Powell Brian A, Fjeld Robert A, Kaplan Daniel I, Coates John T, Serkiz Steven M
Department of Environmental Engineering and Science, Clemson University, Anderson, South Carolina 29625, USA.
Environ Sci Technol. 2004 Nov 15;38(22):6016-24. doi: 10.1021/es049386u.
Changes in aqueous- and solid-phase Pu oxidation state were monitored over time in magnetite (Fe3O4) suspensions containing 239Pu(V)-amended 0.01 M NaCl. Oxidation state distribution was determined by leaching of Pu into an aqueous phase followed by an ultrafiltration/solvent extraction technique. The capability of the technique to measure Pu oxidation state distribution was verified using 230Th(IV), 237Np(V), and 233U(VI) as oxidation state analogues. Reduction of Pu(V) was observed at all pH values (pH 3 to 8) and magnetite concentrations (10 to 100 m2 L(-1)). In the pH range 5 to 8, adsorption was a rate-limiting step, and reduction was mediated by the solid phase; at pH 3 reduction occurred in the aqueous phase. The overall reaction (describing both adsorption and reduction of Pu(V)) was found to be approximately first order with respect to the magnetite concentration and of order -0.34+/-0.02 with respect to the hydrogen ion concentration. Assuming first order dependence with respect to Pu, the overall reaction rate constant was calculated as k(rxn) = 4.79+/-0.62 x 10(-8) (m(-2) L)0.99(mol(-1) L)-0.34(s(-1)). The Pu(IV) solid-phase species became more stable over time.
在含有经239Pu(V)修正的0.01 M氯化钠的磁铁矿(Fe3O4)悬浮液中,随时间监测水相和固相钚氧化态的变化。通过将钚浸出到水相中,然后采用超滤/溶剂萃取技术来确定氧化态分布。使用230Th(IV)、237Np(V)和233U(VI)作为氧化态类似物,验证了该技术测量钚氧化态分布的能力。在所有pH值(pH 3至8)和磁铁矿浓度(10至100 m2 L(-1))下均观察到Pu(V)的还原。在pH值5至8范围内,吸附是限速步骤,还原由固相介导;在pH 3时,还原发生在水相中。发现总体反应(描述Pu(V)的吸附和还原)相对于磁铁矿浓度近似为一级反应,相对于氢离子浓度为-0.34±0.02级反应。假设相对于钚为一级依赖性,计算出总体反应速率常数为k(rxn) = 4.79±0.62×10(-8) (m(-2) L)0.99(mol(-1) L)-0.34(s(-1))。随着时间的推移,Pu(IV)固相物种变得更加稳定。