Lb. Owens et al., GROUNDWATER NITRATE LEVELS UNDER FERTILIZED GRASS AND GRASS-LEGUME PASTURES, Journal of environmental quality, 23(4), 1994, pp. 752-758
High levels of N fertilizer applied to pastures can result in NO3-N co
ncentrations 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 appli
ed annually to small watersheds with orchardgrass (Dactylis glomerata
L.) pastures used for summer-grazing and tall fescue (Festuca arundina
cea Schreb.) areas used for winter-grazing-feeding. At the of the sixt
h year, alfalfa (Medicago sativa L.) was interseeded into the grass pa
stures and N fertilizer was no longer applied. Groundwater samples fro
m developed springs and surface runoff samples were collected and anal
yzed for NH4-N, NO3-N, and total N for the 5-yr fertilization period a
nd for the following 10-yr period without applied N fertilizer. Nitrog
en in groundwater was present mainly in the NO3 form, and concentratio
ns increased throughout the 5-yr period of fertilizer application and
reached levels that were usually in excess of 10 mg N/L. With the chan
ge from N fertilizer to legume N, the NO3-N concentrations in groundwa
ter dropped rapidly during a 2-yr period. In a tall fescue-alfalfa are
a, NO3-N levels decreased from 17.7 to 9.3 mg N/L. In two orchard-gras
s-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 concent
rations declined to levels similar to those before N fertilization. Al
though the amount of N lost via subsurface flow decreased with decreas
ing concentrations, subsurface flow remained the main pathway for N lo
ss compared with surface runoff or sediment-attached N.