EGU25-15101, updated on 15 Mar 2025
https://doi.org/10.5194/egusphere-egu25-15101
EGU General Assembly 2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Poster | Tuesday, 29 Apr, 14:00–15:45 (CEST), Display time Tuesday, 29 Apr, 14:00–18:00
 
Hall A, A.116
Nitrate fate in mixed surface water and groundwater: Role of mixing-dependent denitrification and DNRA in hyporheic zones
Xue Ping1, Zhang Wen1, Yang Xian1, Stefan Krause4,5,6, Songhu Yuan2,3, Zhixin Zhang1, and Menggui Jin1,2
Xue Ping et al.
  • 1China University of Geosciences, School of Environmental Studies, China (xping@cug.edu.cn)
  • 2State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan, China
  • 3Hubei Key Laboratory of Yangtze Catchment Environmental Aquatic Science, School of Environmental Studies, China University of Geosciences, Wuhan, China
  • 4School of Geography, Earth and Environmental Sciences, University of Birmingham, Edgbaston, Birmingham B15 2TT, UK
  • 5Institute for Global Innovation, University of Birmingham, Edgbaston, Birmingham B15 2TT, UK
  • 6Birmingham Institute for Sustainability and Climate Action (BISCA), University of Birmingham, Edgbaston, Birmingham B15 2TT, UK

Hyporheic zones (HZs), where surface water (SW) and groundwater (GW) mix underneath and adjacent to streams, are known for their inherent ability to attenuate contaminants. Mixing of reactants from SW and GW enables the occurrence of mixing-dependent reactions, mixing-dependent denitrification is commonly regarded as the last defense against groundwater-bone nitrate before it enters to streams. However, the impact of mixing-dependent DNRA on nitrate transformation is often overlooked. In this study, we conducted a flume experiment to generate downwelling of SW with dissolved organic carbon (DOC) into the sediments and create a hyporheic exchange flow (HEF) cell. We added nitrate to anoxic upwelling GW to stimulate mixing-dependent reactions. Hydrodynamics, hydrochemical conditions, microbial community and its biogeochemical function with respect to nitrogen transformation were tested and analyzed. The SW and GW mixing zone was situated along the fringe of HEF cell. The mixing zone represented a transition zone between the HEF cell and deeper GW in microbial community structure, and hosted active mixing-dependent reaction potentials. Both mixing-dependent denitrification and DNRA occurred, with the hotspots for these processes appearing predominantly on the right side (closer to the GW) and the left side (closer to the HEF cell) of the mixing zone, rather than evenly within it. The downstream and upstream movement of the mixing zone enhances the mixing-dependent denitrification and DNRA reactions. The NH4+ produced by mixing-dependent DNRA would undergo further nitrification within the HEF cell because higher concentrations of nitrification functional genes present upstream. Disregarding the mixing-dependent DNRA would lead to an overestimation of HZs’ capacity to attenuate groundwater-borne nitrate. This study enhances our understanding of nitrate processing within HZs and contributes valuable insights for the effective management of watershed contaminants.

How to cite: Ping, X., Wen, Z., Xian, Y., Krause, S., Yuan, S., Zhang, Z., and Jin, M.: Nitrate fate in mixed surface water and groundwater: Role of mixing-dependent denitrification and DNRA in hyporheic zones, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-15101, https://doi.org/10.5194/egusphere-egu25-15101, 2025.