Sorption and Ion Exchange Behaviour of Natural Zeolite Packing

C. Purnomo, Bernice Lenora, W. Budhijanto, H. Hinode
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引用次数: 6

Abstract

It is well known that zeolite is an efficient metal ions adsorbent. The excess charge of the zeolite b u lding blocks i.e. (AlO4) -5 and (SiO4) -4 creating a negative surface charge that attract me tal cations. Beside the surface charge, zeolite als o has three dimensional pore structure and reasonably large surface area which also can be used as adsor ption sites. Ease of cation uptake make it suitable for many process with adsorption and desorption application. This st udy was conducted to observe the sorption and ion exchange behaviour of zeolite-betonite rings toward iron and cobalt cations. The results shows that the adsorption patterns foll ow Langmuir isotherm with the highest uptake capaci ty is 59,9 mg/g for Fe(II) and 57. 8 mg/g for Co(II).
天然沸石填料的吸附和离子交换行为
沸石是一种高效的金属离子吸附剂。沸石上的多余电荷由(AlO4) -5和(SiO4) -4组成,产生负电荷,吸引金属离子。除了表面电荷外,沸石还具有三维孔隙结构和相当大的表面积,也可以作为吸附位点。阳离子吸附性能好,适用于多种吸附解吸工艺。本文研究了沸石-膨润土环对铁和钴离子的吸附和离子交换行为。结果表明,吸附模式符合Langmuir等温线,对Fe(II)的最高吸收率分别为59、9 mg/g和57 mg/g。Co(II)为8 mg/g。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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