Pacific Northwest National Laboratory, 902 Battelle Blvd, Richland, WA, 99354, USA.
Pacific Northwest National Laboratory, 902 Battelle Blvd, Richland, WA, 99354, USA.
J Environ Radioact. 2020 May;216:106182. doi: 10.1016/j.jenvrad.2020.106182. Epub 2020 Feb 4.
The use of an aqueous reductant (Na-dithionite) with pH buffer (K-carbonate, pH 12) was evaluated in this laboratory study as a potential remedial approach for removing Fe oxide associated iodine and enhancing pump-and-treat extraction from iodine-contaminated sediments in the unconfined aquifer in the 200 West Area of the Hanford Site. X-ray fluorescence data of untreated sediment indicated that iodine was largely associated with Fe (i.e., potentially incorporated into Fe oxides), but XANES data was inconclusive as to valence state. During groundwater leaching, aqueous and adsorbed iodine was quickly released, then additional iodine was slowly released potentially from slow dissolution of one or more surface phases. The Na-dithionite treatment removed greater iodine mass (2.9x) at a faster rate (1-4 orders of magnitude) compared to leaching with groundwater alone. Iron extractions for untreated and treated sediments showed a decrease in Fe(III)-oxides, which likely released iodine to aqueous solution. Solid phase inorganic carbon and aqueous Ca and Mg analysis further confirmed that significant calcite dissolution did not occur in these experiments meaning these phases did not release significant iodine. Although it was expected that, after treatment, I concentrations would eventually be lower than untreated sediments, continued, elevated iodine concentrations for treated samples over 750 h were observed for leaching experiments. Stop flow events during 1-D column leaching suggested that some iodide precipitated within the first few pore volumes. Further, batch extraction experiments compared iodine-129/127 removal and showed that iodine-129 was more readily removed than iodine-127 suggesting that the two are present in different phases due to their different origins. Although significantly greater iodine is removed with treatment, the long-term leaching needs to be investigated further as it may limit dithionite treatment at the field scale.
本实验室研究评估了使用水还原剂(连二亚硫酸钠)和 pH 缓冲剂(K 碳酸盐,pH 值 12)作为一种潜在的修复方法,用于去除与氧化铁结合的碘,并增强从汉福德场地 200 西区无约束含水层受碘污染的沉积物中进行的抽吸处理提取。未经处理的沉积物的 X 射线荧光数据表明,碘主要与铁(即,可能被纳入氧化铁)结合,但 XANES 数据对价态没有定论。在地下水浸出过程中,水相和吸附碘迅速释放,然后可能从一个或多个表面相的缓慢溶解中缓慢释放更多的碘。与单独用地下水浸出相比,连二亚硫酸钠处理以更快的速度(1-4 个数量级)去除了更多的碘质量(2.9x)。未处理和处理沉积物的铁提取表明 Fe(III)-氧化物减少,这可能将碘释放到水溶液中。固相无机碳和水相 Ca 和 Mg 分析进一步证实,这些实验中没有发生显著的方解石溶解,这意味着这些相没有释放出大量的碘。尽管预计处理后碘浓度最终会低于未经处理的沉积物,但在 1-D 柱浸出实验中,处理样品的碘浓度仍持续升高,超过 750 小时。停流事件表明,在最初几个孔隙体积内,一些碘化物可能沉淀。此外,批量提取实验比较了碘-129/127 的去除率,结果表明碘-129 比碘-127 更容易去除,这表明两者存在于不同的相中,这是由于它们的不同来源。尽管处理后可以去除更多的碘,但需要进一步研究长期浸出情况,因为它可能会限制连二亚硫酸钠在现场规模上的处理。