Modification of kaolinite clay using benzyltriethylammonium chloride as a surfactant: Preparation and characterization

Hana Meftah Elgubbi, S. Othman, F. Harun
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引用次数: 1

Abstract

Natural kaolinite clay from Perak, Malaysia with cation exchange capacity (CEC) of 2.5 meq/100g was modified using cationic surfactant, benzyltriethylammonium chloride (BTEA-Cl), at 0.5, 1.0, 1.5 and 2.0 times the CEC. A number of techniques, namely energy dispersive X-ray (EDX) spectroscopy, X-ray diffraction (XRD), Fourier-transform infrared (FTIR) spectroscopy, scanning electron microscopy (SEM), and Brunauer-Emmett-Teller (BET) nitrogen adsorption-desorption were then used for characterization of the kaolinite and/or organo-modified kaolinite clays. The presence of alkyl groups as a result of successful intercalation of cationic surfactant within the organokaolinite layers of the clay was exhibited by the FTIR spectra. The SEM microphotographs exhibited good dispersion of the natural clay particles and slight agglomeration in the organo-modified clay particles. XRD patterns showed that the d001 spacing of the natural kaolinite clay increased from 7.12 Å to between 7.20 7.34 Å for the organo-modified clays. Following the BET nitrogen adsorption-desorption technique, all clay samples were of Type IV with narrow hysteresis loops. Surface areas of the clays showed drastic decrease from (25.34 m/g) for natural kaolinite clay to between 5.90 13.11 m/g for organo-modified clays. The results suggested that modification of natural kaolinite clay using cation surfactant had successfully occurred. The modification can therefore be further applied for alteration and improvement of the properties of natural clays for various industrial applications.
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以苄基三乙基氯化铵为表面活性剂改性高岭石粘土:制备及表征
采用阳离子表面活性剂苄基三乙基氯化铵(BTEA-Cl)对马来西亚霹雳州天然高岭石粘土进行了阳离子交换容量(CEC)为2.5 meq/100g的改性,其阳离子交换容量分别为CEC的0.5、1.0、1.5和2.0倍。然后利用能量色散x射线(EDX)光谱、x射线衍射(XRD)、傅里叶变换红外(FTIR)光谱、扫描电镜(SEM)和Brunauer-Emmett-Teller (BET)氮吸附-解吸等技术对高岭石和/或有机改性高岭石粘土进行了表征。傅里叶红外光谱表明,阳离子表面活性剂在粘土的有机高岭石层中成功嵌入烷基。SEM显微照片显示天然粘土颗粒分散性好,有机改性粘土颗粒中有轻微的团聚。XRD谱图表明,有机改性粘土的d001间距从7.12 Å增加到7.20 ~ 7.34 Å。采用BET法对氮进行吸附解吸后,黏土样品均为ⅳ型,滞回线窄。黏土的比表面积由天然高岭石黏土的25.34 m/g急剧下降到有机改性黏土的5.90 ~ 13.11 m/g。结果表明,阳离子表面活性剂对天然高岭石粘土的改性是成功的。因此,该改性可以进一步应用于各种工业用途的天然粘土的性质的改变和改善。
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