2022
DOI: 10.1016/j.advwatres.2021.104087
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A systematic model-based evaluation of the influence of hydraulic conductivity, heterogeneity and domain depth on hyporheic nutrient transformation

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Cited by 8 publications
(3 citation statements)
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“…The localized high‐frequency turbulent exchange demonstrated here is likely to be important because of the high metabolic activity and rapid biogeochemical transformation rates near the sediment‐water interface, for example, as observed for nitrogen (Grant, Azizian, et al., 2018; Marzadri et al., 2014). The model framework presented here can be extended to assess the effects of turbulence on biogeochemical processes by including models for hyporheic metabolism (e.g., Bardini et al., 2012; Caruso et al., 2017; Laube et al., 2022). Using this approach to improve parameterization of reach‐ and basin‐scale biogeochemical models, for example, through scaling relationships based on river bed and flow conditions, provides means to account for the effects of both turbulent transport and riverbed clogging on fluvial biogeochemistry.…”
Section: Discussionmentioning
confidence: 99%
“…The localized high‐frequency turbulent exchange demonstrated here is likely to be important because of the high metabolic activity and rapid biogeochemical transformation rates near the sediment‐water interface, for example, as observed for nitrogen (Grant, Azizian, et al., 2018; Marzadri et al., 2014). The model framework presented here can be extended to assess the effects of turbulence on biogeochemical processes by including models for hyporheic metabolism (e.g., Bardini et al., 2012; Caruso et al., 2017; Laube et al., 2022). Using this approach to improve parameterization of reach‐ and basin‐scale biogeochemical models, for example, through scaling relationships based on river bed and flow conditions, provides means to account for the effects of both turbulent transport and riverbed clogging on fluvial biogeochemistry.…”
Section: Discussionmentioning
confidence: 99%
“…It is expressed by the nonlinear partial differential equation. The equation is based on Darcy's law for groundwater flow conception [24][25][26][27][28].…”
Section: Methodsmentioning
confidence: 99%
“…An undulating streambed alters the currents, creating hydraulic gradients along with the soil-water interface that works as a driver of groundwater and surface water exchange [22,23]. The automated generation of streamlines in the subsurface domain, with various streambed setups and subsurface characteristics, could help to bring a better understanding of the process and behavior of the streamlines and residence time distribution under varying streambed conditions, whereas this cannot be efficiently performed in the case in the laboratory experiments [24]. Moreover, it is not possible for repeatability of results, a high number of variations, greater insight into the three-dimensional system, or understanding of individual streamlines or residence time distribution to be well executed in the lab-based experimentation.…”
Section: Introductionmentioning
confidence: 99%