Mitigation of Shallow Groundwater Nitrate in a Poorly Drained Riparian Area and Adjacent Cropland

• Published in: Journal of environmental quality 2007-05, Vol.36 (3), p.628-637
• Main Authors: Davis, J.H, Griffith, S.M, Horwath, W.R, Steiner, J.J, Myrold, D.D
• Format: Article
• Language: English
• Subjects: Agricultural land; Agriculture; Carbon; Carbon - chemistry; chlorides; Chlorides - chemistry; Coastal plains; Cropping systems; Dissolved inorganic carbon; Dissolved organic carbon; Dissolved oxygen; drainage; Freshwater; Groundwater; groundwater contamination; Lolium perenne; microbial activity; Moisture content; nitrates; Nitrates - chemistry; Nitrous oxide; Nitrous Oxide - chemistry; Nutrient cycles; Oxygen - chemistry; pollution control; riparian areas; Riparian ecology; Rivers; Soil - analysis; Soil horizons; soil respiration; soil transport processes; Soil water; Soils; Stream flow; Studies; Surface water; Time Factors; Trifolium repens; Velocity; Water Pollutants, Chemical - chemistry; Water Pollution, Chemical - prevention & control; Water quality
• ISSN: 0047-2425; 1537-2537
• DOI: 10.2134/jeq2006.0186

Riparian ecosystems, through their unique position in the agricultural landscape and ability to influence nutrient cycles, can potentially reduce NO3 loading to surface and ground waters. The purpose of this study was to determine the fate of NO3 in shallow groundwater moving along a lateral flowpath from a grass seed cropping system through an undisturbed mixed-species herbaceous riparian area. Soil A (30-45 cm) and C horizon (135-150 cm) NO3, dissolved oxygen, and nitrous oxide concentrations were significantly higher in the cropping system than the adjacent riparian area. Nitrate concentrations in both horizons of the riparian soil were consistently at or below 0.05 mg N L-1 while cropping system concentrations ranged from 1 to 12 mg N L-1. Chloride data suggested that NO3 dilution occurred from recharge by precipitation. However, a sharp decrease in NO3/Cl ratios as water moved into the riparian area indicated that additional dilution of NO3 concentrations was unlikely. Riparian area A horizon soil water had higher dissolved organic carbon than the cropping system and when the riparian soil became saturated, available electron acceptors (O2, NO3) were rapidly reduced. Dissolved inorganic carbon was significantly higher in the riparian area than the cropping system for both horizons indicating high biological activity. Carbon limitation in the cropping system may have led to microbial respiration using primarily O2 and to a lesser degree NO3. Within 6 m of the riparian/cropping system transition, NO3 was virtually undetectable.