Wu Wei-Min, Carley Jack, Fienen Michael, Mehlhorn Tonia, Lowe Kenneth, Nyman Jennifer, Luo Jian, Gentile Margaret E, Rajan Raj, Wagner Daniel, Hickey Robert F, Gu Baohua, Watson David, Cirpka Olaf A, Kitanidis Peter K, Jardine Philip M, Criddle Craig S
Department of Civil and Environmental Engineering, Stanford University, Stanford, California 94305-4020, USA.
Environ Sci Technol. 2006 Jun 15;40(12):3978-85. doi: 10.1021/es051954y.
To evaluate the potential for in situ bioremediation of U(VI) to sparingly soluble U(IV), we constructed a pilot test facility at Area 3 of the U.S. Department of Energy Natural and Accelerated Bioremediation Research (NABIR) Field Research Center (FRC) in Oak Ridge, TN. The facility is adjacent to the former S-3 Ponds which received trillions of liters of acidic plating wastes. High levels of uranium are present, with up to 800 mg kg(-1) in the soil and 84-210 microM in the groundwater. Ambient groundwater has a highly buffered pH of approximately 3.4 and high levels of aluminum (12-13 mM), calcium (22-25 mM), and nitrate (80-160 mM). Adjusting the pH of groundwater to approximately 5 within the aquifer would deposit extensive aluminum hydroxide precipitate. Calcium is present in the groundwater at levels that inhibit U(VI) reduction, but its removal by injection of a high pH solution would generate clogging precipitate. Nitrate also inhibits U(VI) reduction and is present at such high concentrations that its removal by in situ denitrification would generate large amounts of N2 gas and biomass. To establish and maintain hydraulic control, we installed a four well recirculation system parallel to geologic strike, with an inner loop nested within an outer loop. For monitoring, we drilled three boreholes perpendicular to strike across the inner loop and installed multilevel sampling tubes within them. A tracer pulse with clean water established travel times and connectivity between wells and enabled the assessment of contaminant release from the soil matrix. Subsequently, a highly conductive region of the subsurface was prepared for biostimulation by removing clogging agents and inhibitors and increasing pH. For 2 months, groundwater was pumped from the hydraulically conductive zone; treated to remove aluminum, calcium, and nitrate, and supplemented with tap water; adjusted to pH 4.3-4.5; then returned to the hydraulically conductive zone. This protocol removed most of the aqueous aluminum and calcium. The pH of the injected treated water was then increased to 6.0-6.3. With additional flushing, the pH of the extracted water gradually increased to 5.5-6.0, and nitrate concentrations fell to 0.5-1.0 mM. These conditions were judged suitable for biostimulation. In a companion paper (Wu et al., Environ. Sci. Technol. 2006, 40, 3978-3987), we describe the effects of ethanol addition on in situ denitrification and U(VI) reduction and immobilization.
为评估将六价铀原位生物修复为难溶性四价铀的可能性,我们在美国田纳西州橡树岭市能源部自然与加速生物修复研究(NABIR)现场研究中心(FRC)的3区建造了一个中试测试设施。该设施毗邻 former S - 3 池塘,那里曾接收了数万亿升的酸性电镀废水。土壤中存在高含量的铀,含量高达800 mg kg⁻¹,地下水中铀含量为84 - 210 μM。环境地下水的pH值约为3.4,具有高度缓冲性,且含有高浓度的铝(12 - 13 mM)、钙(22 - 25 mM)和硝酸盐(80 - 160 mM)。在含水层中将地下水pH值调节至约5会沉淀出大量氢氧化铝。地下水中钙的含量会抑制六价铀的还原,但通过注入高pH值溶液去除钙会产生堵塞性沉淀。硝酸盐也会抑制六价铀的还原,且其浓度很高,通过原位反硝化作用去除硝酸盐会产生大量氮气和生物质。为建立并维持水力控制,我们安装了一个与地质走向平行的四井循环系统,内循环嵌套在外循环内。为进行监测,我们垂直于走向在内循环上钻了三个钻孔,并在其中安装了多级采样管。用清水进行示踪剂脉冲实验确定了井间的水流时间和连通性,并能够评估土壤基质中污染物的释放情况。随后,通过去除堵塞剂和抑制剂并提高pH值,为生物刺激准备了地下高导水区域。持续两个月,从高导水区域抽取地下水;进行处理以去除铝、钙和硝酸盐,并补充自来水;将pH值调节至4.3 - 4.5;然后再回注到高导水区域。该方案去除了大部分溶解态的铝和钙。然后将注入的处理后水的pH值提高到6.0 - 6.3。经过额外冲洗,抽出的水的pH值逐渐升高至5.5 - 6.0,硝酸盐浓度降至0.5 - 1.0 mM。这些条件被判定适合进行生物刺激。在一篇配套论文(Wu等人,《环境科学与技术》,2006年,40卷,39