引用本文:
高滋, 杨雪敏, 王煜. 正电子湮没与沸石内静电场[J]. 物理化学学报,
1991, 7(04): 425-429.
doi:
10.3866/PKU.WHXB19910410
Citation: Gao Zi, Yang Xue-Min, Wang Yu. Positron Annihilation and Electrostatic Field in Zeolites[J]. Acta Physico-Chimica Sinica, 1991, 7(04): 425-429. doi: 10.3866/PKU.WHXB19910410
Citation: Gao Zi, Yang Xue-Min, Wang Yu. Positron Annihilation and Electrostatic Field in Zeolites[J]. Acta Physico-Chimica Sinica, 1991, 7(04): 425-429. doi: 10.3866/PKU.WHXB19910410
正电子湮没与沸石内静电场
摘要:
本文测定了不同类型沸石的正电子寿命谱。发现o-Ps的湮没寿命, 与沸石静电场之间有良好的对应关系, 静电场愈强, 湮没寿命愈短。根据正电子寿命谱结果。含不同阳离子的Y沸石的静电场强弱次序为KY<NaY<BaY<CaY<CeY; 沸石硅铝比增加, 静电场亦随之增强. 当沸石硅铝比和孔径同时改变时, o-Ps在沸石内表面的湮没寿命受静电场影响较大, 湮没寿命τ_3随静电场增加而缩短, 而o-Ps在沸石笼内的湮没寿命则主要取决于沸石孔径, 湮没寿命τ_4随沸石平均孔径增大而线性地增长.
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关键词:
- 正电子湮没谱; 沸石; 静电场; 孔径
English
Positron Annihilation and Electrostatic Field in Zeolites
Abstract:
Positron annihilation measurements have been carried ont for Y zeolites with different types of cations, faujasites with different Si/Al ratios and zeolites with different structures. The o-Ps annihilation lifetimes are closely correlated with the variations of the electrostatic field in the zeolites. The o-Ps lifetimes are shortened when the electrostatic field in the zeolites is increased. Positron annihilation data show that the electrostatic field of cation-exchanged Y zeolites varies in the order of KY<NaY<BaY<CaY<CeY. As the Si/Al ratio of the faujasites increases the annihilation lifetimes are decreased, because the electrostatic field in the zeolite is increased owing to the diminished shielding from the neighboring cations. For zeolites with different structures and pore sizes the o-Ps annihilation lifetime on the surface is affected mainly by the variation of the electrostatic field in the zeolites, while the o-Ps annihilation lifetime in the cages depends distinctly on the zeolite pore size. The o-Ps annihilation lifetime in the cages is directly proportional to the average pore size of the zeolites. This linear relationship between the o-P annihilation lifetime and the average pore size may be utilized to estimate quickly the pore size of zeolites with unknown structure.
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