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Published in J Environ Qual 23:752-758 (1994)
© 1994 American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
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Groundwater Nitrate Levels under Fertilized Grass and Grass-Legume Pastures

L. B. Owens* and W. M. Edwards

USDA-Agricultural Research Service, North Appalachian Exp. Watershed, P.O. Box 478, Coshocton, OH 43812;

R. W. Van Keuren

Dep. of Agronomy, The Ohio State Univ./Ohio Agric. Res. Dev. Ctr., 1680 Madison Ave., Wooster, OH 44691.

* Corresponding author (!a031ccoshoct).

ABSTRACT

High levels of N fertilizer applied to pastures can result in NO3-N concentrations in groundwater exceeding the USEPA potable water standard of 10 mg N/L. This study was conducted to determine groundwater NO3-N levels following a change in N source from fertilizer to a legume in a grass-pasture grazed by beef cattle. For 5 yr, 224 kg N/ha was applied annually to small watersheds with orchardgrass (Dactylis glomerata L.) pastures used for summer-grazing and tall fescue (Festuca arundinacea Schreb.) areas used for winter-grazing-feeding. At the beginning of the sixth year, alfalfa (Medicago sativa L.) was interseeded into the grass pastures and N fertilizer was no longer applied. Groundwater sampies from developed springs and surface runoff samples were collected and analyzed for NH4-N, NO3-N, and total N for the 5-yr fertilization period and for the following 10-yr period without applied N fertilizer. Nitrogen in groundwater was present mainly in the NO3 form, and concentrations increased throughout the 5-yr period of fertilizer application and reached levels that were usually in excess of 10 mg N/L. With the change from N fertilizer to legume N, the NO3-N concentrations in groundwater dropped rapidly during a 2-yr period. In a tall fescue-alfalfa area, NO3-N levels decreased from 17.7 to 9.3 mg N/L. In two orchard-grass-alfalfa areas, NO3-N levels decreased from 11.2 to 2.7 and from 8.3 to 3.6 mg N/L. During the remainder of the 10-yr period, NO3-N concentrations declined to levels similar to those before N fertilization. Although the amount of N lost via subsurface flow decreased with decreasing concentrations, subsurface flow remained the main pathway for N loss compared with surface runoff or sediment-attached N.


NOTES

Joint contribution from USDA-ARS and OSU-OARDC.

Received for publication August 2, 1993.


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