Locating Extra-Framework Cations in Low-Silica Zeolites by a Combinatorial Approach of the Direct Space Method and Rietveld Refinement: Application to Ni2+ and Co2+ Enriched Clinoptilolite

被引:9
作者
Garcia-Basabe, Yunier [2 ,3 ]
Gomez, Ariel [1 ]
Rodriguez-Iznaga, Inocente [4 ]
Montero, Alfredo [5 ]
Vlaic, Gilberto [6 ]
Lausi, Andrea [6 ]
Rabdel Ruiz-Salvador, A. [2 ]
机构
[1] Univ Guelph, Dept Phys, Guelph, ON N1G 2W1, Canada
[2] Univ Havana, Zeolites Engn Lab, IMRE, Havana 10400, Cuba
[3] Univ Matanzas, Dept Phys, Fac Mech & Chem Engn, Matanzas 40100, Cuba
[4] Univ Havana, Mat Technol Lab, IMRE, Havana 10400, Cuba
[5] CEADEN, Dept Anal, Havana, Cuba
[6] Elettra Synchrotron Light Source, Trieste, Italy
关键词
RAY-POWDER DIFFRACTION; SYNCHROTRON X-RAY; CRYSTAL-STRUCTURE; EXCHANGED HEULANDITE; NEUTRON-DIFFRACTION; ION-EXCHANGE; CRYSTALLOGRAPHIC DETERMINATION; NMR-SPECTROSCOPY; NATURAL ZEOLITES; HEAVY-METALS;
D O I
10.1021/jp9105772
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
The location of extra-framework cations in low-silica zeolites is determined from in-house X-ray powder diffraction pattern by a successful implementation of a newly developed methodology. The method combines reciprocal and direct space methods plus a cost function that accounts for simultaneous lit of the chemical composition and the X-ray diffractogram. We demonstrated that the iterative combination of relaxation methods (Monte Carlo exploration and lattice energy minimization) helps to improve the structural refinement. The methodology is successfully applied to the study of natural clinoptilolite samples enriched with Ni and Co; in both cases. two different cation sites were found octahedrally coordinated to water molecules. The most populated site is located in the center of the A channel, while the second one is found in the window of the B channel. This result was validated using XANES and EXAFS spectroscopies.
引用
收藏
页码:5964 / 5974
页数:11
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