Raman spectroscopy of hydrazine-intercalated kaolinite at 77, 298, 323, 343 and 358 K

被引:7
作者
Martens, WN
Ding, Z
Frost, RL
Kristof, J
Kloprogge, JT
机构
[1] Queensland Univ Technol, Ctr Instrumental & Dev Chem, Brisbane, Qld 4001, Australia
[2] Univ Veszprem, Dept Analyt Chem, H-8201 Veszprem, Hungary
关键词
D O I
10.1002/jrs.812
中图分类号
O433 [光谱学];
学科分类号
0703 ; 070302 ;
摘要
The Raman spectrum at 298 K of hydrazine-intercalated kaolinite shows a single band at 3620 cm(-1). No other hydroxyl stretching bands are observed. Upon obtaining the spectrum at liquid nitrogen temperature the band is observed at 3616 cm(-1), the same position as for the inner hydroxyl of the non-intercalated kaolinite. Hence this band is assigned to the inner hydroxyl of kaolinite. After exposure to the atmosphere for 10 min and upon obtaining spectra at 77 K, two additional bands are observed at 3607 and 3625 cm(-1). These additional bands are only observed after the onset of deintercalation. The band observed at 3625 cm(-1) is assigned to the inner surface hydroxyls, hydrogen bonded to the hydrazine. The fact that the band is only observed after the onset of deintercalation suggests that the band is Raman inactive and infrared active. Raman spectroscopic analysis indicates that there are two types of hydrazine molecules as evidenced by two NH bands, (a) weakly hydrogen bonded as evidenced by two bands observed around 3300 and 3312 cm(-1) and (b) a strongly hydrogen-bonded hydrazine as evidenced by bands at 2890 and 2948 cm(-1). The two NH symmetric stretching bands at around 3300 and 3312 cm(-1) combined with the two NH antisymmetric stretching bands at 3361 and 3367 cm(-1) suggest that there are two slightly different NH2 units in the hydrazine-intercalated complex. Copyright (C) 2002 John Wiley Sons, Ltd.
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页码:31 / 36
页数:6
相关论文
共 10 条
[1]   Deintercalation of hydrazine-intercalated low-defect kaolinite [J].
Frost, RL ;
Kloprogge, JT ;
Kristof, J ;
Horvath, E .
CLAYS AND CLAY MINERALS, 1999, 47 (06) :732-741
[2]   Effect of water on the formamide-intercalation of kaolinite [J].
Frost, RL ;
Kristof, J ;
Horvath, E ;
Kloprogge, JT .
SPECTROCHIMICA ACTA PART A-MOLECULAR AND BIOMOLECULAR SPECTROSCOPY, 2000, 56 (09) :1711-1729
[3]   New techniques for studying the intercalation of kaolinites from Georgia with formamide [J].
Frost, RL ;
Lack, DA ;
Paroz, GN ;
Tran, THT .
CLAYS AND CLAY MINERALS, 1999, 47 (03) :297-303
[4]   Vibrational spectroscopy of formamide-intercalated kaolinites [J].
Frost, RL ;
Kristof, J ;
Horvath, E ;
Kloprogge, JT .
SPECTROCHIMICA ACTA PART A-MOLECULAR AND BIOMOLECULAR SPECTROSCOPY, 2000, 56 (06) :1191-1204
[5]   INFLUENCE OF HYDRAZINE ON THE VIBRATIONAL-MODES OF KAOLINITE [J].
JOHNSTON, CT ;
STONE, DA .
CLAYS AND CLAY MINERALS, 1990, 38 (02) :121-128
[6]  
Kristóf J, 2001, J THERM ANAL CALORIM, V63, P279
[7]   Thermal behaviour of kaolinite intercalated with formamide, dimethyl sulphoxide and hydrazine [J].
Kristóf, J ;
Frost, RL ;
Kloprogge, JT ;
Horváth, E ;
Gábor, M .
JOURNAL OF THERMAL ANALYSIS AND CALORIMETRY, 1999, 56 (02) :885-891
[8]   INFRARED STUDIES OF HYDROGEN BONDING INTERACTION BETWEEN KAOLINITE SURFACES AND INTERCALATED POTASSIUM ACETATE HYDRAZINE FORMAMIDE AND UREA [J].
LEDOUX, RL ;
WHITE, JL .
JOURNAL OF COLLOID AND INTERFACE SCIENCE, 1966, 21 (02) :127-&
[9]  
WADA K, 1962, AM MINERAL, V46, P78
[10]  
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