ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
京西煤系高岭土中铁、钛赋存状态研究
  
关键词:kaolin  AEM  modes of occurrence of Fe and Ti
基金项目:北京市自然科学基金项目(编号:3042013)
作者单位E-mail
杨晓杰 中国矿业大学(北京)力建学院北京100083 yxjxumt@sohu.com 
刘冬明 中国矿业大学(北京)力建学院北京100083  
李桂刚 中国矿业大学(北京)力建学院北京100083  
陈开惠 中国科学院地质与地球物理研究所北京100029  
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摘要:
The Modes of Occurrence of Fe and Ti in Kaolin of West Beijing
      The modes of occurrence of Fe and Ti in kaolin of west Beijing were studied in detail by AEM and Mossbauer spectra. The results show that the mineral phases of Fe and Ti in the concentrates are mainly anatase with small amounts of goethite and Fe-Ti phase. Structural Fe is the main existing form of Fe and Ti in kaolinite. Four-fold coordination Fe 3 in Si-O tetrahedra and six-fold coordination Fe 3 and Fe 2 in Al-O octahedra are three existing types of structural Fe. This study is of significance both in the theoretical research on the kaolinite mineralogy and in the developmental practice of kaolinites in coal measures of west Beijing.
YANG Xiao-jie,LIU Dong-ming,LI Gui-gang,YE Kai-hui.2006.The Modes of Occurrence of Fe and Ti in Kaolin of West Beijing[J].Acta Geoscientica Sinica,27(2):141-144.
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