Localized zones of denitrification in a floodplain aquifer in southern Wisconsin, USA

A floodplain aquifer within an agricultural watershed near Madison, Wisconsin (USA), was studied to determine whether denitrification was occurring below the surface organic layer. Groundwater levels and concentrations of O₂, Cl⁻, NO ₃ ⁻ , SO ₄ ²⁻ , dissolved organic carbon (DOC), and major cations were monitored over a 1-year period along a 230-m transect between an agricultural field and a stream discharge point. Seventeen groundwater samples were analyzed for δ¹⁵NNO₃ and δ¹⁸ONO₃ composition. Samples in which NO ₃ ⁻ was too low for stable isotope analysis were analyzed for excess dissolved N₂. Groundwater NO ₃ ⁻ concentrations declined between the agricultural field and the discharge point. Chloride and δ¹⁵NNO₃/δ¹⁸ONO₃ data indicated that the drop in NO ₃ ⁻ was caused primarily by dilution of shallow NO ₃ ⁻ -rich water with deeper, NO ₃ ⁻ -depleted groundwater. Two localized zones of denitrification were identified in the upland-wetland transition by their δ¹⁵NNO₃ and δ¹⁸ONO₃ signatures, and two in the stream hyporheic zone by the presence of excess dissolved N₂. The combined stratigraphic, hydrologic, and geochemical data in these locations correspond to groundwater mixing zones where NO ₃ ⁻ is delivered to subsurface layers that support denitrification fueled by dissolved (e.g. DOC or dissolved Fe(II)) and/or solid-phase (e.g. particulate organic carbon, solid-associated Fe(II), or pyrite) electron donors.