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Actinide Sorption Studies Using the Isotopes 237Np and 239Np

The sorption of Np(V) on γ-Al2O3 and the reference clay mineral kaolinite was studied in batch experiments in the presence and absence of ambient CO2 with 0.1 M NaClO4 as background electrolyte. The short-lived isotope 239Np (t1/2 = 2.36 d) was used instead of 237Np (t1/2 = 2.14 × 106 a) to study the sorption behaviour of Np(V) at environmentally-relevant concentrations, i.e., 7 pM Np. In addition, 239Np served as tracer to measure sorption isotherms over six orders of magnitude in neptunium concentration. γ-Al2O3 served as a reference for clay minerals like kaolinite to investigate the interaction of Np(V) with aluminol groups, which are crucial binding sites of clays.