2014
DOI: 10.1002/2013wr014711
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Improved understanding of bimolecular reactions in deceptively simple homogeneous media: From laboratory experiments to Lagrangian quantification

Abstract: 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 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 tr… Show more

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Cited by 27 publications
(9 citation statements)
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“…relatively uniform soils and smooth surface) in this experiment, the flow velocity can vary along the soil surface (Deng et al, 2006) where the delayed flow forms the late-time tailing. It is also noteworthy that we observed similar late-time tailing behavior in tracer transport through relatively uniform and saturated soils repacked in sand columns (Zhang et al, 2014). To further check the sensitivity of the tailing behavior to model parameters, we add two more model results with ¼ 0.80 and ¼ 0.30 s À1 for model (1), and ¼ 0.75 and ¼ 0.15 s À1 for model (2) (see the gray and dashed lines in Figure 5(a) and (b)).…”
Section: A Preliminary Application Of the Physical Modelsupporting
confidence: 79%
“…relatively uniform soils and smooth surface) in this experiment, the flow velocity can vary along the soil surface (Deng et al, 2006) where the delayed flow forms the late-time tailing. It is also noteworthy that we observed similar late-time tailing behavior in tracer transport through relatively uniform and saturated soils repacked in sand columns (Zhang et al, 2014). To further check the sensitivity of the tailing behavior to model parameters, we add two more model results with ¼ 0.80 and ¼ 0.30 s À1 for model (1), and ¼ 0.75 and ¼ 0.15 s À1 for model (2) (see the gray and dashed lines in Figure 5(a) and (b)).…”
Section: A Preliminary Application Of the Physical Modelsupporting
confidence: 79%
“…Anomalous transport with retention or early arrivals have been well documented in many disciplines, motivating the development of nonlocal physical models such as the fractional advection‐dispersion equation (fADE) [ Metzler and Klafter , ; Kilbas et al ., ; Herrmann , ]. In hydrology, anomalous diffusion due to retention has been observed for tracers transport in soils [ Pachepsky et al ., ; Levy and Berkowitz , ; Bromly and Hinz , ; Cortis and Berkowitz , ; Delay et al ., ; Hunt et al ., ], rocks [ LaBolle and Fogg , ; Kosakowski , ; Pedretti et al ., ; Ronayne , ], and streams [ Czernuszenko et al ., ; González‐Pinzón et al ., ], while anomalous diffusion with early arrivals has been found for conservative tracer transport in soils [ Zhang et al ., ], streams [ Deng et al ., , ; Kim and Kavvas , ], bed load or suspended sediment transport in rivers [ Stark et al ., ; Houssais and Lajeunesse , , among many others], and solutes moving along fractured media at various scales [ Benson et al ., ; Reeves et al ., , b; Zhang et al ., ]. The fADE is found to be superior to the second‐order advection‐dispersion equation (ADE) in quantifying the observed non‐Fickian transport behavior [ Benson et al ., , 2004; Schumer et al ., ; Zhang et al ., ].…”
Section: Introductionmentioning
confidence: 99%
“…Laboratory experiments of conservative tracer transport through repacked sand columns were conducted recently to explore the anomalous dynamics at the Darcy scale (Zhang et al ). One glass tube with internal dimensions of 100 cm in length and 4 cm in diameter was packed with coarse sand, and transport of Brilliant Blue FCF (BBF) was then monitored with various flow rates through the saturated column.…”
Section: Applicationsmentioning
confidence: 99%