Reversibility in radionuclide/bentonite bulk and colloidal ternary systems

  • Sherriff N
  • Issa R
  • Morris K
  • et al.
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Abstract

Ternary systems of 152 Eu(III), bulk bentonite and ethylenediaminetetraacetic acid (EDTA) ([Eu] = 7.9 × 10 –10 M; pH = 6.0–7.0) have been studied. Without EDTA, there was slow uptake in a two-stage process, with initial rapid sorption of Eu(III) (96%), followed by slower uptake of a much smaller fraction (3.0% over a period of one month). The reversibility of Eu(III) binding was tested by allowing Eu(III) to sorb to bentonite for 1–322 days. EDTA was added to the pre-equilibrated Eu bentonite systems at 0.01 M, a concentration that was sufficient to suppress sorption in a system where EDTA was present prior to the contact of Eu(III) with bentonite. A fraction of the Eu was released instantaneously (30–50%), but a significant amount remained bound. With time, the amount of Eu(III) retained by the bentonite reduced, with a slow fraction dissociation rate constant of approximately 4.3 × 10 –8 s –1 (values in the range 2.2 × 10 –8 – 1.0 × 10 –7 s –1 ) for pre-equilibration times ≥7 days. Eventually, the amount of Eu(III) remaining bound to the bentonite was within error of that when EDTA was present prior to contact (4.5% ± 0.6), although in systems with pre-equilibration times >100 days, full release took up to 500 days. Europium interactions with colloidal bentonite were also studied, and the dissociation rate constant measured by a resin competition method. For the colloids, more Eu was found in the slowly dissociating fraction (60–70%), but the first-order dissociation rate constant was faster, with an average rate constant of 8.8 × 10 –7 s –1 and a range of 7.7 × 10 –7 –9.5 × 10 –7 s –1 . For both bulk and colloidal bentonite, although slow dissociation was observed for Eu(III), there was no convincing evidence for 'irreversible' binding.

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APA

Sherriff, N., Issa, R., Morris, K., Livens, F., Heath, S., & Bryan, N. (2015). Reversibility in radionuclide/bentonite bulk and colloidal ternary systems. Mineralogical Magazine, 79(6), 1307–1315. https://doi.org/10.1180/minmag.2015.079.06

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