The Influence of pH, Ionic Strength and Temperature on Cs, Ba, Co, and Eu Sorption on Biotite - Experiments and Modelling
- 1. Department of Chemistry and Chemical Engineering, Division of Nuclear Chemistry Chalmers University of Technology, Kemivaegen 4, SE-41296 Goeteborg, (Sweden)
Description
The sorption behavior of 134Cs, 133Ba, 60Co and 152Eu, in a mixture, at tracer concentration [10-8 M] on crushed Na-converted biotite (particle size 0.25-0.5 mm) was investigated by the batch sorption experiment with S:L ratio of 1:50 under the inert gas conditions ([O2] <1 ppm) for up to two months. The experiment was carried out in triplicate with pH adjusted to 5, 6, 7, 8 or 9 with buffered solutions of 0.001, 0.01 and 0.1 M NaClO_4 at 40 and 60 C. Titration experiments on the biotite surface were conducted over a pH range of around 3 to 11 at 40 and 60 C respectively. The results were modelled to obtain pKa,1 = -7.10 ±0.05 at 40 C and -6.93 ±0.32 at 60 C, pKa,2 = -4.90 ±0.32 at 40 C, and -5.00 ±0.13 at 60 C using PHREEQC chemical speciation calculations coupled with an error minimization routine. Sorption results for the pH-range 5-9 show that for Cs, Ba, Co, and Eu, at 40 C and I= 0.001 M the Rd values were 0.6-2.3, 0.2-3.8, 0.01-4.0 and 2.4-11.3 m3/kg respectively. Corresponding results for 40 C and I= 0.01 M were Rd = 0.2-0.8, 0.03-5.1, 0.01-10.9 and 0.2-22.3 m3/kg and for 40 C and I= 0.1 M, were Rd = 0.05-0.2, 0.02-0.4, 0.01-8.61 and 2.7-13.63 m3/kg. For 60 C and I= 0.001 M the Rd values for Cs, Ba, Co, and Eu were 0.7-7.8, 0.3-4.4, 0.03-5.77 and 3.1-18.3 m3/kg respectively. Corresponding results for 60 C and I= 0.01 M were Rd = 0.2-3.2, 0.02-8.1, 0.01-19.3 and 0.2-22.9 m3/kg and for 60 C and I= 0.1 M Rd = 0.1-0.9, 0.1-0.8, 0.01-18.0 and 5.3-30.0 m3/kg. The sorption of all four elements is dependent on pH, ionic strength, and temperature. A computer code was developed that coupled PHREEQC geochemical modeling software with Python programming language to fit the sorption experimental data with the compensation for biotite dissolution. Sorption of all metals was successfully modelled with a combination of one amphoteric (i.e. 2-pKa) surface complexation site and one ion exchange site. The model was fitted to the data without any compensation for electrostatic effects. The modeling result shows that the Cs sorption is primarily governed by two surface species: SOCs, a surface complex, and CsX, an ion exchange species. However, in the case of Ba, two surface complexes: SOBa+ and SOBaOH and one ion-exchange species, BaX2, mainly contribute to sorption. The Co sorption data was fitted by considering three-surface complexes: SOCo+, SOCoOH, and SOCo(OH)2- but no ion exchange is involved. The model predicts that Eu is sorbed as three different surface complexes: SOEu2+, SOEuOH+, and SOEu(OH)2, and in addition, also one ion-exchange species EuX3
Files
Additional details
Publishing Information
- Imprint Title
- ATALANTE 2024: book of abstracts
- Imprint Pagination
- 248 p.
- Journal Page Range
- p. 175
- Report number
- INIS-FR--25-0422
Conference
- Title
- 6. International ATALANTE Conference on Nuclear Chemistry for Sustainable Fuel Cycles
- Dates
- 1-6 Sep 2024
- Place
- Avignon (France)
INIS
- Country of Publication
- France
- Country of Input or Organization
- France
- Subject category
- S12: MANAGEMENT OF RADIOACTIVE WASTES, AND NON-RADIOACTIVE WASTES FROM NUCLEAR FACILITIES;
- Resource subtype / Literary indicator
- Conference
- Descriptors DEI
- PH VALUE; TEMPERATURE DEPENDENCE; SORPTION; BIOTITE; CESIUM 134; BARIUM 133; COBALT 60; EUROPIUM 152; CHEMICAL STATE; COMPUTERIZED SIMULATION
- Descriptors DEC
- ALKALINE EARTH ISOTOPES; BARIUM ISOTOPES; BETA DECAY RADIOISOTOPES; BETA-MINUS DECAY RADIOISOTOPES; BETA-PLUS DECAY RADIOISOTOPES; CESIUM ISOTOPES; COBALT ISOTOPES; DAYS LIVING RADIOISOTOPES; ELECTRON CAPTURE RADIOISOTOPES; EUROPIUM ISOTOPES; EVEN-ODD NUCLEI; HOURS LIVING RADIOISOTOPES; INTERMEDIATE MASS NUCLEI; INTERNAL CONVERSION RADIOISOTOPES; ISOMERIC TRANSITION ISOTOPES; ISOTOPES; MICA; MINERALS; MINUTES LIVING RADIOISOTOPES; NUCLEI; ODD-ODD NUCLEI; RADIOISOTOPES; RARE EARTH NUCLEI; SILICATE MINERALS; SIMULATION; YEARS LIVING RADIOISOTOPES