Ion-exchange equilibria of synthetic 4A zeolite with Ni2+, Co2+, Cd2+ and Zn2+ ions

I. Gal, O. Janković, S. Malčić, P. Radovanov, M. Todorović
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引用次数: 48

Abstract

Linde 4A zeolite was converted to Ni, Co, Zn and Cd forms by replacing sodium ions with divalent cations. The replacement was from 82%(Ni) up to 100%(Cd). Chemical, T.G.A., D.T.A. and X-ray analysis of the divalent metal zeolites have been made and data on the composition of the unit cells and the thermal stability of the lattices were obtained. Ni-zeolite is unstable, its crystal lattice being completely destroyed above 70°C, whereas Co-, Zn- and Cd-zeolites are stable up to 750–850°C. The adsorption of water on the latter zeolites is reversible. Ion-exchange isotherms for Co2+, Zn2+ and Cd2+ at three temperatures were obtained and the thermodynamic functions, ΔG°, ΔH° and ΔS°, of the ion-exchange equilibria calculated. The thermodynamic data are discussed with respect to hydration and size of the cations. A possible explanation of the instability of Ni-zeolite is suggested.
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合成4A沸石与Ni2+、Co2+、Cd2+和Zn2+离子的离子交换平衡
用二价阳离子取代钠离子,将林德4A沸石转化为Ni、Co、Zn和Cd。替换量从82%(Ni)到100%(Cd)。对二价金属沸石进行了化学分析、热能谱分析、差热能谱分析和x射线分析,得到了单元胞的组成和晶格的热稳定性数据。ni -沸石不稳定,其晶格在70°C以上完全破坏,而Co-, Zn-和cd -沸石在750-850°C时稳定。后一种沸石对水的吸附是可逆的。得到了三种温度下Co2+、Zn2+和Cd2+的离子交换等温线,并计算了离子交换平衡的热力学函数ΔG°、ΔH°和ΔS°。热力学数据讨论了有关水化和大小的阳离子。对镍沸石的不稳定性提出了一种可能的解释。
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