An Investigation of the Dehydroxylation of Kaolinite Using Energy-Filtering Transmission Electron Microscopy

에너지여과 투과전자현미경을 이용한 카올리나이트의 탈수반응 연구

  • 이수정 (연세대학교 지구시스템과학과) ;
  • 김윤중 (기초과학지원연구소 중앙분석기기부) ;
  • 문희수 (연세대학교 지구시스템과학과)
  • Published : 1999.06.01

Abstract

The dehydroxylation of kaolinite was investigated in detail by means of energy-filtering transmission electron microscope with both orientations parallel and perpendicular to c. The dehydroxylation could be characterized by the broad background including (0.211) band (20~24$^{\circ}$ 2$\theta$) on X-ray diffraction and by the three halo rings (d-spacing : 3.28~4.40$\AA$ (near (02,11) band), 2.41~245$\AA$ (near (20,13) band), 1.16~1.23$\AA$ (near (0.8,44) band)), and (02,11) and (20,13) spots on electron diffraction. These indicate existence of a short-range order along the a and b axes. Interplanar spacing of (001) is reduced to about 6.86$\AA$ and the sharp additional intensity maximum of about 14.2$\AA$ reveals that metakaolinite has a modulated structure along c axis. It is proposed that the modulated structure is attributed to the domains consisting of more than two-layers due to the changes of positions of the vacant octahedral sites in successive layers.

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