LTA和FAU沸石与NH4H2PO4熔体反应生成结晶NH4AlP2O7

Susan M. Bradley , Russell F. Howe
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引用次数: 4

摘要

对沸石A (LTA)、X和Y (FAU)与NH4H2PO4熔体在230℃下不同时间(30 min ~ 36 h)反应的研究发现,每种情况下形成的最终产物都具有与焦磷酸铝铵NH4AlP2O7一致的粉末X射线衍射图,其单晶结构尚未见报道。未检测到中间晶相。然而,Si MAS NMR证实了一些Si仍然存在,x射线光电子能谱显示它主要位于晶体表面。发现晶体具有极低的表面积(约10m2−1),因此不具有多孔性。MAS NMR研究发现它由焦磷酸铝中的六坐标铝和四坐标磷组成,在高硅环境中由四坐标硅组成。这些结果与之前的报道相矛盾,该反应产生“磷酸铝硅酸盐,其中磷取代到沸石骨架位置,从而形成有前途的阴离子交换剂”(A. Dyer, S.A. Malik, A. Araya, T.J. McConville,在:P.A. Williams, M.J. Hudson(编),离子交换的最新进展(Pap)。Int。会议交换。过程),1987年,第257-263页。
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Reaction of LTA and FAU zeolites with NH4H2PO4 melts yields crystalline NH4AlP2O7

Study of the reaction of zeolites A (LTA), and X and Y (FAU) with NH4H2PO4 melts at 230°C for varying time periods (30 min to 36 h) found the final product formed in each case to have a powder X-ray diffraction pattern consistent with ammonium aluminum pyrophosphate, NH4AlP2O7, the single crystal structure of which has not been reported. No intermediate crystalline phases were detected. 29Si MAS NMR confirmed, however, that some Si was still present, and X-ray photoelectron spectroscopy revealed it to be located primarily at the crystallite surfaces. The crystallites were found to have an extremely low surface area (ca. 10m2g−1), and hence not to be porous. MAS NMR studies found it to consist of six-coordinate aluminum and four-coordinate phosphorus in the aluminum pyrophosphate, and four-coordinate silicon in a highly siliceous environment. These results contradict the previous report of this reaction producing ‘phosphated aluminosilicates in which phosphorus substitutes into the zeolite framework sites thereby forming promising anion exchangers’ (A. Dyer, S.A. Malik, A. Araya, T.J. McConville, in: P.A. Williams, M.J. Hudson (Eds.), Recent Developments in Ion Exchange (Pap. Int. Conf. Ion Exch. Processes), 1987, pp. 257–263.).

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Author index Subject index Contents Investigation of organosilanes as structure-directing agents in zeolite synthesis The influence of gel properties on the kinetics of crystallization and particulate properties of MFI-type zeolities. I. The influence of time and temperature of gel ageing on the particulate properties of silicalite-1 microcrystals
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