NITROGEN CYCLING AND TILE DRAINAGE NITRATE LOSS IN A CORN SOYBEAN WATERSHED/

Citation
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
Citations number
35
Categorie Soggetti
Environmental Sciences",Ecology,Agriculture
ISSN journal
01678809
Volume
68
Issue
1-2
Year of publication
1998
Pages
85 - 97
Database
ISI
SICI code
0167-8809(1998)68:1-2<85:NCATDN>2.0.ZU;2-X
Abstract
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.