Study of individual Na-montmorillonite particles size, morphology, and apparent charge

被引:141
作者
Cadene, A
Durand-Vidal, S
Turq, P
Brendle, J
机构
[1] Univ Paris 06, Lab Liquides Ion & Interfaces Chargees L12C, F-75252 Paris, France
[2] Univ Haute Alsace, Lab Mat Mineraux, UMR CNRS 7016, F-68093 Mulhouse, France
关键词
montmorillonite; sheets; tactoids; aggregates; morphology; size distribution; apparent charge; AFM; PCS; conductivity;
D O I
10.1016/j.jcis.2004.12.016
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
Size. morphology. and apparent charge of individual Na-montmorillonite particles of natural MX-80 sodium montmorillonite were investigated in the present study by the use of three Coupling methods. In the first part of this work, natural and synthetic montmorillonite clays Were studied with atomic force microscopy (AFM) and photo-correlation spectroscopy (PCS). Both techniques exhibit the presence of two clay Populations with a high dispersion of the length distribution. Microscopic analysis of the system revealed that clay particles Could be reasonably approximated at low concentrations to ellipsoidal tactoids about 1.2 nm high. Average dimensions of the first population were typically 320-400 nm long/250 nm wide and 200-250 nm long/120 nm wide for natural and synthetic clays, respectively. The second population exhibits smaller sizes: 65 and 50 nm long and 35 and 25 nm wide for natural and synthetic clays, respectively. The statistics obtained for natural clay were then verified by PCS experiments on sodium montmorillonite suspensions. Both techniques reveal an important length dispersion. However, the relative proportions of the two kinds of particles could not be established properly because of both lack of statistics and limitations of the employed techniques. In the following part. conductivity measurements were performed Oil dilute montmorillonite clay Suspensions. Raw data were then interpreted with the sizes and morphological information gained in the first part of the present work. The apparent charge of the clay sheets Was found to be 8% of the Structural charge. (c) 2004 Elsevier Inc. All rights reserved.
引用
收藏
页码:719 / 730
页数:12
相关论文
共 39 条
[31]  
SAUZEAT E, 2001, MX80 REFERENCE METHO
[32]   INFLUENCE OF EXCHANGEABLE CATION COMPOSITION ON THE SIZE AND SHAPE OF MONTMORILLONITE PARTICLES IN DILUTE SUSPENSION [J].
SCHRAMM, LL ;
KWAK, JCT .
CLAYS AND CLAY MINERALS, 1982, 30 (01) :40-48
[33]   DIRECT PROCEDURE FOR DETERMINING NUMBER OF PLATES IN TACTOIDS OF SMECTITES - NA-CA-MONTMORILLONITE CASE [J].
SHOMER, I ;
MINGELGRIN, U .
CLAYS AND CLAY MINERALS, 1978, 26 (02) :135-138
[34]   Imaging structured water and bound polysaccharide on mica surface at ambient temperature [J].
Spagnoli, C ;
Loos, K ;
Ulman, A ;
Cowman, MK .
JOURNAL OF THE AMERICAN CHEMICAL SOCIETY, 2003, 125 (23) :7124-7128
[35]   Layer charge and electrophoretic mobility of smectites [J].
Thomas, F ;
Michot, LJ ;
Vantelon, D ;
Montargès, E ;
Prélot, B ;
Cruchaudet, M ;
Delon, JF .
COLLOIDS AND SURFACES A-PHYSICOCHEMICAL AND ENGINEERING ASPECTS, 1999, 159 (2-3) :351-358
[36]   Nanomorphology of montmorillonite particles:: Estimation of the clay edge sorption site density by low-pressure gas adsorption and AFM observations [J].
Tournassat, C ;
Neaman, A ;
Villiéras, F ;
Bosbach, D ;
Charlet, L .
AMERICAN MINERALOGIST, 2003, 88 (11-12) :1989-1995
[37]   Height anomalies in tapping mode atomic force microscopy in air caused by adhesion [J].
VanNoort, SJT ;
VanderWerf, KO ;
DeGrooth, BG ;
VanHulst, NF ;
Greve, J .
ULTRAMICROSCOPY, 1997, 69 (02) :117-127
[38]   SUBSTRATE PREPARATION FOR RELIABLE IMAGING OF DNA-MOLECULES WITH THE SCANNING FORCE MICROSCOPE [J].
VESENKA, J ;
GUTHOLD, M ;
TANG, CL ;
KELLER, D ;
DELAINE, E ;
BUSTAMANTE, C .
ULTRAMICROSCOPY, 1992, 42 :1243-1249
[39]   ANALYSIS AND IMPLICATIONS OF THE EDGE STRUCTURE OF DIOCTAHEDRAL PHYLLOSILICATES [J].
WHITE, GN ;
ZELAZNY, LW .
CLAYS AND CLAY MINERALS, 1988, 36 (02) :141-146