The isomorphous substitution of Si(4Al) with P in FAU zeolite and its stabilization effect

Qiang Zhang,Hongjuan Zhao, Xingyu Liu, Rui Li, Tian Xia, Yue Ma, Yuren Wang,Kang Chen, Jiujiang Wang, Penghui Zeng,Honghai Liu,Chaowei Liu, Xionghou Gao, Chunming Xu, Baojian Shen

CHEMICAL ENGINEERING JOURNAL(2024)

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Abstract
It's a dream to make zeolites more stable so as to keep the activity and stability of the catalyst. Phosphorus modification is an effective method, however, the known post -modification predominantly presents as nonframework P, and the P -loss is a big trouble in application. We have discovered that in the reaction of PCl3 or SiCl4 + PCl3 with NaY zeolite, a portion of P enters the framework of the zeolite, forming a PO4-AlO4 structure. Further investigations revealed that P cannot be incorporated into the framework through P for Al isomorphous substitution, but rather through isomorphous substitution with Si(4Al). PCl3 exhibits two effects in reaction: at lower quantities, it mainly undergoes isomorphous substitution with Si(4Al); at higher quantities, it leads to zeolite dealumination generating aluminum vacancies, which disrupt the zeolite framework or promotes Si for Al isomorphous substitution. After hydrothermal aging at 800 degrees C for 4 h, the stable presence of framework PO4- AlO4 implies that the weakest site Si(4Al) becomes the more stable site P(4Al) in the Y zeolite framework. Compared with the JPY (prepared by impregnating (NH4)2HPO4 solution to high silica Y zeolite) sample, after 10 cycles of hydrothermal and water washing treatment, the P2O5 loss rate of DPY (prepared by SiCl4 + PCl3 with NaY) zeolite ranged from 0.4 % to 3.5 %, significantly lower compared to the range of 18.7 % to 25.9 % observed in the JPY sample. This indicates that in DPY zeolite, the interaction between P and the zeolite is stronger and less prone to loss. Moreover, P is more uniformly distributed on the surface and bulk phase of DPY than JPY sample.
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Key words
P -modified zeolite,P for Si(4Al) isomorphous substitution,Hydrothermal stability,P loss,P distribution
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