Abstract
We quantified nutrient concentrations and water quality parameters in soils and water from a working farm (in operation for over 100 years), through contrasting agricultural wetlands, to their receiving waters. Contrasting wetlands were a forested alluvial swamp and a ditched wetland swale. Our objective was to determine if nutrients diminished in concentration or changed in form as water moved through wetlands below the farm. Soils were collected from around the farm and receiving wetlands and were analyzed for nitrate, ammonium, and phosphorus. Water samples, collected from shallow piezometers and surface waters were analyzed for nitrate + nitrite, and total phosphorus. Nitrate in groundwater and surface water in the alluvial swamp were much lower than concentrations measured in flows from farmlands. Nitrogen in upland water was dominated by nitrate, but ammonium dominated in the swamp. Phosphorus was low in wetland soils and also diminished through the swamp. Despite receiving agricultural run-off for many decades, the natural alluvial swamp still provided an effective environment for water quality mitigation of nitrate and phosphorus. The ditched wetland swale did not significantly reduce nitrate but appeared to provide some phosphorus mitigation. Agricultural wetland conservation is an especially effective, low cost tool for water quality management.
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Acknowledgements
We thank Dr. James L. Shelton, the UGA Forest Hydrology Lab, UGA Aquatic Toxicology Lab, the UGA Marine Sciences Lab, the UGA Aquatic Ecosystem Ecology Lab, the UGA Aquatic Entomology Lab, and the USFS Aiken, SC office for technical assistance on this project. We appreciate the cooperation of the Department of Crop and Soil Sciences, Iron Horse Farm with our efforts. This project has been funded in part by the United States Environmental Protection Agency under assistance agreement (CD-00D39815) to DPB. The contents of this document do not necessarily reflect the views and policies of the Environmental Protection Agency, nor does the EPA endorse trade names or recommend the use of commercial products mentioned in this document.
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Fig. S1. Iron Horse Farm hydroperiod and precipitation over the sampling period. Colored lines correspond to sampling events while the gray horizontal line indicates ground level. Dates over the sampling period are listed at the bottom of the figure and the left side shows groundwater depth and locations (landscape descriptions) of each odyssey logger Fig. S2 Map showing median NO3− values in each of the landscape assessment areas. Colored number outlines indicated different sampling types (orange-soil, dark blue-surface water, light blue-groundwater). White lines indicate landscape region boundaries compared using ANOVA/Kruskal-Wallis Fig. S3 Map showing phosphorus median values in each of the landscape assessment areas. Colored number outlines indicated different sampling types (orange-soil, dark blue-surface water, light blue-groundwater). White lines indicate landscape region boundaries compared using ANOVA/Kruskal-Wallis Fig. S4 Water quality parameters in surface waters and groundwater (shallow piezometer samples) across landscape positions on each side of the farm and in the reference wetland. Arrows point along hydraulic gradients from upland positions to receiving waters. Distributions reflect monthly samples collected over a year Table S1 Mean daily precipitation on days of purging wells (Purging) and bimonthly water sampling at Iron Horse farm (Sampling) Fig. S5 Relationship of NO3− to NH4+ in shallow groundwater samples during August 2017 sampling. August 2017 provided a single months example of variation among different forms of nitrogen and possible method for future biogeochemical assessment. Dissolved inorganic nitrogen (DIN) appeared in one form or the other, with no samples showing a significant mix of the two forms. There was no significant difference in landscape positions but water samples showed biogeochemical activity in the alluvial swamp through high levels of NO3− in the pasture/feedlot toeslope and high levels of NH4+ in the alluvial swamp. Fig. S6 NO3− in Iron Horse Farm soils, landscape positions show composition (soils plugs collected and mixed to form one sample) soil sampling results and circles show distribution (individual samples assessed at each circle) soil sampling results. NO3− is higher in soil on the south side of the farm but shows a small instance of elevated NO3− on the north side Fig. S7 NH4+ in Iron Horse Farm soils, landscape positions show composition (soils plugs collected and mixed to form one sample) soil sampling results and circles show distribution (individual samples assessed at each circle) soil sampling results. NH4+ is high in soil in the alluvial swamp with variance within the swamp and along wet fringes on the south side of the farm Fig. S8 PO43− in Iron Horse Farm soils, landscape positions show composition (soils plugs collected and mixed to form one sample) soil sampling results and circles show distribution (individual samples assessed at each circle) soil sampling results. PO43− is high in soil in the feed lot and upper agricultural field and shows lower levels elsewhere around the farm (PDF 1.54 mb)
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Matteson, C.T., Jackson, C.R., Batzer, D.P. et al. Nitrogen and Phosphorus Gradients from a Working Farm through Wetlands to Streams in the Georgia Piedmont, USA. Wetlands 40, 2139–2149 (2020). https://doi.org/10.1007/s13157-020-01335-z
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DOI: https://doi.org/10.1007/s13157-020-01335-z