Pipe Dreams: The Effects of Stream Bank Soil Pipes on Hyporheic Denitrification Caused by a Peak Flow Event

Abstract

Peak flow events in gaining stream/river channels cause lung model hyporheic exchange with the banks (bank storage), which fosters beneficial reactions as polluted channel water cycles through riparian groundwater. Soil pipes are common along stream/riverbanks, and enhance exchange, yet their effect on reactions such as denitrification is unknown. We used MODFLOW with the Conduit Flow Package to simulate lung model exchange during a peak flow event in a section of stream bank/riparian soil with soil pipes, and MT3D‐USGS to estimate nitrate transport and denitrification. We varied soil matrix hydraulic conductivity (K) and first‐order reaction constant (k), as well as soil pipe density, length, and height above the initial channel water surface elevation (H). The addition of soil pipes enhanced stream bank (riparian) denitrification relative to banks without pipes, e.g., a 76% increase due to adding a single 1.5 m pipe. Denitrification increased linearly with pipe density but exhibited nonlinear trends with other parameters. Sensitivity analysis revealed length and density to be most influential. Soil pipe enhancement of denitrification was governed by hyporheic volume in most cases in our study. Exceptions included (a) coarse soil (K = 10−3 m/s) and (b) low k and H > 0. Scaling our results to the stream corridor scale estimated that five soil pipes per m cumulatively induced 3% nitrate removal along a 1 km reach. Overall, soil pipes enhanced advection of nitrate into the banks, and also increased residence times of that nitrate under certain conditions, which together enhanced denitrification. This enhancement has implications for excess nitrate management in watersheds.

Numerical simulation of overbank hyporheic transport and biogeochemical reactions in a compound channel

“…The hyporheic zone (HZ) is the volume beneath and adjacent to a river where surface and ground water mix (Gualtieri, 2014; Tonina, 2012), which is considered to be a biogeochemical hot spot in the river system (Lotts & Hester, 2020). Such mixing enhances the transport of nutrients, pollutants, energy, oxygen, nitrogen, and carbon in riverine systems (Lin et al, 2020; Wallace et al, 2020; Wu et al, 2020).…”

“…the river system (Lotts & Hester, 2020). Such mixing enhances the transport of nutrients, pollutants, energy, oxygen, nitrogen, and carbon in riverine systems (Lin et al, 2020;Wallace et al, 2020;Wu et al, 2020).…”