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蛭石精矿的有机改性试验
引用本文:李雪梅,廖立兵,谷勤,李瑞,王春燕.蛭石精矿的有机改性试验[J].岩矿测试,2008,27(1):63-66.
作者姓名:李雪梅  廖立兵  谷勤  李瑞  王春燕
作者单位:中国地质大学材料科学与工程学院,北京,100083
摘    要:采用十六烷基三甲基溴化铵(HDTMAB)对蛭石精矿进行了有机改性,利用X射线衍射法(XRD)、红外光谱(IR)、差示扫描量热法(DSC)和热失重分析(TG)对蛭石精矿和有机改性蛭石进行了表征。实验结果表明,当反应液中蛭石与水的质量比为1∶10、反应温度在60~70℃时,HDTMAB的阳离子HDTMA进入绝大部分蛭石晶粒的晶层,将蛭石的晶层间距撑大,蛭石的(001)晶面间距d001从1.45986 nm增大到3.70134 nm。HDTMA进入了单晶颗粒之间,将蛭石颗粒分散成单晶颗粒。

关 键 词:蛭石精矿  十六烷基三甲基溴化铵  有机改性
文章编号:0254-5357(2008)01-0063-04
收稿时间:2007-07-08
修稿时间:2007-09-29

Experiments on the Organic Modification of Vermiculite Concentrate
LI Xue-mei,LIAO Li-bing,GU Qin,LI Ri,WANG Chun-yan.Experiments on the Organic Modification of Vermiculite Concentrate[J].Rock and Mineral Analysis,2008,27(1):63-66.
Authors:LI Xue-mei  LIAO Li-bing  GU Qin  LI Ri  WANG Chun-yan
Institution:(School of Material Science and Technology,China University of Geosciences,Beijing 100083,China)
Abstract:The vermiculite concentrate is organic modified with hexadecyl trimethyl ammonium bromide(HDTMAB) and vermiculite and organo-vermiculite are characterized by X-ray diffraction spectrometry(XRD),infrared spectrometry(IR),differential scanning calorimetry(DSC) and gravitational thermal analysis(TG).The experimental results show that when the mass ratio of vermiculite to water is 1∶10 in reaction suspension and the reaction temperature is controlled at 60~70℃,HDTMA cations enter the interlayer gap of most vermiculite particle and enlarge the distance between the crystal layers of vermiculite(the distance of the(001) crystal plane of vermiculite increasing from 1.45986 nm to 3.70134 nm).HDTMA cations enter the gap between single crystal particles of vermiculite and separate the vermiculite particles into single crystal particles with nanometer size.
Keywords:vermiculite concentrate  hexadecyl trimethyl ammonium bromide (HDTMAB)  organic modification
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