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

R. Job, W. Fahrner, A. Yoshida
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摘要

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