Paul
Estevenon
abcd,
Thomas
Dumas
*a,
Pier Lorenzo
Solari
e,
Eleonore
Welcomme
a,
Stephanie
Szenknect
b,
Adel
Mesbah
b,
Kristina O.
Kvashnina
cd,
Philippe
Moisy
a,
Christophe
Poinssot
a and
Nicolas
Dacheux
*b
aCEA, DES, ISEC, DMRC, Univ Montpellier, Marcoule, France. E-mail: thomas.dumas@cea.fr; Tel: +33 4 66 33 92 05
bICSM, Univ Montpellier, CNRS, CEA, ENSCM, Bagnols-sur-Cèze, France. E-mail: nicolas.dacheux@umontpellier.fr
cThe Rossendorf Beamline at the ESRF, CS40220, 38043 Grenoble Cedex 9, France
dHelmholtz Zentrum Dresden-Rossendorf (HZDR), Institute of Resource Ecology, P.O. Box 510119, 01314, Dresden, Germany
eSynchrotron Soleil, L'Orme des Merisiers, Saint-Aubin, BP 48, F-91192 Gif-sur-Yvette Cedex, France
First published on 6th April 2022
Correction for ‘Formation of plutonium(IV) silicate species in very alkaline reactive media’ by Paul Estevenon et al., Dalton Trans., 2021, 50, 12528–12536, DOI: 10.1039/D1DT02248B.
Ref. | Actinide-silicate system | Conditions | pH | Colloid size | |
---|---|---|---|---|---|
Below MWSA | Above MWSA | ||||
MWSA: mononuclear wall of silicic acid. | |||||
Observation in carbonate ion rich reactive media | |||||
2 | Th-Silicate | [NaHCO3] = 0.05 mol L−1 | ≥7 | 7–20 nm | |
[Th] = 10−3 mol L−1 | |||||
Si/Th = 0.3–8 | |||||
3 and 23 | U-Silicate | [NaHCO3] = 0.05 mol L−1 | 7–9.5 | ≤20 nm | |
[U] = 10−3 mol L−1 | |||||
Si/U = 0.25–3 | |||||
24 | U-Silicate | [NaHCO3] = 0.05 mol L−1 | 9–10.5 | ≤220 nm | 1–10 nm |
[U] = 10−3 mol L−1 | |||||
Si/U = 2–4 | |||||
4 and 25 | Np-Silicate | [NaHCO3] = 0.1 mol L−1 | 7–9 | ≤250 nm | 5 nm |
[Np] = 10−3 mol L−1 | |||||
Si/Np = 0.7–8.6 | |||||
Observation in carbonate ion free reactive media | |||||
20 | Th-Silicate | ThO2·xH2O | 6–12 | Th solubility increase | |
[Si] = 10−3–0.15 mol L−1 | |||||
18 | Th-Silicate | ThO2·xH2O | 10–13.3 | Th solubility increase | |
[Si] = 1.8 × 10−2 mol L−1 | |||||
15 | Pu-Silicate | PuO2·xH2O | 11–13.8 | Pu solubility increase | |
[Si] = 10−3–10−2 mol L−1 |
This mistake also led to a misinterpretation of the literature data reported in this table in the discussion. Indeed, the sentence beginning on line 25 of page 12529 (at the start of the penultimate paragraph of the Introduction section) is incorrect; the corrected text is:
“These colloids correspond to 1–20 nm particles at high silicate ion concentrations (above silicic acid mononuclear wall; [Si] = 2 × 10−3 mol L−1 (ref. 26)) and ≤200 nm agglomerates at lower concentrations”.
The sentence beginning on line 54 of page 12531 (in the third paragraph of the Results and discussion section) is also incorrect; the corrected text is:
“It is worth noting that no evidence of particle agglomeration was observed; that result is consistent with the results obtained for the other actinide silicate colloids above the silicic acid mononuclear wall.4,24,25”
These errors do not affect the overall conclusions of the paper.
The authors would like to apologize for these errors and any consequent inconvenience caused.
The Royal Society of Chemistry apologises for these errors and any consequent inconvenience to authors and readers.
This journal is © The Royal Society of Chemistry 2022 |