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首页> 外文期刊>Journal of Thermal Analysis and Calorimetry >Thermal decomposition of hydrotalcite with molybdate and vanadate anions in the interlayer
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Thermal decomposition of hydrotalcite with molybdate and vanadate anions in the interlayer

机译:水滑石与钼酸盐和钒酸盐阴离子在中间层中的热分解

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摘要

Hydrotalcites containing carbonate, vanadate and molybdate were prepared by coprecipitation. The resulting materials were characterized by XRD, and TG/DTA to determine the stability of the hydrotalcites synthesized. The thermal decomposition of carbonate hydrotalcites consist of two decomposition steps between 300 and 400°C, attributed to the simultaneous dehydroxylation and decarbonation of the hydrotalcite lattice. Water loss ascribed to dehydroxylation occurs in two decomposition steps, where the first step is due to the partial dehydroxylation of the lattice, while the second step is due to the loss of water interacting with the interlayer anions. Dehydroxylation results in the collapse of the hydrotalcite structure to that of its corresponding metal oxides, including MgO, Al2O3, MgAl2O4, NaMg4(VO4)3 and Na2Mg4(MoO4)5. The presence of oxy-anions proved to be beneficial in the stability of the hydrotalcite structure, shown by the delay in dehydroxylation of oxy-anion containing hydrotalcites compared to the carbonate hydrotalcite. This is due to the substantial amount of hydroxyl groups involved in a network of hydrogen bonds involving the intercalated anions. Therefore, the stability of the hydrotalcite structure appears to be dependent on the type of anion present in the interlayer. The order of thermal stability for the synthesized hydrotalcites in this study is Syn-HT-V>Syn-HT-Mo> Syn-HT-CO3-V>Syn-HT-CO3-Mo>Syn-HT-CO3. Carbonate containing hydrotalcites prove to be less stable than oxy-anion only hydrotalcites.
机译:通过共沉淀制备含有碳酸盐,钒酸盐和钼酸盐的水滑石。通过XRD和TG / DTA对所得材料进行表征,以确定合成的水滑石的稳定性。碳酸盐水滑石的热分解包括300至400°C的两个分解步骤,这归因于水滑石晶格的同时脱羟基和脱碳。归因于脱羟基的水损失在两个分解步骤中发生,其中第一步是由于晶格的部分去羟基化,而第二步是由于与层间阴离子相互作用的水的损失。脱羟基作用导致水滑石结构坍塌为相应的金属氧化物,包括MgO,Al2 O3 ,MgAl2 O4 ,NaMg4 (VO4 < / sub>)3 和Na2 Mg4 (MoO4 )5 。含氧阴离子的存在被证明对水滑石结构的稳定性是有益的,这与含碳酸水滑石的含氧阴离子水滑石的脱羟基延迟有关。这是由于涉及插入阴离子的氢键网络中大量羟基所致。因此,水滑石结构的稳定性似乎取决于存在于中间层中的阴离子的类型。本研究中合成水滑石的热稳定性顺序为:Syn-HT-V> Syn-HT-Mo> Syn-HT-CO3 -V> Syn-HT-CO3 -Mo> Syn -HT-CO3 。与仅含氧阴离子的水滑石相比,含碳酸盐的水滑石的稳定性较差。

著录项

  • 来源
    《Journal of Thermal Analysis and Calorimetry》 |2008年第3期|879-886|共8页
  • 作者单位

    Inorganic Materials Research Program School of Physical and Chemical Sciences Queensland University of Technology GPO Box 2434 Brisbane Queensland 4001 Australia;

    Inorganic Materials Research Program School of Physical and Chemical Sciences Queensland University of Technology GPO Box 2434 Brisbane Queensland 4001 Australia;

    Inorganic Materials Research Program School of Physical and Chemical Sciences Queensland University of Technology GPO Box 2434 Brisbane Queensland 4001 Australia;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    carbonate; hydrotalcite; iowaite; molybdate; pyroaurite; stitchtite; thermogravimetry; vanadate;

    机译:碳酸盐;水滑石;碘水;钼酸盐;焦铁矿;针铁矿;热重法;钒酸盐;

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