Intercalation of kaolinite with acetamide

被引:38
作者
Frost, RL
Kristof, J
Paroz, GN
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
acetamide; DRIFT spectroscopy; intercalation; hydrogen bonding; kaolinite; Raman spectroscopy; X-ray diffraction;
D O I
10.1007/s002690050185
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
Upon intercalation of both ordered (low defect) and disordered thigh defect) kaolinites with acetamide, two types of interaction are observed. Firstly, hydrogen bonding between the NH2 groups of the acetamide with the siloxane oxygens is formed, as evidenced by the formation of two new bands at 3400 and 3509 cm(-1). Secondly, the appearance of additional bands at similar to 3600 cm(-1) in both the infrared and Raman spectra of the acetamide intercalates is attributed to a second type of hydrogen bonding by the interaction of the C=O group and the inner sur face hydroxyls. Changes in the intensity of the hydroxyl deformation modes in the 895 to 940 cm(-1) region are attributed to the changes in the hydrogen bonding of the kaolinite surfaces. It is proposed that the hydrogen bonding between the adjacent kaolinite layers is replaced with hydrogen bonding between both kaolinite surfaces and the acetamide molecule. Changes in the molecular structure of acetamide are observed upon intercalation. The amide 1 band is lost and replaced with a well-defined NH2 deformation vibration. The loss of the amide 1 band is attributed the hydrogen bond formation between the amide hydrogens and the siloxane surface. The bands of the C=O group at 1680 and 1740 cm(-1) become a single band at 1680 cm(-1). The amide 2 band remains unchanged. The lack of intensity of the 1740 cm(-1) band is attributed to the formation of hydrogen bonding between the inner surface hydroxyl groups and the carbonyl group.
引用
收藏
页码:257 / 263
页数:7
相关论文
共 9 条
[1]   AMIDE MODES AND PROTEIN CONFORMATION [J].
BANDEKAR, J .
BIOCHIMICA ET BIOPHYSICA ACTA, 1992, 1120 (02) :123-143
[2]   Raman microprobe spectroscopy of halloysite [J].
Frost, RL ;
Shurvell, HF .
CLAYS AND CLAY MINERALS, 1997, 45 (01) :68-72
[3]   FT-Raman spectroscopy of the lattice region of kaolinite and its intercalates [J].
Frost, RL ;
Tran, TH ;
Kristof, J .
VIBRATIONAL SPECTROSCOPY, 1997, 13 (02) :175-186
[4]   The structure of an intercalated ordered kaolinite - a Raman microscopy study [J].
Frost, RL ;
Tran, TH ;
Kristof, J .
CLAY MINERALS, 1997, 32 (04) :587-596
[5]   Hydroxyl deformation in kaolins [J].
Frost, RL .
CLAYS AND CLAY MINERALS, 1998, 46 (03) :280-289
[6]  
Frost RL, 1996, CAN J APPL SPECTROSC, V41, P10
[7]  
FROST RL, 1997, CLAY MINER, V32, P293
[8]  
Hinckley DN., 1962, CLAYS CLAY MINER, V11, P229, DOI [10.1346/ccmn.1962.0110122, DOI 10.1346/CCMN.1962.0110122]
[9]  
WADA K, 1961, AM MINERAL, V46, P79