journal article·2017-09

Formation of zeolites in metakaolin-based geopolymers and their potential application for Cs immobilization

M. Arbel Haddad, E. Ofer-Rozovsky, G. Bar-Nes, E.J.C. Borojovich, A. Nikolski, D. Mogiliansky, A. Katz

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Abstract

Abstract Alkali-activated aluminisilicate materials, also known as geopolymers, have been considered as attractive candidates for nuclear waste immobilization, due to their ability to incorporate cations, combined with high chemical resistance and suitable mechanical and thermal properties. The goal of the present research was to study the incorporation and immobilization of Cs in low-Si geopolymers (SiO2:Al2O3 molar ratio ≤ 2) which are known to have a relatively high crystalline phase content. A series of low-Si geopolymers was prepared from metakaolin using activating solutions containing CsOH and NaOH at different proportions. The structural evolution of the resulting products was followed using X-ray diffraction, the incorporation of Cs in the geopolymer was followed by pore water analysis, and its immobilization efficiency was determined from leaching tests following the ANSI/ANS-16.1 standard procedure. Like low-Si NaOH-based geopolymers, the mixed CsOH-NaOH geopolymers contain a significant amount of crystalline material which is imbedded within an amorphous matrix. Formulations with 1%Cs yielded the crystalline phases zeolite A and zeolite X. At 50%Cs the Cs-bearing zeolite F was formed. All three phases were observed at an intermediate Cs content (7%Cs). Pore water analysis indicated a preference for Cs uptake from the activating solution, while leaching experiments indicated selectivity for Cs immobilization in the mixed CsOH-NaOH geopolymers. Correlation of the apparent diffusion constants for both Na and Cs, as obtained from the leaching experiments, with the structural data lead to the conclusion that Cs is more efficiently bound by zeolite F, whereas Na binding is preferred by zeolites A and X. Nevertheless, the leachability indices for both Cs and Na were well above 6, indicating that such matrices may be considered as waste forms for 137Cs.
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OpenAlex topics: Nuclear materials and radiation effects · Concrete and Cement Materials Research · Chemical Synthesis and Characterization

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References (39)

Show source-provided references
1. Immobilization of intermediate-level wastes in geopolymers10.1016/0022-3115(94)90364-6 ↗
2. Aqueous leachability of metakaolin-based geopolymers with molar ratios of Si/Al = 1.5-410.1016/j.jnucmat.2008.06.015 ↗
3. Transmission electron microscopy and nuclear magnetic resonance studies of geopolymers for radioactive waste immobilization10.1111/j.1551-2916.2007.01532.x ↗
4. Geopolymeric agent for immobilization of radioactive ashes after biomass burning10.1023/A:1023845628670 ↗
5. Immobilization of simulated radionuclide 133Cs+ by fly ash-based geopolymer10.1016/j.jhazmat.2013.08.049 ↗
6. Immobilization of cesium in alkaline activated fly ash matrix10.1016/j.jnucmat.2005.06.006 ↗
7. Caesium immobilisation in hydrated calcium-silicate-aluminate systems10.1016/S0008-8846(98)00163-X ↗
8. Instrinsic sorption potential of cement components for 134Cs10.1016/0008-8846(84)90137-6 ↗
9. The mechanism of cesium immobilization in densified silica-fume blended cement pastes10.1016/j.cemconres.2007.09.017 ↗
10. Ojovan · 2014
11. IAEA-TECDOC-1701 · 2013
12. Atomic structure of a cesium aluminosilicate geopolymer: a pair distribution function study10.1021/cm703369s ↗
13. Formation of ceramics from metakaolin-based geopolymers. Part II: K-based geopolymer10.1111/j.1551-2916.2008.02922.x ↗
14. Preparation and properties of hydroceramic waste forms made with simulated hanford low-activity waste10.1111/j.1551-2916.2005.00775.x ↗
15. Formulation of caesium based and caesium containing geopolymers10.1179/174367609X422072 ↗
16. XRD analysis of the role of cesium in sodium-based geopolymer10.1111/jace.13399 ↗
17. What happens to 5 Year old metakaolin geopolymers' the effect of alkali cation
18. Preparation and X-ray characterization of pollucite ( CsA1Si206 )
19. Crystal chemistry and phase transitions in substituted pollucites along the CsAlSi2O6-CsTiSi2O6.5 join: a powder synchrotron X-ray diffractometry study10.1111/j.1151-2916.2002.tb00251.x ↗
20. Cation exchange behaviour of synthetic cesium aluminosilicates10.1016/0020-1650(78)80103-2 ↗
21. Do geopolymers actually contain nanocrystalline zeolites? a reexamination of existing results10.1021/cm050230i ↗
22. The formation of crystalline phases in metakaolin-based geopolymers in the presence of sodium nitrate10.1007/s10853-016-9767-0 ↗
23. Kraus · 2000
24. Modeling the silica glass structure by the Rietveld method10.1016/0022-3093(94)00664-4 ↗
25. Pearson’s Crystal Data: Crystal Structure Database for Inorganic Compounds (on CD-ROM), Release 2011/12, (n.d.).
26. Expression and analysis of pore fluids from hardened pastes and mortars10.1016/0008-8846(81)90069-7 ↗
27. ANS/ANSI-16.1 Standard · 1986
28. On zeolite K-F and its rubidium and cesium analogs
29. The crystal structure of the synthetic zeolite10.1524/zkri-1974-1-203 ↗
30. Cation exchange in the synthetic zeolite K-F10.1039/j19710002914 ↗
31. Reactive transport numerical model for durability of geopolymer materials10.4236/aces.2016.64036 ↗
32. NRC · 1991
33. Siskind · 1991
34. Ion exchange equilibria in zeolite minerals10.1007/BF00196136 ↗
35. Self-diffusion of sodium and cesium ions in hydrous titanium oxide10.1016/0167-2738(94)90048-5 ↗
36. Self-diffusion and ionic transport of sodium and cesium ions in particles of hydrous zirconia10.1016/0167-2738(92)90167-N ↗
37. Alkali metal ion exchange selectivity of Al-substituted tobermorite10.1557/JMR.1989.0698 ↗
38. Hydrated metal ions in aqueous solution: how regular are their structures?10.1351/PAC-CON-09-10-22 ↗
39. Pore solution composition and alkali diffusion in inorganic polymer cement10.1016/j.cemconres.2010.04.008 ↗