摘要
测量了NaY及USY沸石的正电子寿命谱.得到NaY沸石有四个寿命分量:两个短寿命分量和两个长寿命分量.两个长寿命分量中,τ3,τ4分别是oPs在β笼和超笼中的湮没.USY沸石有五个寿命分量:两个短寿命分量和三个长寿命分量,三个长寿命分量中,τ3为oPs在笼中的湮没,τ4,τ5分别为oPs在“二次微孔”和“二次中孔”中的湮没.与NaY沸石相比,在真空中,USY的τ4增加到14ns,τ5增加到92ns.实验证实了离子交换及高温水热处理对沸石的孔结构有很大的影响.还测量了USY沸石在不同大气压力下(0—01MPa)的正电子寿命谱,随着USY沸石吸附空气的增加,τ5,I5明显减少,τ5从(真空中)92ns下降57ns(01MPa),I5从15%下降到9%.研究表明,空气中的O2不仅猝灭了Ps,抑制了Ps的生成,而且减小了oPs的寿命.另外,空气密度的增加使oPs的Pickof湮没增加,也抑制了Ps的生成.
The structures of NaY and ultrastability Y type (USY) zeolite were studied by positron lifetime spectroscopy.Four lifetimes could be obtained in NaY zeolite,the two larger components were assigned to be o Ps annihilation in the β cage and supercage respectively.In USY zeolite,however,an additional lifetime component τ 5 was observed,which was about 92ns in vacuum with continuous distribution from 39ns to 142ns by the Laplace inversion analysis of lifetime spectrum.The second larger lifetimes τ 4 also increased to 14ns,compared to that in NaY zeolite.Existence of the longer lifetimes τ 4 and τ 5 is due to the porous structure of USY.The positron lifetime in USY zeolite was also measured as a function of air pressure ranging from 0 (vacuum) to 0 1MPa.The most interesting was the variation of the largest components τ 5 and I 5.They both decreased with increasing air pressure.The results can be explained as follows.First,the oxygen contained in the air could quench the Ps and reduce its lifetime and intensity.Second,the increasing density of air could also increase the probability of o Ps pick off annihilation and reduce its formation.These would lead to the decrease of its lifetime and intensity.
出处
《物理学报》
SCIE
EI
CAS
CSCD
北大核心
1997年第11期2267-2273,共7页
Acta Physica Sinica