Nature and strength of acid sites in HY zeolites: a multitechnical approach

A. Boréave , A. Auroux , C. Guimon
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引用次数: 93

Abstract

The combination of several physico-chemical techniques such as temperature programmed desorption, microcalorimetry, infrared spectroscopy and photoelectron spectroscopy, together with structural data (by XRD and NMR), has allowed a detailed study of the acidity of commercial HY faujasites, both non-dealuminated and dealuminated by hydrothermal treatment. These techniques have been used with different basic probe molecules such as ammonia, pyridine and 2,6-lutidine (2,6-dimethylpyridine). They have demonstrated the existence of three different regions of acid strength. The weak sites associated to NH3 adsorption heats between 70 and 130 kJ mol−1 are of Lewis and Brönsted types, the former being predominent in the dealuminated zeolites. The sites of intermediary strength are essentially the framework bridged hydroxyl groups (heats between 130 and 150 kJ mol−1). The strong sites (heats above 160 kJ mol−1) contain a significant number of extra-framework Lewis-type sites, but also Brönsted sites. The strength of these sites seems to be due to mutual interactions between Lewis and Brönsted sites. The use of 2,6-lutidine has furthermore allowed us to differentiate between two different populations of Lewis sites.

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HY沸石中酸位的性质和强度:一种多技术方法
结合几种物理化学技术,如程序升温解吸、微量热法、红外光谱和光电子能谱,以及结构数据(通过XRD和NMR),可以详细研究商业HY faujasites的酸度,包括未脱铝和经水热处理脱铝。这些技术已用于不同的碱性探针分子,如氨、吡啶和2,6-lutidine(2,6-二甲基吡啶)。他们已经证明存在三个不同的酸强度区域。NH3吸附热在70 ~ 130 kJ mol−1之间的弱位主要为Lewis型和Brönsted型,其中Lewis型在脱铝沸石中占优势。中间强度的位置基本上是框架桥接羟基(热在130和150 kJ mol−1之间)。强位(温度高于160 kJ mol−1)含有大量的框架外lewis型位,但也含有Brönsted位。这些站点的强大似乎是由于Lewis和Brönsted站点之间的相互作用。2,6-鲁替丁的使用进一步使我们能够区分Lewis位点的两种不同种群。
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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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