Infrared spectroscopy as a tool for the analysis of framework topology and extra-framework components in microporous cancrinite- and sodalite-related aluminosilicates

被引:7
|
作者
Chukanov, Nikita V. [1 ,2 ]
Aksenov, Sergey M. [3 ,4 ]
V. Pekov, Igor V. [2 ]
机构
[1] RAS, Inst Problems Chem Phys, Moscow 142432, Russia
[2] Moscow MV Lomonosov State Univ, Fac Geol, Vorobievy Gory, Moscow 119991, Russia
[3] Russian Acad Sci, Kola Sci Ctr, Lab Arctic Mineral & Mat Sci, 14 Fersman str, Apatity 184209, Russia
[4] Geol Inst, Russian Acad Sci, Kola Sci Ctr, 14 Fersman str, Apatity 184209, Russia
基金
俄罗斯科学基金会;
关键词
Microporous aluminosilicate; Cancrinite; Sodalite; Multilayer cancrinite-related material; STACKING-SEQUENCE OCCURRENCE; LOVOZERO ALKALINE PLUTON; AB-TYPE FRAMEWORK; CENTER-DOT H2O; CRYSTAL-CHEMISTRY; GROUP MINERALS; VOLCANIC COMPLEX; IR SPECTROSCOPY; FTIR; SOMMA;
D O I
10.1016/j.saa.2022.121993
中图分类号
O433 [光谱学];
学科分类号
0703 ; 070302 ;
摘要
The identification of the framework type in multilayer cancrinite- and sodalite-group minerals and synthetic compounds is predominantly based on the unit-cell dimensions determined from powder or single-crystal X-ray diffraction data, by analogy with previously characterized samples with known crystal structures. However, topological type of the framework cannot be reliably determined in this way because of the different possible ABC staking sequences and different sets of cages with the same number of layers in the repeat unit. To solve this problem, additional criteria are required. The use of infrared (IR) spectroscopy makes it possible to distinguish
引用
收藏
页数:10
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