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首页> 外文期刊>Geochimica et Cosmochimica Acta: Journal of the Geochemical Society and the Meteoritical Society >Multicomponent reactive transport modeling of uranium bioremediation field experiments
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Multicomponent reactive transport modeling of uranium bioremediation field experiments

机译:铀生物修复现场实验的多组分反应输运模型

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A reaction network integrating abiotic and microbially mediated reactions has been developed to simulate biostimulationfield experiments at a former Uranium Mill Tailings Remedial Action (UMTRA) site in Rifle, Colorado. The reaction net-work was calibrated using data from the 2002 field experiment, after which it was applied without additional calibrationto field experiments performed in 2003 and 2007. The robustness of the model specification is significant in that (1) the2003 biostimulation field experiment was performed with 3 times higher acetate concentrations than the previous biostimu-lation in the same field plot (i.e., the 2002 experiment), and (2) the 2007 field experiment was performed in a new unperturbedplot on the same site. The biogeochemical reactive transport simulations accounted for four terminal electron-accepting pro-cesses (TEAPs), two distinct functional microbial populations, two pools of bioavailable Fe(III) minerals (iron oxides andphyllosilicate iron), uranium aqueous and surface complexation, mineral precipitation and dissolution. The conceptual modelfor bioavailable iron reflects recent laboratory studies with sediments from the UMTRA site that demonstrated that the bulk(90%) of initial Fe(III) bioreduction is associated with phyllosilicate rather than oxide forms of iron. The uranium reactionnetwork includes a U(VI) surface complexation model based on laboratory studies with Rifle site sediments and aqueous com-plexation reactions that include ternary complexes (e.g., calcium—uranyl—carbonate). The bioreduced U(IV), Fe(II), and sul-fide components produced during the experiments are strongly associated with the solid phases and may play an importantrole in long-term uranium immobilization.
机译:已经开发了一个整合了非生物和微生物介导的反应的反应网络,以模拟科罗拉多州步枪市以前的铀厂尾矿补救行动(UMTRA)站点的生物刺激场实验。使用2002年现场实验的数据对反应网络进行校准,然后将其应用到2003年和2007年进行的现场实验中,而无需进行额外的校准。模型规范的鲁棒性在于:(1)进行了2003年生物刺激现场实验在相同的田地中(即2002年实验),乙酸盐浓度比以前的生物刺激高3倍;(2)2007年的田间试验是在同一地点的新无扰动地块中进行的。生物地球化学反应输运模拟解释了四个末端电子接受过程(TEAP),两个不同的功能微生物种群,两个可生物利用的Fe(III)矿物质池(氧化铁和页硅酸盐铁),铀水和表面络合,矿物沉淀和解散。可生物利用铁的概念模型反映了最近对UMTRA站点沉积物进行的实验室研究,表明最初的Fe(III)生物还原的大部分(90%)与页硅酸盐而不是铁的氧化物形式有关。铀反应网络包括基于实验室研究的U(VI)表面络合模型,该实验室研究涉及步枪位点沉积物和包括三元络合物(例如钙-铀酰-碳酸根)的水性络合反应。实验过程中产生的生物还原的U(IV),Fe(II)和硫化物组分与固相密切相关,并可能在长期铀固定化中发挥重要作用。

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