Environmental Sciences Division, Oak Ridge National Laboratory, Oak Ridge, Tennessee 37831-6038, United States.
Environ Sci Technol. 2013 Jun 18;47(12):6440-8. doi: 10.1021/es3033555. Epub 2013 Jun 4.
A field test with a one-time emulsified vegetable oil (EVO) injection was conducted to assess the capacity of EVO to sustain uranium bioreduction in a high-permeability gravel layer with groundwater concentrations of (mM) U, 0.0055; Ca, 2.98; NO3(-), 0.11; HCO3(-), 5.07; and SO4(2-), 1.23. Comparison of bromide and EVO migration and distribution indicated that a majority of the injected EVO was retained in the subsurface from the injection wells to 50 m downgradient. Nitrate, uranium, and sulfate were sequentially removed from the groundwater within 1-2 weeks, accompanied by an increase in acetate, Mn, Fe, and methane concentrations. Due to the slow release and degradation of EVO with time, reducing conditions were sustained for approximately one year, and daily U discharge to a creek, located approximately 50 m from the injection wells, decreased by 80% within 100 days. Total U discharge was reduced by 50% over the one-year period. Reduction of U(VI) to U(IV) was confirmed by synchrotron analysis of recovered aquifer solids. Oxidants (e.g., dissolved oxygen, nitrate) flowing in from upgradient appeared to reoxidize and remobilize uranium after the EVO was exhausted as evidenced by a transient increase of U concentration above ambient values. Occasional (e.g., annual) EVO injection into a permeable Ca and bicarbonate-containing aquifer can sustain uranium bioreduction/immobilization and decrease U migration/discharge.
进行了一次单次乳化植物油(EVO)注入的野外试验,以评估 EVO 在具有地下水浓度(mM)U 为 0.0055、Ca 为 2.98、NO3(-)为 0.11、HCO3(-)为 5.07 和 SO4(2-)为 1.23 的高渗透砾石层中维持铀生物还原的能力。溴化物和 EVO 迁移和分布的比较表明,注入的大部分 EVO 从注入井保留在地下,向下游 50 米。硝酸盐、铀和硫酸盐在 1-2 周内从地下水中依次去除,同时乙酸盐、Mn、Fe 和甲烷浓度增加。由于 EVO 随时间缓慢释放和降解,还原条件持续了大约一年,距离注入井约 50 米的小溪中每天的 U 排放量在 100 天内减少了 80%。在一年的时间里,总 U 排放量减少了 50%。通过对回收含水层固体的同步加速器分析证实了 U(VI)向 U(IV)的还原。来自上游的氧化剂(例如溶解氧、硝酸盐)似乎在 EVO 耗尽后重新氧化并重新迁移铀,这表现为 U 浓度暂时高于环境值。偶尔(例如每年)向含有钙和碳酸氢盐的可渗透含水层注入 EVO 可以维持铀的生物还原/固定,并减少 U 的迁移/排放。