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Rudin, Stefan; Klinkenberg, Martina; Kowalski, Piotr M.; Bornhake, Thomas; Bosbach, Dirk
18th International Conference on Chemistry and Migration Behaviour of Actinides and Fission Products in the Geosphere: Migration 2023. Book of abstracts2023
18th International Conference on Chemistry and Migration Behaviour of Actinides and Fission Products in the Geosphere: Migration 2023. Book of abstracts2023
AbstractAbstract
[en] The first aim of this study was to determine the role of the structurally different kink sites at these steps for the crystal growth kinetics by computing the activation energies of the Ba2+, Ra2+ and SO42- ion attachment processes. Here, we have combined several advanced methods of computational quantum mechanics to optimize accuracy and efficiency of the simulations: a hybrid Density Functional Theory (DFT) and Soft-sphere Continuum Solvation (SSCS) approach for computation of barite-aqueous phase interface, and a Nudged Elastic Band (NEB) approach for calculation of activation energies. A barite (001) surface structure was constructed, including steps and all relevant attachment positions for kink-site nucleation, and verified by comparison with experimental data. Our simulations show that Ba2+ attachment to the [120] steps of the (001) surface is a complicated multistep process, involving several water detachment-steps and the formation of outer, inner sphere and bidentate complexes with the barite surface. Two mechanisms mainly determine the shape of the energy path, the creation of bonds and the dehydration of the attaching ion. Energy differences between ion attachment processes at different sites are predominantly caused by the influence of the different [120] steps. The rate-limiting steps for Ba2+ attachment were the formation of the first bond to the barite surface and complete uptake. The Ba2+ ion completely attached to the barite surface is the configuration with the lowest energy, and the Ba2+ ion completely dissolved is the minimum energy configuration with the highest energy. The energy pathway derived from this study can explain the barite growth exclusively by the driving forces of surface processes, which are also postulated to be responsible for the anisotropic barite (001) surface growth. This is not the case with the classical force-field-based approach of Stack et al. 2012, which shows the same basic minimum energy structures but with different relative energies and the inner sphere complex as the configuration with the lowest energy. The DFT-NEB-SSCS approach also provides more detailed energy paths that allow for an in-depth comparison of the different ion attachment processes at a certain site. On-going simulations for the uptake of 226Ra into the (001) barite surface indicate distinct differences between Ra2+ and Ba2+, related to the different water coordination numbers, and slight variations within the attachment path. Ra2+ could therefore be kinetically favored during recrystallization due to an easier dehydration compared to Ba2+ at the barite (001) surface
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Grambow, B.; Abdelouas, A.; Landesman, C.; Montavon, G.; Suzuki-Muresan, T.; Pierret, T.; Ollitrault, I.; Decatoire, M. (Subatech, Nantes (France)); Plas, F. (ANDRA (France)); Savoye, S. (DES/ISAS/DRMP/SPC/L3MR, CEA Centre Paris-Saclay 91191 Gif-sur-Yvette (France)); Claret, F. (BRGM, Orleans, (France)); Wittebroodt, Ch. (IRSN, Fontenay-aux-Roses (France)); Subatech, Nantes (France); ANDRA (France); CEA Centre Paris-Saclay (France); BRGM, Orleans, (France); IRSN, (France); 520 p; Sep 2023; p. 95-96; Migration 2023: 18. International Conference on Chemistry and Migration Behaviour of Actinides and Fission Products in the Geosphere; Nantes (France); 24-29 Sep 2023; 9 refs. ; Available from the INIS Liaison Officer for France, see the INIS website for current contact and E-mail addresses
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ALKALINE EARTH ISOTOPES, ALPHA DECAY RADIOISOTOPES, CALCULATION METHODS, CARBON 14 DECAY RADIOISOTOPES, CHARGED PARTICLES, DISPERSIONS, ENERGY, EVEN-EVEN NUCLEI, HEAVY ION DECAY RADIOISOTOPES, HEAVY NUCLEI, HOMOGENEOUS MIXTURES, IONS, ISOTOPES, MECHANICS, MINERALS, MIXTURES, NUCLEI, OXYGEN COMPOUNDS, RADIOISOTOPES, RADIUM ISOTOPES, SIMULATION, SOLUTIONS, SULFATE MINERALS, SULFUR COMPOUNDS, VARIATIONAL METHODS, YEARS LIVING RADIOISOTOPES
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