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Composite modification mechanism of cationic modifier to amphoteric modified kaolin and its effects on surface characteristics

机译:阳离子改性剂对两性改性高岭土的复合改性机理及其对表面特性的影响

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In this study, the changes of S (DC) curves (sum amount of dodecyl trimethyl ammonium cation and Ca2+/2 adsorbed on dodecyl dimethyl betaine-modified kaolin under different dodecyl trimethyl ammonium cation molar fractions) were analyzed to reveal the modification mechanism of cationic modifier (dodecyl trimethyl ammonium bromide) on amphoteric modified kaolin (kaolin modified by dodecyl dimethyl betaine). In addition, total organic carbon content and surface characteristics of different modified kaolins were analyzed using X-ray diffraction, specific surface area calculation, Fourier transform infrared spectroscopy, thermogravimetry, and scanning electron microscope. Results showed that: (1) "S (DC)" curves of compositely modified kaolin with dodecyl dimethyl betaine-modified ratios of 15, 30 and 60 % started to rise (appeared hydrophobic binding) at dodecyl trimethyl ammonium bromide-modified ratios of 16.80, 7.63, and 0.68 % (the critical point for different modification mechanisms), respectively. (2) Total organic carbon content of modified kaolins under different modification mechanisms showed hydrophobic modification mode > ion exchange and hydrophobic binding coexisting mode > ion exchange mode. Interlayer spacing showed no significant change under different modification modes. Specific surface area decreased slowly with enhanced hydrophobic modification mode. Fourier transform infrared spectroscopy and thermogravimetry results showed the modification effects of both dodecyl dimethyl betaine and dodecyl trimethyl ammonium bromide modification on kaolin surfaces. Scanning electron microscope results presented that the number of lamellar structures increased on clay surfaces with enhanced hydrophobic modification mode.
机译:在这项研究中,分析了S(DC)曲线的变化(十二烷基三甲基铵阳离子改性分数下十二烷基二甲基甜菜碱改性的高岭土上十二烷基三甲基铵阳离子和Ca2 + / 2的总量),以揭示阳离子的改性机理。两性改性高岭土(经十二烷基二甲基甜菜碱改性的高岭土)上的改性剂(十二烷基三甲基溴化铵)。另外,使用X射线衍射,比表面积计算,傅立叶变换红外光谱,热重分析和扫描电子显微镜分析了不同改性高岭土的总有机碳含量和表面特性。结果表明:(1)十二烷基二甲基甜菜碱改性比率为15、30和60%的复合改性高岭土的“ S(DC)”曲线在十二烷基三甲基溴化铵改性比率为16.80时开始上升(出现疏水结合)。 ,7.63和0.68%(不同修改机制的临界点)。 (2)在不同的改性机理下,改性高岭土的总有机碳含量为疏水改性模式>离子交换和疏水结合共存模式>离子交换模式。在不同的改性方式下,层间间距没有明显变化。比表面积随着疏水改性模式的增强而缓慢降低。傅里叶变换红外光谱和热重分析结果表明十二烷基二甲基甜菜碱和十二烷基三甲基溴化铵对高岭土的改性效果。扫描电子显微镜结果表明,随着疏水改性方式的增强,层状结构的数量在粘土表面增加。

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