Hydroxyl-stretching bands in polarized micro-Raman spectra of oriented single-crystal Keokuk kaolinite

被引:21
作者
Shoval, S
Yariv, S
Michaelian, KH
Boudeulle, M
Panczer, G
机构
[1] Open Univ, Geol Grp, Dept Nat Sci, IL-61392 Tel Aviv, Israel
[2] Hebrew Univ Jerusalem, Dept Inorgan & Analyt Chem, IL-91904 Jerusalem, Israel
[3] Nat Res Canada, Western Res Ctr, CANMET, Devon, AB T9G 1A8, Canada
[4] Univ Lyon 1, CNRS, LPCML, UMR 5620, F-69622 Villeurbanne, France
关键词
hydroxyl groups; IR spectra; kaolinite; Raman spectra; SEM micrographs;
D O I
10.1346/000986002761002676
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
Polarized micro-Raman spectra of a single large crystal of Keokuk kaolinite were recorded in the OH-stretching region with the laser beam directed along the different crystal axes. The Raman spectra are characterized by five OH-stretching bands at 3694, 3683, 3668, 3650 and 3620 cm(-1) labeled A. Z. B. C and D, respectively. The relative intensities of these five bands depend on the orientation of the crystal and the scattering geometry. The spectra agree with the assertion that bands A and Z arise from out-of-plane vibrations, whereas band D corresponds to an in-plane vibration. The area ratios of the various bands were calculated from fitted curves of spectra recorded with the electric vector of the laser beam parallel to different crystallographic planes. The increments in the relative areas of bands B and C were parallel to those of bands A and Z and it appears that out-of-plane vibrations made considerable contributions to these bands also. From the change of area ratios with the change in the direction of the electric vector of the laser beam, bands A and Z were attributed to LO and TO frequencies of one inner-surface hydroxyl vibration. Bands A + Z, B, C and D were attributed to the vibrations of the hydroxyls assigned by Bish (1993) as OH(3), OH(4), OH(2) and OH(l), respectively. These observations were supported by photoacoustic and transmission IR spectra.
引用
收藏
页码:56 / 62
页数:7
相关论文
共 23 条
[1]   RIETVELD REFINEMENT OF THE KAOLINITE STRUCTURE AT 1.5-K [J].
BISH, DL .
CLAYS AND CLAY MINERALS, 1993, 41 (06) :738-744
[2]   RIETVELD REFINEMENT AND FOURIER-TRANSFORM INFRARED SPECTROSCOPIC STUDY OF THE DICKITE STRUCTURE AT LOW-TEMPERATURE [J].
BISH, DL ;
JOHNSTON, CT .
CLAYS AND CLAY MINERALS, 1993, 41 (03) :297-304
[3]   Differing effects of particle size and shape in the infrared and Raman spectra of kaolinite [J].
Farmer, VC .
CLAY MINERALS, 1998, 33 (04) :601-604
[4]   Transverse and longitudinal crystal modes associated with OH stretching vibrations in single crystals of kaolinite and dickite [J].
Farmer, VC .
SPECTROCHIMICA ACTA PART A-MOLECULAR AND BIOMOLECULAR SPECTROSCOPY, 2000, 56 (05) :927-930
[5]   FOURIER-TRANSFORM RAMAN-SPECTROSCOPY OF KAOLINITE, DICKITE AND HALLOYSITE [J].
FROST, RL .
CLAYS AND CLAY MINERALS, 1995, 43 (02) :191-195
[6]  
Frost RL, 1996, CAN J APPL SPECTROSC, V41, P10
[7]  
HAYES JB, 1963, IOWA ACAD SCI, V70, P261
[8]   RAMAN-SPECTROSCOPIC STUDY OF KAOLINITE IN AQUEOUS SUSPENSION [J].
JOHNSTON, CT ;
SPOSITO, G ;
BIRGE, RR .
CLAYS AND CLAY MINERALS, 1985, 33 (06) :483-489
[9]  
Johnston CT, 1998, AM MINERAL, V83, P75
[10]   POLARIZED SINGLE-CRYSTAL FOURIER-TRANSFORM INFRARED MICROSCOPY OF OURAY DICKITE AND KEOKUK KAOLINITE [J].
JOHNSTON, CT ;
AGNEW, SF ;
BISH, DL .
CLAYS AND CLAY MINERALS, 1990, 38 (06) :573-583