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Improved understanding of bimolecular reactions in deceptively simple homogeneous media: From laboratory experiments to Lagrangian quantification

机译:在看似简单的均匀介质中增进对双分子反应的理解:从实验室实验到拉格朗日定量

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摘要

Medium heterogeneity affects reaction kinetics by controlling the mixing of reactant particles, but the linkage between medium properties and reaction kinetics is difficult to build, even for simple, relatively homogeneous media. This study aims to explore the dynamics of bimolecular reactions, aniline + 1,2-naphthoquinone-4-sulfonic acid → 1,2-naphthoquinone-4-aminobenzene, in relatively homogeneous flow cells. Laboratory experiments were conducted to monitor the transport of both conservative and reactive tracers through columns packed with silica sand of specific diameters. The measured tracer breakthrough curves exhibit subdiffusive behavior with a late-time tail becoming more pronounced with decreasing sand size, probably due to the segregated flow regions formed more easily in columns packed with smaller size sand. Numerical analysis using a novel Lagrangian model shows that subdiffusion has a twofold effect on bimolecular reactions. While subdiffusion enhances the power-law growth rate of product mass by prolonging the exposure of reactant particles in the depletion zone, the global reaction rate is constrained because subdiffusion constrains the mobility of reactant particles. Reactive kinetics in deceptively simple homogeneous media is therefore controlled by subdiffusion, which is sensitive to the dimensions of packed sand.
机译:介质的非均质性通过控制反应物颗粒的混合来影响反应动力学,但是即使对于简单,相对均质的介质,介质性能和反应动力学之间的联系也难以建立。这项研究的目的是在相对均质的流通池中探索双分子反应动力学,即苯胺+ 1,2-萘醌-4-磺酸→1,2-萘醌-4-氨基苯。进行了实验室实验,以监测保守示踪剂和反应示踪剂在填充有特定直径硅砂的色谱柱中的传输。测得的示踪剂穿透曲线表现出亚扩散行为,随着沙子尺寸的减小,后期尾部变得更加明显,这可能是由于在填充较小尺寸沙子的色谱柱中更容易形成分离的流动区域。使用新型拉格朗日模型的数值分析表明,亚扩散对双分子反应具有双重影响。虽然亚扩散通过延长耗尽区中的反应物颗粒的暴露来提高产物质量的幂律增长率,但整体反应速率受到了限制,因为亚扩散会限制反应物颗粒的迁移率。因此,看似简单的均质介质中的反应动力学受到亚扩散的控制,该扩散对堆积砂的尺寸敏感。

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  • 来源
    《Water resources research》 |2014年第2期|1704-1715|共12页
  • 作者单位

    State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Hohai University, Nanjing, China,Desert Research Institute, Las Vegas, Nevada, USA;

    School of Resources and Environmental Engineering, Hefei University of Technology, Hefei, China;

    Department of Civil Engineering, New Mexico State University, Las Cruces, New Mexico, USA,;

    Department of Mathematics, University of Nevada, Las Vegas, Nevada, USA;

    State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Hohai University, Nanjing, China,Department of Geoscience, University of Nevada, Las Vegas, Nevada, USA;

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