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铁层离-柱撑蒙脱石的结构初探

CHARACTERIZATION OF IRON DELAMINATED PILLARED MONTMORILLONITE: A PRIMARY STUDY

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【作者】 袁鹏王辅亚肖万生吴大清杨丹何宏平

【Author】 YUAN Peng, WANG Fu-ya, XIAO Wan-sheng, WU Da-qing, YANG Dan, HE Hong-ping(Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China)

【机构】 中国科学院广州地球化学研究所

【摘要】 利用低角度X射线衍射分析、红外光谱、比表面积及孔结构分析,研究铁柱撑蒙脱石的结构特性,结果显示:经柱撑处理后的蒙脱石以层离结构为主,同时含有部分柱撑蒙脱石结构。前者为粘土片层与铁离子水解产生的聚合羟基铁的簇状物堆垛而成的卡房状孔结构,与XRD图上低角度衍射峰对应;后者则与(001)衍射峰时应。与柱撑结构不同,层离结构中,大量阴离子(NO3-)能够作为平衡铁水解聚合物正电荷的反离子而较稳定地存在,研究还发现铁层离-柱撑蒙脱石具有作为新型催化剂、吸附剂应用的前景。

【Abstract】 Iron oxide pillared clay was synthesized by the reaction of montmorillonite with base-hydrolyzed solutions of nitrate salt of Fe(Ⅲ) salts. In contrast with the classical PILCs structure with intercalation of metal irons hydrolysis product, based on the analyses of powder X-ray diffraction (XRD),nitrogen adsorption-desorption isotherms and Fourier transform infrared spectroscopy (FTIR),a resultant iron-clay with novel meso-microporous delaminated structure containing pillared fragments was recognized. One high d spacing beyond 6.4 nm and another d spacing of ca. 1.5 nm are observed in the XRD patterns of resultant iron-clays. The former is assigned to the distribution of pores in the delaminated structure rather than the (001) reflection of periodic structure of intercalation and the latter d spacing of ca. 1.5 nm corresponds to the intercalation of primary hydrolysis product of Fe (Ⅲ). Considerable NO3 is found to be retained in the mesoporous delaminated structure to neutralize the positive charge of iron aggregate. The resultant delaminated pillared clay is of prospects in the field of novel heterogeneous catalysts and adsorbents.

【基金】 中科院广州地球化学所知识创新工程领域前沿项目(批准号:GIGCX-04-02);广东省自然科学基金(批准号:04002140)
  • 【会议录名称】 2005年全国矿物科学与工程学术会议论文集
  • 【会议名称】2005年全国矿物科学与工程学术会议
  • 【会议时间】2005-09
  • 【会议地点】中国绵阳
  • 【分类号】O611.1
  • 【主办单位】中国矿物岩石地球化学学会工艺矿物学专业委员会、中国矿物岩石地球化学学会矿物物理矿物结构专业委员会、中国硅酸盐学会工艺岩石学分会
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