not significantly enriched in the coals from the Kailuan Coalfield, North China. The content of REEs increases in the order of cleaned coal (76.63 w/10^-6 ), raw coal (85.84 w/10^-6 ), middling coal (88.6 w/10^-6 ), tailing coal ( 125.93 w/10^-6 ) , and coal slime ( 177.08 w/10^-6 ). The values of δEu and δCe are similar among raw coal and its washing products. The obvious difference of REEs in raw coal and its products is their different concentrations. Six states of REEs, water soluble, exchangeable, organic, carbonate,silicate, and sulfide states, are classified to study modes of occurrence. Modes of coccurrence of REEs in raw coal and middling coal are similar. REEs in the cleaned coal are mainly associated with organic matrix and silicates. Most of REEs in the tailing coal and coal slime are associated with alumino-silicate mineral matters. However, Tm, Yb and Lu associated with organic matter are surprised high in all coal washing products compared with the other REEs. Tm, Yb, and Lu associated with organic matter in the coal slime are 2.4% , 3.5% and 2.8%, respectively. Combined with the results of sequential chemical extraction and mineral composition analyses,it can be concluded that the dominant influence factors on the concentration and modes of occurrence of REEs are in order of clay minerals, organic matter, pyrite, quartz and calcite.
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