Influence of sources on plutonium mobility and oxidation state transformations in vadose zone sediments.
Well-defined solid sources of Pu(III) (PuCl3), Pu(IV) (Pu (NO3)4 and Pu (C2O4)2), and Pu(VI) (Pu02(NO3)2) were placed in lysimeters containing vadose zone sediments and exposed to natural weather conditions for 2 or 11 years. The objective of this study was to measure the release rate of Pu and the changes in the Pu oxidation states from these Pu sources with the intent to develop a reactive transport model source-term. Pu(III) and Pu(IV) sources had identical Pu concentration depth profiles and similar Pu release rates. Source release data indicate that PuIV(C2O4)2 was the least mobile, whereas Pu(VI)O2(NO3)2 was the most mobile. Synchrotron X-ray fluorescence (SXRF) revealed that Pu was very unevenly distributed on the sediment and Mn concentrations were too low (630 mg kg(-1)) and perhaps of the wrong mineralogy to influence Pu distribution. The high stability of sorbed Pu(IV) is proposed to be due to the formation of a stable hydrolyzed Pu(IV) surface species. Plutonium X-ray absorption near-edge spectroscopy (XANES) analysis conducted on sediment recovered at the end of the studyfrom the Pu(IV)(NO3)4- and Pu(III)(III)Cl3-amended lysimeters contained essentially identical Pu distributions: approximately 37% Pu(III), 67% Pu(IV), 0% Pu(V), and 0% Pu(VI). These results were similar to those using a wet chemistry Pu oxidation state assay, except the latter method did not detect any Pu(III) present on the sediment but instead indicated that 93-98% of the Pu existed as Pu(IV). This discrepancy was likely attributable to incomplete extraction of sediment Pu(III) by the wet chemistry method. Although Pu has been known to exist in the +3 oxidation state under microbially induced reducing conditions for decades, to our knowledge, this is the first observation of steady-state Pu(III) in association with natural sediments. On the basis of thermodynamic considerations, Pu(III) has a wide potential distribution, especially in acidic environments, and as such may warrant further investigation.
Kaplan
Daniel I
DI
Savannah River National Laboratory, Aiken, South Carolina 29808, USA. daniel.kaplan@srs.gov
Powell
Brian A
BA
Duff
Martine C
MC
Demirkanli
Deniz I
DI
Denham
Miles
M
Fjeld
Robert A
RA
Molz
Fred J
FJ
D005453:Fluorescence; D019015:Geologic Sediments / Q000032:analysis* / Q000737:chemistry; D010084:Oxidation-Reduction; D011005:Plutonium / Q000032:analysis* / Q000737:chemistry; D013057:Spectrum Analysis; D014875:Water Pollutants, Radioactive / Q000032:analysis* / Q000737:chemistry; D014881:Water Supply; D014965:X-Rays
D014875:Water Pollutants, Radioactive; D011005:Plutonium