Structure of natural and NH4-exchanged Sasbach faujasite: a single-crystal study

被引:2
作者
Fantini, Riccardo [1 ]
Arletti, Rossella [2 ,3 ]
Pastero, Linda [2 ]
Quartieri, Simona [4 ]
Di Renzo, Francesco [5 ]
Camara, Fernando [6 ]
Vezzalini, Giovanna [1 ]
机构
[1] Univ Modena & Reggio Emilia, Dipartimento Sci Chim & Geol, Via Campi 103, I-41125 Modena, Italy
[2] Univ Torino, Dipartimento Sci Terra, Via Valperga Caluso 35, I-10125 Turin, Italy
[3] NIS Ctr Nanostruct Interfaces & Surfaces, Via Quarello 4, I-10100 Turin, Italy
[4] Univ Messina, Dipartimento Sci Matemat & Informat, Sci Fis & Sci Terra, Viale F Stagno dAlcontres 31, I-98166 Messina S Agata, Italy
[5] CNRS UM ENSCM, UMR5253, Inst Charles Gerhardt Montpellier, 240 Av Emile Jeanbrau, F-34296 Montpellier 5, France
[6] Univ Milan, Dipartimento Sci Terra, Via Mangiagalli 34, I-20133 Milan, Italy
关键词
natural faujasite; FAU; NH4-exchanged form; crystal structure; single-crystal X-ray diffraction; zeolite; STRUCTURE REFINEMENT; ZEOLITE MORDENITE; DYE MOLECULES; ADSORPTION; DECOMPOSITION; LOCATION;
D O I
10.1127/ejm/2018/0030-2745
中图分类号
P57 [矿物学];
学科分类号
070901 ;
摘要
The interest for the environmental, industrial and technological applications of Si-rich zeolites is very high. Among the large-pore zeolites, faujasite is one of the most exploited. The aim of this paper is to obtain detailed structural information on natural and NH4-exchanged faujasite before using this zeolite for dealumination tests, targeting the realization of large single crystals of all-silica faujasite. As one of the most Si-rich natural samples, faujasite from Sasbach (Na13.64K0.87Mg10.46Ca8.89Sr0.34(Al51.95Si139.57)O-384 center dot 272.29 H2O; space group Fd-3m;a = 24.6906(2) angstrom) was chosen for study. Single-crystal X-ray diffraction structural refinements of both natural and NH4-exchanged samples are reported and discussed. In the natural faujasite sample, almost all the extraframework species could be located for the first time. In the NH4-exchanged sample the ammonium and water molecule sites were located. Ammonium cations occupy two of the sites occupied by the extraframework species in the original mineral.
引用
收藏
页码:515 / 523
页数:9
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