IR-SPECTRA OF OCTADECYLAMMONIUM-MONTMORILLONITE IN THE RANGE OF THE SI-O VIBRATIONS

被引:30
作者
SLOSIARIKOVA, H
BUJDAK, J
HLAVATY, V
机构
[1] Department of Inorganic Chemistry, Faculty of Natural Sciences, Comenius University, Bratislava
来源
JOURNAL OF INCLUSION PHENOMENA AND MOLECULAR RECOGNITION IN CHEMISTRY | 1992年 / 13卷 / 03期
关键词
CLAY; SMECTITES; MONTMORILLONITE; OCTADECYLAMMONIUM-MONTMORILLONITE; IR SPECTRA; SI-O VIBRATIONS;
D O I
10.1007/BF01042785
中图分类号
O6 [化学];
学科分类号
0703 ;
摘要
The bonding of octadecylammonium on the internal surface of montmorillonite influences the arrangement of the SiO4 tetrahedra in the structure of montmorillonite. The effect can be observed in smectites with a relatively well-ordered structure as seen in the IR spectra of octadecylammonium-montmorillonite in the range of Si-O vibrations.
引用
收藏
页码:267 / 272
页数:6
相关论文
共 6 条
  • [1] THE INFRA-RED SPECTRA OF LAYER SILICATES
    FARMER, VC
    RUSSELL, JD
    [J]. SPECTROCHIMICA ACTA, 1964, 20 (07): : 1149 - 1173
  • [2] JORDAN JW, 1949, MINERAL MAG, V28, P598
  • [3] EFFECT OF SWELLING ON INFRARED-ABSORPTION SPECTRUM OF MONTMORILLONITE
    LEROT, L
    LOW, PF
    [J]. CLAYS AND CLAY MINERALS, 1976, 24 (04) : 191 - 199
  • [4] NEWMAN ACD, 1987, CHEM CLAYS CLYA MINE
  • [5] SLOSIARIKOVA H, 1986, CHEM PAP, V40, P585
  • [6] Theng B.K.G., 1974, CHEM CLAY ORGANIC RE