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Modeling in-situ uranium(VI) bioreduction by sulfate-reducing bacteria

机译:模拟还原硫酸盐细菌的原位铀(VI)生物还原

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We present a travel-time based reactive transport model to simulate an in-situ bioremediation experiment for demonstrating enhanced bioreduction of uranium(VI). The model considers aquatic equilibrium chemistry of uranium and other groundwater constituents, uranium sorption and precipitation, and the microbial reduction of nitrate, sulfate and U(VI). Kinetic sorption/desorption of U(VI) is characterized by mass transfer between stagnant micro-pores and mobile flow zones. The model describes the succession of terminal electron accepting processes and the growth and decay of sulfate-reducing bacteria, concurrent with the enzymatic reduction of aqueous U(VI) species. The effective U(VI) reduction rate and sorption site distributions are determined by fitting the model simulation to an in-situ experiment at Oak Ridge, TN. Results show that (1) the presence of nitrate inhibits U(VI) reduction at the site; (2) the fitted effective rate of in-situ U(VI) reduction is much smaller than the values reported for laboratory experiments; (3) U(VI) sorption/desorption, which affects U(VI) bioavailability at the site, is strongly controlled by kinetics; (4) both pH and bicarbonate concentration significantly influence the sorption/desorption of U(VI), which therefore cannot be characterized by empirical isotherms; and (5) calcium-uranyl-carbonate complexes significantly influence the model performance of U(VI) reduction.
机译:我们提出了一个基于旅行时间的反应性运输模型来模拟原位生物修复实验,以证明铀(VI)的生物还原作用得到了增强。该模型考虑了铀和其他地下水成分的水生平衡化学,铀的吸收和沉淀以及硝酸盐,硫酸盐和U(VI)的微生物还原。 U(VI)的动力学吸附/解吸的特征是停滞的微孔与流动区之间的传质。该模型描述了终端电子接受过程的连续过程以及硫酸盐还原菌的生长和衰变,同时还伴随着酶催化的U(VI)水溶液的还原。通过将模型模拟拟合到田纳西州橡树岭的原位实验,可以确定有效的U(VI)还原速率和吸附位点分布。结果表明:(1)硝酸盐的存在抑制了该位点的U(VI)还原; (2)原位U(VI)降低的拟合有效率远小于实验室实验报告的值; (3)U(VI)的吸附/解吸影响了现场的U(VI)生物利用度,受动力学的强烈控制; (4)pH和碳酸氢盐浓度都显着影响U(VI)的吸附/解吸,因此不能用经验等温线来表征; (5)铀酰碳酸钙复合物显着影响U(VI)还原的模型性能。

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