High-temperature transformations of Cu-rich hydrotalcites

被引:84
作者
Kannan, S [1 ]
Rives, V
Knözinger, H
机构
[1] Cent Salt & Marine Chem Res Inst, Silicates & Catalysis Discipline, Bhavnagar 364002, Gujarat, India
[2] Univ Salamanca, Dept Quim Inorgan, Salamanca 38008, Spain
[3] Univ Munich, Dept Chem Phys Chem, D-81377 Munich, Germany
关键词
Cu-hydrotalcite; in situ powder x-ray diffraction; thermal behavior; FT-IR spectroscopy;
D O I
10.1016/j.jssc.2003.08.023
中图分类号
O61 [无机化学];
学科分类号
070301 ; 081704 ;
摘要
CuM(II)Al ternary hydrotalcites (M(II) = Ni, Co and Mg) with a (Cu + M(II))/Al atomic ratio of 3.0 and Cu/M(II) atomic ratio of 5.0 were synthesized by coprecipitation under low supersaturation. Powder X-ray diffraction of the as-synthesized samples showed a pattern characteristic of hydrotalcite-like (HT-like) structure (JCPDS: 41-1428). Thermal analyses of these samples showed four stages of weight loss/heat change when recorded in nitrogen. Analysis of the evolved gases characterized the nature of these transformations. The thermoanalytical effects differed significantly especially for the high-temperature transformations, when the treatment was performed in oxygen. In situ powder X-ray diffraction of the samples was carried out to elucidate the phase evolution of these compounds. Surprisingly formation of CuO was noted at temperatures around 200degreesC well below the destruction of the layered network. The nature of the resulting phases varied with both the nature of the co-bivalent metal ion and the heating atmosphere. FT-IR spectroscopy confirmed the retention of carbonate ions at higher temperatures (above 700degreesC), although the concentration of carbonate anion (most likely unidentate) varied with the calcination temperature. The crystallinity of CuO increased significantly above 600degreesC, probably through dissociation of copper oxycarbonate. Significant differences in the thermal transformation temperatures (for the third and the fourth transformations) of these samples containing different co-bivalent metal ions were not observed. This suggests that an association of the co-bivalent metal ions and/or trivalent metal ion in this phase is unlikely. A plausible thermal evolution scheme of these hydrotalcites is proposed. (C) 2003 Elsevier Inc. All rights reserved.
引用
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页码:319 / 331
页数:13
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