Crystal structure of Ag-exchanged levyne intergrown with erionite: single crystal X-ray diffraction and molecular dynamic simulations

Cametti, Georgia; Churakov, Sergey V. (2020). Crystal structure of Ag-exchanged levyne intergrown with erionite: single crystal X-ray diffraction and molecular dynamic simulations. American mineralogist, 105(11), pp. 1631-1638. Mineralogical Society of America 10.2138/am-2020-7500

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The modification of natural zeolites via ion exchange is an efficient technique used to improve their performances and tune their properties for specific applications. In this study, a natural levyne-Ca intergrown with erionite was fully exchanged by Ag+ and its structure (with idealized chemical composition Ag6(Si,Al)18O36∙18H2O) was investigated by combining a theoretical and experimental approach. Single crystal X-ray diffraction data demonstrated that Ag-levyne maintained the R-3m space group, characteristic of the natural levyne. Ag ions distribute over partially occupied sites along the three-fold axis and, differently from the pristine material, at the wall of the 8-membered ring window of the lev cavity. The lack of approximately 30% of Ag ions that could not be located by the structural refinement is ascribed to the strong disorder of the extraframework occupants. The structural results obtained by molecular dynamics simulations are in overall agreement with the experimental data and showed that, on average, Ag+ is surrounded by approximately 2 H2O and 1 framework oxygen at distances between 2.43 and 2.6 Å. Molecular dynamic trajectories indicate that the occurrence of silver inside the D6R cage depends on the water content: silver occupancy of D6R cages is estimated to be 83%, 30%, and 0% when the structure contains 3, 2.5, and 2 H2O per Ag ion, respectively.
The cation-exchange process, as demonstrated by SEM-EDS analyses affects the intergrown erionite as well. A structural characterization of the Ag-erionite phase (with dimension less than 100 μm) was possible by means of a CuKα micro-focus source: structure solution pointed to P63/mmm space group, indicating no change with respect to natural erionite. In agreement with previous studies, K ions in the cancrinite cage could not be exchanged, whereas Ag+ is found in the eri cavity.

Item Type:

Journal Article (Original Article)


08 Faculty of Science > Institute of Geological Sciences

UniBE Contributor:

Cametti, Georgia, Churakov, Sergey


500 Science > 550 Earth sciences & geology




Mineralogical Society of America




Georgia Cametti

Date Deposited:

01 Mar 2021 16:37

Last Modified:

05 Dec 2022 15:48

Publisher DOI:



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