A concise study on luminescence of dealuminated faujasite and the formation of nanoclusters in the zeolite host structure

R. Job, W. Fahrner, A. Yoshida
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Abstract

Strong cathodoluminescence (CL) in the blue spectral range was observed in dealuminated Faujasite (DAF) zeolite-Y. CL and photoluminescence (PL) measurements are discussed on the background of the formation of nanoclusters in the open cages of the zeolite host structure. DAF was mixed with a SnCl/sub 2/ solution and subsequently dried under stirring and annealed in H/sub 2/- or O/sub 2/-ambient to establish metallic Sn or semiconducting SnO/sub 2/ clusters in the zeolite pores. Samples with various nominal weight ratios were prepared, i.e. SnO/sub 2//DAF=0.15-0.8 and Sn/DAF=0.1-0.6. X-ray powder diffraction (XRD) analysis shows that the nominal incorporation of Sn or SnO/sub 2/ resulted in weak reduction of the lattice constants. At 77 K all samples exhibit a strong CL signal in the blue spectral range, which was clearly visible by the eye, but no significant spectral properties which might be attributed to a nanocluster formation could be deduced. PL measurements at 77 K do not give significant verification of a cluster formation, too. One can conclude that the strong CL mainly originates from the DAF and that the incorporation of Sn or SnO/sub 2/ clusters was either rather poor and/or has no significant influence on the luminescence behavior.
脱铝faujasite的发光及在沸石主体结构中形成纳米团簇的简要研究
脱铝Faujasite (DAF)沸石y在蓝色光谱范围内有很强的阴极发光(CL)。本文讨论了在沸石基质结构的开放笼中形成纳米团簇的背景下,CL和光致发光(PL)的测量。将DAF与SnCl/ sub2 /溶液混合,搅拌干燥,在H/ sub2 /-或O/ sub2 /-环境中退火,在沸石孔隙中形成金属Sn或半导体SnO/ sub2 /团簇。制备了SnO/sub 2//DAF=0.15 ~ 0.8和Sn/DAF=0.1 ~ 0.6的标称重量比样品。x射线粉末衍射(XRD)分析表明,Sn或SnO/ sub2 /的名义掺入导致晶格常数的微弱降低。在77 K时,所有样品在蓝色光谱范围内都表现出强烈的CL信号,这可以用眼睛清楚地看到,但没有可能归因于纳米团簇形成的显著光谱特性可以推断出来。在77 K下的PL测量也没有给出星团形成的重要验证。可见,强CL主要来源于DAF, Sn或SnO/sub - 2/簇的掺入对发光行为的影响较差或不显著。
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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