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TEXTURAL PROPERTIES AND CATALYTIC ACTIVITY OF HYDROTALCITES

机译:水滑石的织构性质和催化活性

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Double-layered hydroxides with hydrotalcite structure were synthesized with Mg/Al atomic ratios of 2.5 and 3 and with different contents of exchangeable Cl- and CO32- anions. The basicity of these solids depends on several structural parameters and on the activation temperature. Microcalorimetric measurements, IR spectroscopy using a probe molecule, and a catalytic test reaction were carried out to characterize the basic sites. The structural evolution of the hydrotalcite upon exchange of Cl- for CO32- and calcination temperature shows a transformation with simultaneous removal of CO2 and water without phase segregation up to 673 K. The mixed oxide formed later could reversibly lead to the layered structure upon rehydration and carbonation. This process was studied by microcalorimetry and IR spectroscopy. The adsorption isotherm of CO2 shows an increase of the uptake and consequently of the basicity with initial CO32- content and calcination temperature up to 800 K. IR spectroscopy shows that the carbonation of the mixed oxide is essentially superficial and that the hydrotalcite structure may be restored upon H2O addition and 373-K treatment. Two types of Lewis acid sites related to a linear coordination of CO2 with Mg2+ and Al3+ cations are assigned. The appearance of a bicarbonate species implies that the basic sites are essentially OH groups. Moreover, a small number of strong basic sites, adsorbing CO2 with 140 kJ/mol, probably correspond to O2- centers. Hammett correlation in the condensation reaction of acetone and different substituted benzaldehydes shows analogies between hydrotalcite catalysis and the homogeneous basic reaction. The activities increase with CO32- content, calcination temperature, and Mg/Al ratio of the hydrotalcites. The basic strength of hydrotalcites is comparable to that of piperidine in homogeneous catalysis. (C) 1995 Academic Press, Inc. [References: 39]
机译:合成了具有水滑石结构的双层氢氧化物,其Mg / Al原子比为2.5和3,并且具有不同含量的可交换Cl-和CO32-阴离子。这些固体的碱度取决于几个结构参数和活化温度。进行了微量量热测量,使用探针分子的红外光谱以及催化测试反应来表征碱性位点。 Cl-交换为CO32-和煅烧温度时水滑石的结构演变显示出一种转变,同时去除了CO2和水,没有相分离,直至673K。后来形成的混合氧化物在水合后可逆地导致分层结构碳化。通过微量量热法和红外光谱研究了该过程。 CO2的吸附等温线显示出吸收的增加,因此在初始CO32含量和煅烧温度高达800 K时呈碱性。红外光谱表明,混合氧化物的碳酸化基本上是表面的,水滑石结构可以恢复加水和373-K处理后。分配了与CO2与Mg2 +和Al3 +阳离子线性配位相关的两种类型的Lewis酸位。碳酸氢盐物质的出现暗示碱性位点基本上是OH基团。此外,少量的强碱性位点(以140 kJ / mol吸附CO2)可能对应于O2中心。丙酮和不同取代的苯甲醛缩合反应中的哈米特相关性表明,水滑石催化与均相碱性反应相似。活性随CO3含量,煅烧温度和水滑石的Mg / Al比而增加。在均相催化中,水滑石的基本强度与哌啶相当。 (C)1995 Academic Press,Inc. [参考:39]

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