Le. Gentry et al., NITROGEN CYCLING AND TILE DRAINAGE NITRATE LOSS IN A CORN SOYBEAN WATERSHED/, Agriculture, ecosystems & environment, 68(1-2), 1998, pp. 85-97
Nitrogen (N) in surface waters has been linked to agricultural crop pr
oduction, and more specifically, to NO3- exported by tile drainage. Th
e objective of this study was to evaluate agricultural N pools and flu
xes in a seed corn/soybean (Zea maize L./Glycine max L.) watershed (40
ha) to relate soil inorganic N pools with annual losses of NO3- in dr
ainage tiles. During a 2-year period beginning in October 1993, soil s
amples in the top 50 cm located near the tile systems (predominantly D
rummer silty clay loam, fine-silty, mixed mesic Typic Haplaquolls) wer
e analyzed for microbial biomass C and N, inorganic N, and N mineraliz
ation rates. Water flow and NO3- concentrations were continuously meas
ured in the three drainage tiles. Soil microbial biomass N ranged from
83 to 156 kg N ha(-1), and appeared more closely related to soil mois
ture than soil inorganic N pools. Soil inorganic N ranged from a low o
f 13 kg N ha(-1) during the soybean growing season to a high of 115 kg
N ha(-1) after N fertilization. Following good growing seasons in 199
3 and 1993, high crop uptake of N resulted in relatively small soil in
organic N pools of 40 and 24 kg N ha(-1), respectively, after crop har
vest. In 1995, however, when poor growing conditions decreased crop N
accumulation, 98 kg N ha(-1) remained in the watershed after harvest.
Based on an average effective drainage area of 30 ha, 38 and 64 kg N h
a(-1) leached out of the watershed through tile drainage for a total o
f 3.1 Mg N for the 1995 and 1996 water years, respectively. Tile N exp
ort from the watershed was greatest during high flow events when there
concurrently existed large pools of soil inorganic N in the form of N
O3-. Differences in annual N export for each tile were the result of a
combination of factors including; timing and area of N fertilization,
amount and distribution of precipitation, crop uptake of soil derived
N, and inorganic N pools remaining after harvest. (C) 1998 Elsevier S
cience B.V.