The calcium complexation and acid-base properties of α-d-isosaccharinate (Isa) in neutral and in (hyper)alkaline solutions have been investigated via potentiometric titrations, multinuclear NMR, ESI-MS and quantum chemical calculations. Isa is the primary alkaline degradation product of cellulose, and may be present in radioactive waste repositories and therefore, it could contribute to the mobilization of radioactive nuclei. Because of its limited availability, d-gluconate (Gluc) is commonly used as a structural and functional model of Isa. Therefore, the thermodynamic and structural data obtained for Isa were compared with those of Gluc. The formation constants of the CaIsa and CaGluc complexes present in neutral solutions are practically identical, but the binding sites are in different positions and the CaIsa solution species cannot be detected. The stepwise formation constant of the CaIsaH complex (forming in alkaline medium) is somewhat larger than that of CaGlucH, which is in line with the observation that IsaH is a stronger base than GlucH. The most striking difference is that, unlike Gluc, Isa does not form polynuclear complexes with Ca. The structural reason for this is that the alcoholate groups on C2 and C3 adjacent to the carboxylate moiety on Gluc are able to simultaneously bind Ca, making the formation of polynuclear Ca-complexes possible. On Isa, only the alcoholate on C2 is involved, while the other one on C6 is not (supposedly for steric reasons). In conclusion, during the interactions of Gluc and Isa with Ca, differences rather than similarities prevail.
AbstractCertain complexing agents (such as D-gluconate, D-isosaccharinate, etc.) as well as actinides and lanthanides are simultaneously present in cementitious radioactive waste repositories and (in the presence of water) are capable of forming complex compounds. Such processes may immobilize radionuclides and are of importance in the thermodynamic modelling of the aqueous chemistry of waste repositories. Nd(III) is considered to be a suitable model for trivalent lanthanides and actinides, due to the similarity of their ionic radii. In the current work, solid complexes isolated from aqueous solution containing Nd(III), Ca(II) and D-gluconate (Gluc−) were investigated. In an aqueous solution containing Nd(III) and Gluc−, the formation of a precipitate was observed at pH ≥ 8. This precipitate was found to redissolve around pH ~ 11, but reprecipitated when Ca(II) ions were added to the solution. In order to gain an insight in binary and ternary aqueous systems, in the present work we report the structure of these solid complexes obtained from XRD, FT-IR, Raman, SEM-EDAX and UV-DRS measurements. The structure of these solids, where possible, was compared with those identified in solution. The compositions of these complexes are suggested to be NdGlucH−1(OH) · 2H2O and CaNdGlucH−1(OH)3 · 2H2O, respectively. In these, the chemical environment of the Nd(III) was found to be the same as that in the NdGlucH−1(OH)0(aq) solution species.
The complexation equilibria between
Mg2+ and d-gluconate (Gluc–)
ions are of particular importance in modeling the chemical speciation
in low- and intermediate-level radioactive waste repositories. NMR
measurements and potentiometric titrations conducted at 25 °C
and 4 M ionic strength revealed the formation of the MgGluc+, MgGlucOH0, MgGluc(OH)2–, and Mg3Gluc2(OH)40 complexes.
The trinuclear species provides indirect evidence for the existence
of multinuclear magnesium(II) hydroxido complexes, whose formation
was proposed earlier but has not been confirmed yet. Additionally,
speciation calculations demonstrated that MgCl2 can markedly
decrease the solubility of thorium(IV) at low ligand concentrations.
Regarding the structure of MgGluc+, both IR spectra and
density functional theory (DFT) calculations indicate the monodentate
coordination of Gluc–. By the potentiometric data,
the acidity of the water molecules is higher in the MgGluc+ and MgGlucOH0 species than in the Mg(H2O)62+ aqua ion. On the basis of DFT calculations,
this ligand-promoted hydrolysis is caused by strong hydrogen bonds
forming between Gluc– and Mg(H2O)62+. Conversely, metal-ion-induced ligand deprotonation
takes place in the case of calcium(II) complexes, giving rise to salient
variations on the NMR spectra in a strongly alkaline medium.
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