Journal
JOURNAL OF HAZARDOUS MATERIALS
Volume 408, Issue -, Pages -Publisher
ELSEVIER
DOI: 10.1016/j.jhazmat.2020.124419
Keywords
Zeolite; Cesium; Strontium; Ion exchange; Structural dependence
Categories
Funding
- National Research Foundation of Korea - Korean Government [NRF2020M2A8A5023551]
- Basic Science Research Program through the National Research Foundation of Korea [NRF-2020R1A2C3003694]
- C.EM, SPST of ShanghaiTech University [EM02161943]
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Zeolites with high Si/Al ratios exhibit enhanced affinity to Cs+ ions, while zeolites containing 8-membered rings show extra-high selectivity for Cs+. In contrast, the affinity of Sr2+ ions to zeolites decreases as the Si/Al ratio increases, and Sr2+ exchange is less dependent on zeolite structures due to strong hydration. The kinetics of Sr2+ exchange is slower than that of Cs+ exchange due to the bulkiness of hydrated Sr2+ ions, with larger micropore channels beneficial for faster exchange kinetics.
Zeolites are widely used for capturing radioactive Cs+ and Sr2+, but the important structural factors determining their performance have not been clearly understood. To investigate the structure-property relationship, we prepared thirteen zeolites with various structures and Si/Al ratios. Ion-exchange experiments revealed that Cs+ exhibited an enhanced affinity to zeolites with high Si/Al ratios, which could be explained by the dielectric theory. Notably, zeolites containing 8-membered ring (8MR) showed extra-high Cs+ selectivity. Structural analysis using X-ray diffraction proved that Cs+ with an ionic diameter of 3.6 angstrom was selectively coordinated within 8MR having a cavity diameter of 3.6-4.1 angstrom. Such unique size-selective Cs+ coordination is analogous to ion complexation by macrocyclic organic ligands (e.g., crown ethers). Divalent Sr2+ showed decreasing affinity to zeolites as the Si/Al ratio increased, because of the increasing average Al-Al distance distribution. Sr2+ exchange exhibited an insignificant dependence on zeolite structures due to its strong hydration, which inhibited close interaction with zeolite frameworks. In terms of kinetics, Sr2+ exchange was significantly slower than Cs+ exchange because of the bulkiness of hydrated Sr2+ ions. Therefore, the micropore channels with large apertures (e.g., 12-membered ring) were beneficial for achieving fast ion-exchange kinetics, especially in the case of Sr2+.
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