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十六烷基三甲基溴化铵直接处理钙基蒙脱土

崔继文12, 孙瑞岩3, 李士伟1, 王力峰1, 那辉1   

  1. 1. 吉林大学 化学学院, 长春 130021; 2. 佳木斯大学 化学与药学院, 黑龙江省 佳木斯 154000; 3. 长春中医药大学 药学院, 长春 130021
  • 收稿日期:2006-07-18 修回日期:1900-01-01 出版日期:2007-03-26 发布日期:2007-03-26
  • 通讯作者: 崔继文

CaMontmorillonite Directly Modified by Hexadecyl Trimethyl Ammonium Bromide

CUI Jiwen12, SUN Ruiyan3, LI Shiwei1, WANG Lifeng1, NA Hui1   

  1. 1. College of Chemistry, Jilin University, Changchun 130021, China; 2. College of Chemistry and Pharmacy, Jiamusi University, Jiamusi 154000, Heilongjiang Province, China; 3. College of Pharmacy, Changchun University of Chinese Medicine, Changchun 130021, China
  • Received:2006-07-18 Revised:1900-01-01 Online:2007-03-26 Published:2007-03-26
  • Contact: CUI Jiwen

摘要: 采用离子交换法直接用十六烷基三甲基溴化铵处理钙基蒙脱土, 成功制备出理想的有机蒙脱土, 经红外光谱分析(FTIR)、 差热分析(DTA)和X射线晶体衍射(XRD)分析等测试手段表征. 研究了蒙脱土处理方式、 离子交换时间和次数对有机蒙脱土结构的影响. 结果表明, 有机蒙脱土的层间距由1.49 nm扩大到2.21 nm.

关键词: 钙基蒙脱土, 离子交换法, 层间距

Abstract: A new type of organomontmorillonite (C16-MMT) is reported. Camontmo rillonite (Ca-MMT) was directly modified with hexadecyl trimethyl ammonium bromide viaionexchange. The effects of dispose measure of montmorillonite and ionexchange conditions including ionexchange time and ionexchange times on the structure of C16-MMT were investigated by X-ray diffraction (XRD). The X-ray patterns reveal that the interlamellar spacing of the clay, corresponding to the (001) plane peak, increases from 1.49 nmof the purifiedCa-MMT to 2.21 nm of C16-MMT.

Key words: Ca-montmorillonite, ion-exchanged method, interlamellar spacing

中图分类号: 

  • O614.231