Changes in the morphology of organoclays with HDTMA+ surfactant loading

被引:283
作者
He, HP
Frost, RL
Bostrom, T
Yuan, P
Duong, L
Yang, D
Yunfel, XF
Kloprogge, JT
机构
[1] Univ Queensland, Sch Phys & Chem Sci, Inorgan Mat Res Program, Brisbane, Qld 4001, Australia
[2] Chinese Acad Sci, Guangzhou Inst Geochem, Guangzhou 510640, Peoples R China
基金
中国国家自然科学基金;
关键词
intercalation; surfactant; montmorillonite; organoclay; TEM; SEM morphology;
D O I
10.1016/j.clay.2005.10.011
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
The detailed understanding of the interlayer structure of organoclays is of importance in the design of organoclay based materials and their industrial applications. In this study, transmission electron microscopy (TEM), scanning electron microscopy (SEM) and X-ray diffraction (XRD) have been used to provide new insights into the interlayer structure and morphology of HDTMA(+)/montmorillonite organoclays. XRD patterns show that thermal treatment has an important effect on the stability of organoclays, reflected by significant changes in the basal spacing. TEM and SEM micrographs demonstrate that the organoclays with lower surfactant packing density are mainly composed of irregular layer stacking with a number of curved organoclay layers, while those with higher surfactant packing density are mainly composed of regularly intercalated and flat layers. Variations of the interlayer distances exist in all organoclays and are more pronounced in the organoclays with lower surfactant packing density. This study demonstrates that not only the arrangement model of surfactant but also the morphology of organoclay strongly depend on the surfactant packing density within the montmorillonite interlayer space. (c) 2005 Elsevier B.V. All rights reserved.
引用
收藏
页码:262 / 271
页数:10
相关论文
共 36 条
[1]   Transmission electron microscopy study of smectite illitization during hydrothermal alteration of a rhyolitic hyaloclastite from Ponza, Italy [J].
Bauluz, B ;
Peacor, DR ;
Ylagan, RF .
CLAYS AND CLAY MINERALS, 2002, 50 (02) :157-173
[2]   THE BRITTLE MICA-LIKE KNIASO4 AND ITS ORGANIC DERIVATIVES [J].
BENEKE, K ;
LAGALY, G .
CLAY MINERALS, 1982, 17 (02) :175-183
[3]  
BRINDLEY GW, 1965, AM MINERAL, V50, P1355
[4]   New organo-montmorillonite complexes with hydrophobic and hydrophilic functions [J].
Choy, JH ;
Kwak, SY ;
Han, YS ;
Kim, BW .
MATERIALS LETTERS, 1997, 33 (3-4) :143-147
[5]   ORGANO-BENTONITES WITH QUATERNARY ALKYLAMMONIUM IONS [J].
FAVRE, H ;
LAGALY, G .
CLAY MINERALS, 1991, 26 (01) :19-32
[6]  
Gu AJ, 2001, J APPL POLYM SCI, V79, P1902, DOI 10.1002/1097-4628(20010307)79:10<1902::AID-APP190>3.3.CO
[7]  
2-J
[8]   SEGMENTAL DYNAMICS AND RELAXATION OF N-OCTANE AT SOLID-LIQUID INTERFACES [J].
GUPTA, S ;
KOOPMAN, DC ;
WESTERMANNCLARK, GB ;
BITSANIS, IA .
JOURNAL OF CHEMICAL PHYSICS, 1994, 100 (11) :8444-8453
[9]   Conformation of poly(ethylene oxide) intercalated in clay and MoS2 studied by two-dimensional double-quantum NMR [J].
Harris, DJ ;
Bonagamba, TJ ;
Schmidt-Rohr, K .
MACROMOLECULES, 1999, 32 (20) :6718-6724
[10]   Infrared study of HDTMA+ intercalated montmorillonite [J].
He, HP ;
Ray, FL ;
Zhu, JX .
SPECTROCHIMICA ACTA PART A-MOLECULAR AND BIOMOLECULAR SPECTROSCOPY, 2004, 60 (12) :2853-2859