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AbstractAbstract
[en] Fluorescence spectroscopy was used to study the Ca2+/UO22+/CO32- solution system at different ionic strengths. Fluorescent titrations confirmed formation of Ca2UO2(CO3)3 complex for which the values of log β213 were measured at 0.1, 0.3, 0.7, 1.0 and 3.0 m (NaClO4) at pcH = 8.1. Specific interaction theory (SIT) was used to correlate the log β213 values as a function of ionic strength. The value obtained for log β2130(I = 0) wsas 29.8 ± 0.7, indicating that Ca2UO2(CO3)3 was the predominant specie at the pH 8 in calcium rich, oxic waters. (orig.)
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ACTINIDE COMPLEXES, ACTINIDE NUCLEI, ALKALINE EARTH ISOTOPES, ALKALINE EARTH METAL COMPOUNDS, ALPHA DECAY RADIOISOTOPES, BETA DECAY RADIOISOTOPES, BETA-MINUS DECAY RADIOISOTOPES, CALCIUM COMPOUNDS, CALCIUM ISOTOPES, CARBON COMPOUNDS, CARBONATES, CHEMICAL ANALYSIS, COMPLEXES, DAYS LIVING RADIOISOTOPES, EMISSION SPECTROSCOPY, EVEN-ODD NUCLEI, HEAVY ION DECAY RADIOISOTOPES, HEAVY NUCLEI, INTERMEDIATE MASS NUCLEI, ISOTOPES, KINETICS, NEON 24 DECAY RADIOISOTOPES, NUCLEI, OXYGEN COMPOUNDS, QUANTITATIVE CHEMICAL ANALYSIS, RADIOISOTOPES, REACTION KINETICS, SPECTROSCOPY, SPONTANEOUS FISSION RADIOISOTOPES, URANIUM COMPLEXES, URANIUM ISOTOPES, VOLUMETRIC ANALYSIS, YEARS LIVING RADIOISOTOPES
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