CHARACTERIZATION OF UNTREATED AND ALKYLAMMONIUM ION-EXCHANGED ILLITE/SMECTITE BY HIGH-RESOLUTION TRANSMISSION ELECTRON-MICROSCOPY

被引:11
作者
CETIN, K [1 ]
HUFF, WD [1 ]
机构
[1] UNIV CINCINNATI,DEPT GEOL,CINCINNATI,OH 45221
关键词
ALKYLAMMONIUM; CLAYS; DIAGENESIS; ILLITE; INTERSTRATIFICATION; SMECTITE; TRANSMISSION ELECTRON MICROSCOPY;
D O I
10.1346/CCMN.1995.0430308
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
High resolution transmission electron microscopy (HRTEM) have been performed on dispersed portions of one R > 1 and two R3 illite/smectite (I/S) samples from Silurian K-bentonites. R > 1 sample was studied by HRTEM before and after alkylammonium ion treatment and R3 samples were studied only after alkylammonium ion treatment. The HRTEM images of the chemically untreated R > 1 sample were predominated by lattice fringe contrast with 20-40 Angstrom periods, interpreted to represent various ordered VS units. HRTEM images of the three alkylammonium-treated samples displayed very small, dispersed particles composed of illite packets separated by alkylammonium expanded interlayers. In the R > 1 sample, illite packets were mostly 20 Angstrom to 40 Angstrom thick whereas in R3 samples they were predominantly over 40 A. Although a good degree of dispersion of the bulk samples was achieved, dispersed particles recorded on images were thicker than the fundamental particles postulated by Nadeau and coworkers. Alkylammonium ion-expanded interlayer thicknesses point out a trend toward a higher charge in the expandable interlayers (i.e., illite particle surfaces) with increasing illite content from the R > 1 sample to the R3 samples. In the R3 samples, the interlayer charge is sufficiently high to be vermiculitic.
引用
收藏
页码:337 / 345
页数:9
相关论文
共 35 条
[1]  
AHN JH, 1989, CLAY CLAY MINER, V37, P542
[2]  
AHN JH, 1986, CLAY CLAY MINER, V34, P165
[3]  
AHN JH, 1990, AM MINERAL, V75, P267
[4]  
ALTANER SP, 1988, AM MINERAL, V73, P766
[6]  
CETIN K, 1995, IN PRESS CLAYS CLAY
[7]  
CETIN K, 1992, THESIS U CINCINNATI
[8]  
EBERL DD, 1988, AM MINERAL, V43, P1335
[9]   LAYER-CHARGE AND CATION-EXCHANGE CHARACTERISTICS OF VERMICULITE (WEATHERED BIOTITE) ISOLATED FROM A GRAY LUVISOL IN NORTHEASTERN SASKATCHEWAN [J].
GHABRU, SK ;
MERMUT, AR ;
STARNAUD, RJ .
CLAYS AND CLAY MINERALS, 1989, 37 (02) :164-172
[10]   HIGH-RESOLUTION TRANSMISSION ELECTRON-MICROSCOPY OF MIXED-LAYER ILLITE SMECTITE - COMPUTER-SIMULATIONS [J].
GUTHRIE, GD ;
VEBLEN, DR .
CLAYS AND CLAY MINERALS, 1989, 37 (01) :1-11