首页> 外文期刊>Fuel >The migration of heavy metal elements during pyrolysis of oil shale in Mongolia
【24h】

The migration of heavy metal elements during pyrolysis of oil shale in Mongolia

机译:蒙古油页岩热解过程中重金属元素的迁移

获取原文
获取原文并翻译 | 示例
获取外文期刊封面目录资料

摘要

The migration of trace elements during the pyrolysis of Mongolian oil shale is studied at the macroscopic (the porosity change) and microscopic (the occurrence state) levels. Four groups of oil shale (904, 1054, 10513 and 10807) in the Dalai Bulang mining area of Mongolia were studied. Oil shale samples were heated in a tube furnace in argon atmosphere. Final temperatures of pyrolysis varied from 300 degrees C to 900 degrees C resulting in different char. The content of eight kinds of heavy metal elements in the oil shale and the pyrolysis semi-coke were determined by inductively coupled plasma mass spectometry (ICP-MS), through which the distribution and the migration of these elements were analyzed. The specific surface area and pore distribution of different semi-coke were detected by specific surface area analyzer. The influence of surface area and pore distribution on heavy metal element migration was investigated. The sequential chemical extraction (SEC) was carried out on the original oil shale samples. Trace elements in different occurrence models were also detected by ICP-MS. Then the relationship between occurrence models and trace element migration during pyrolysis was also analyzed. The results show that 1) The concentrations of heavy metal elements in four kinds of oil shale groups are similar, and the occurrence models of the same kind of heavy metal elements in four samples are also similar. 2) The migration amount of Zn and Cu is small at the temperature below 500 degrees C, while both of the elements escaped rapidly at the temperature above 700 degrees C. Because Zn and Cu are mainly present in the carbonate which decomposed rapidly at the temperature above 600 degrees C. 3) The mobility of most of the elements in the sample shows a downward trend during 500-600 degrees C and 800-900 degrees C. During these temperature ranges the specific surface area of the semi-coke was increased, because the elements was reabsorbed by the semi-coke.
机译:在宏观(孔隙度变化)和微观(发生状态)水平研究了蒙古油页岩热解过程中微量元素的迁移。研究了蒙古达赖布朗矿区的四组油页岩(904、1054、10513和10807)。油页岩样品在氩气氛下的管式炉中加热。热解的最终温度从300摄氏度到900摄氏度不等,从而形成不同的炭。采用电感耦合等离子体质谱法(ICP-MS)测定了油页岩和热解半焦中8种重金属元素的含量,并分析了这些元素的分布和迁移。用比表面积分析仪检测不同半焦的比表面积和孔分布。研究了表面积和孔分布对重金属元素迁移的影响。对原始油页岩样品进行了顺序化学提取(SEC)。 ICP-MS还检测了不同发生模型中的痕量元素。然后分析了热解过程中发生模型与微量元素迁移之间的关系。结果表明:1)4种油页岩组中重金属元素的含量相似,4种样品中同一种重金属元素的赋存模型也相似。 2)在低于500摄氏度的温度下Zn和Cu的迁移量很小,而在高于700摄氏度的温度下两种元素都迅速逸出。因为Zn和Cu主要存在于碳酸盐中,在该温度下会迅速分解高于600摄氏度。3)样品中大多数元素的迁移率在500-600摄氏度和800-900摄氏度之间呈下降趋势。在这些温度范围内,半焦的比表面积增加,因为元素被半焦重新吸收。

著录项

  • 来源
    《Fuel》 |2018年第1期|381-387|共7页
  • 作者单位

    Northeast Elect Power Univ, Sch Energy Resources & Mech Engn, Jilin, Jilin, Peoples R China;

    Northeast Elect Power Univ, Sch Energy Resources & Mech Engn, Jilin, Jilin, Peoples R China;

    Northeast Elect Power Univ, Sch Energy Resources & Mech Engn, Jilin, Jilin, Peoples R China;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Trace element; Migration; Pyrolysis; Oil shale;

    机译:微量元素;迁移;热解;油页岩;

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号