This research addresses
a subject discussed controversially for
almost 70 years. The interactions between the uranyl(VI) ion, U(VI),
and citric acid, H3Cit, were examined using a multi-method
approach comprising nuclear magnetic resonance (NMR), ultraviolet–visible
(UV–vis), attenuated total reflectance Fourier-transform infrared
(ATR FT-IR), and extended X-ray absorption fine-structure (EXAFS)
spectroscopies as well as density functional theory (DFT) calculations.
Combining 17O NMR spectroscopy and DFT calculation provided
an unambiguous decision on complex configurations, evidencing for
the first time that the dimeric complex, (UO2)2(HCit–H)2
2–, exists
as two diastereomers with the syn-isomer in aqueous
solution strongly favored over the anti-isomer. Both
isomers interconvert mutually with exchange rates of ∼30 s–1 at −6 °C and ∼249 s–1 at 60 °C in acidic solution corresponding to an activation
barrier of about 24 kJ mol–1. Upon increasing the
pH value, ternary dimeric mono- and bis-hydroxo as well as trimeric
complexes form, that is, (UO2)2(HCit–H)2(OH)3–, (UO2)2(HCit–H)2(OH)2
4–, (UO2)3(O)(Cit–H)3
8–, and (UO2)3(O)(OH)(Cit–H)2
5–, respectively. Stability
constants were determined for all dimeric and trimeric species, with
log β° = −(8.6 ± 0.2) for the 3:3 species being
unprecedented. Additionally, in the 6:6 sandwich complex, formed from
two units of 3:3 species, the 17O NMR resonance of the
trinuclear uranyl(VI) core bridging μ3-O is shown
for the first time. Species distribution calculations suggest that
the characterized polynuclear U(VI)–citrate species do not
significantly increase uranium(VI) mobility in the environment. Furthermore,
we revise the misconceptions in the aqueous U(VI)–citric acid
solution chemistry, that is, structures proposed and repeatedly taken
up, and outline generalized isostructural considerations to provide
a basis for future U(VI) complexation studies.