Fluoride complexation of rutherfordium (Rf, element 104)
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E. Strub
The fluoride complexation of the group-4 elements Zr, Hf and Rf, and of the pseudo-homolog Th, has been investigated in mixed HNO3/HF solutions by studying Kd values on both cation exchange resins (CIX) and anion exchange resins (AIX) using the automated rapid chemistry apparatus ARCA. On the CIX, the four elements are strongly retained as cations below 10-3 M HF. For Zr and Hf, the decrease of the Kd values due to the formation of fluoride complexes occurs between 10-3 M HF and 10-2 M HF. For Rf and Th, this decrease is observed at one order of magnitude higher HF concentrations. On the AIX, for Zr and Hf, a rise of the Kd values due to the formation of anionic fluoride complexes is observed between 10-3 M HF and 10-2 M HF, i.e. in the same range of HF concentrations where the decrease of the Kd values on the CIX is observed, yielding a consistent picture. For Rf and Th, on the AIX, no rise of the Kd values is observed even if the HF concentration is increased up to 1 M. By varying the concentration of the counter ion NO3- which is competing for the binding sites on the AIX resin, it could be shown, nevertheless, that Rf does form anionic fluoride complexes. Apparently, there is a more specific competition of NO3- with respect to [RfFx](x-4)- than with [ZrFy](y-4)- and [HfFz](z-4)-.
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Articles in the same Issue
- Investigation of 50Cr(d,n)51Mn and natCr(p,x)51Mn processes with respect to the production of the positron emitter 51Mn
- Fluoride complexation of rutherfordium (Rf, element 104)
- Continuous on-line chromatography of short lived isotopes of tungsten as homolog of seaborgium (element 106)
- Cation-cation complexes of PuO2+ and NpO2+ with Th4+ and UO22+
- The influence of dibutylphosphate on actinide extraction by 30% tributylphosphate
- Synthesis and spectroscopic properties of neptunium VI and plutonium VI oxoanion compounds
- Thermodynamic model for the solubility of thorium dioxide in the Na+-Cl--OH--H2O system at 23°C and 90°C
- Uranium and thorium isotopes in some red sea sediments