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Where the past meets the present

Connecting nitrogen from watersheds to streams through groundwater flowpaths

Bibliographic Data

ID15550221
AuthorsEric M Moore (0000-0002-2479-2677, University of Connecticut, corresponding author), Janet R Barclay (0000-0003-1643-6901, United States Geological Survey), A Haynes (0000-0002-0190-2976, University of California, Santa Cruz), Adam B Haynes, Kevin Jackson (0000-0002-2156-5073, University of Connecticut), Kevin E Jackson, Alaina Bisson (0009-0005-4419-4542, University of Connecticut), Alaina M Bisson, Martin A Briggs (0000-0003-3206-4132, United States Geological Survey), Ashley M Helton (0000-0001-6928-2104, University of Connecticut)
Year2023
Volume18
Issue12
Pages124039-124039
Publication date2023-11-14
Open AccessYes
TypeARTICLE
VenueEnvironmental Research Letters (JOURNAL)
Journal identifiersISSN: 1748-9326 • E-ISSN: 1748-9326
PublisherIOP Publishing (PUBLISHER • GB)
DOI10.1088/1748-9326/ad0c86
OpenAlexW4388661857
LanguageEN
Citations received1
References cited65

Groundwater discharge to streams is a nonpoint source of nitrogen (N) that confounds N mitigation efforts and represents a significant portion of the annual N loading to watersheds. However, we lack an understanding of where and how much groundwater N enters streams and watersheds. Nitrogen concentrations at the end of groundwater flowpaths are the culmination of biogeochemical and physical processes from the contributing land area where groundwater recharges, within the aquifer system, and in the near-stream riparian area where groundwater discharges to streams. Our research objectives were to quantify the spatial distribution of N concentrations at groundwater discharges throughout a mixed land-use watershed and to evaluate how relationships among contributing and riparian land cover, modeled aquifer characteristics, and groundwater discharge biogeochemistry explain the spatial variation in groundwater discharge N concentrations. We accomplished this by integrating high-resolution thermal infrared surveys to locate groundwater discharge, biogeochemical sampling of groundwater, and a particle tracking model that links groundwater discharge locations to their contributing area land cover. Groundwater N loading from groundwater discharges within the watershed varied substantially between and within streambank groundwater discharge features. Groundwater nitrate concentrations were spatially heterogeneous ranging from below 0.03–11.45 mg-N/L, varying up to 20-fold within meters. When combined with the particle tracking model results and land cover metrics, we found that groundwater discharge nitrate concentrations were best predicted by a linear mixed-effect model that explained over 60% of the variation in nitrate concentrations, including aquifer chemistry (dissolved oxygen, Cl − , SO 4 2− ), riparian area forested land cover, and modeled physical aquifer characteristics (discharge, Euclidean distance). Our work highlights the significant spatial variability in groundwater discharge nitrate concentrations within mixed land-use watersheds and the need to understand groundwater N processing across the many spatiotemporal scales within groundwater cycling

Aquifer · Baseflow · Biogeochemical cycle · Drainage basin · Geography · Groundwater · Groundwater discharge · Groundwater flow · Groundwater model · Habitat · Hydrology (agriculture · Land cover · Land use · Nitrate · Riparian zone · Streamflow · STREAMS · Watershed · Chemistry · Environmental Science · Groundwater and Isotope Geochemistry · Hydrology and Watershed Management Studies · Soil and Water Nutrient Dynamics · Ecology · Environmental Chemistry · Geology

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Citations per year1
Citation span2025 - 2025 (1)
Highly citedNo

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