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首页> 外文期刊>International Journal of Nanotechnology >Creating nanoporosity in Na, Ca and Mg exchanged erionite zeolite
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Creating nanoporosity in Na, Ca and Mg exchanged erionite zeolite

机译:在Na,Ca和Mg交换的堇青石沸石中产生纳米孔隙

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摘要

This paper deals with the emergence of pores in natural erionite zeolite during ion-exchange treatment with aqueous Na+, Mg2+ and Ca2+ solutions of different concentrations. The exchange took place at variable time and temperature of exposure. The effect of this cationic exchange upon the zeolite micropores is analysed by scanning electron microscopy, energy dispersive X-ray spectroscopy and N-2 adsorption at 76 K. The characterisation results suggest the presence of Na+ at the pores' mouth that causes an increased adsorption inside nanocavities as well as on the external area of the exchanged zeolites. The generation of pores emerging in erionite zeolites after ion exchange was evaluated through Dubinin-Astakhov and classical BarrettJoyner-Halenda methods. Depending on the exchanging conditions, Na+ was found to be well distributed and accessible for N-2 adsorption. The results indicate that the tested exchange treatments with Na+ favour creation of emerging pores, as an increase of the adsorption capacity occurs.
机译:本文探讨了用不同浓度的Na +,Mg2 +和Ca2 +水溶液离子交换处理天然毛沸石沸石中孔的出现。交换发生在暴露的时间和温度不同的地方。通过扫描电子显微镜,能量色散X射线光谱和76 K下的N-2吸附,分析了阳离子交换对沸石微孔的影响。表征结果表明,孔口中存在Na +导致吸附增加。纳米腔内部以及交换沸石的外部区域。通过Dubinin-Astakhov和经典的BarrettJoyner-Halenda方法评估了离子交换后毛沸石沸石中出现的孔的生成。根据交换条件,发现Na +分布均匀,可用于N-2吸附。结果表明,随着吸附容量的增加,用Na +进行的测试交换处理有利于形成新出现的孔。

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