Nitrogen losses in runoff from three adjacent agricultural watersheds with claypan soils

Despite improvements in the use of soil conservation practices, crop rotation and managed fertilizer applications, large losses of nitrogen (N) in runoff continue to occur from row-cropped watersheds. Increasing requirements for implementing water quality standards in the United States, has increase...

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Bibliographic Details
Published in:Agriculture, ecosystems & environment ecosystems & environment, 2006-10, Vol.117 (1), p.39-48
Main Authors: Udawatta, Ranjith P., Motavalli, Peter P., Garrett, Harold E., Krstansky, J. John
Format: Article
Language:English
Subjects:
agricultural runoff
agricultural watersheds
claypan soils
corn
Corn–soybean rotation
crop rotation
fallow
Glycine max
land management
losses from soil
nitrate nitrogen
Nitrate-N in runoff
nitrogen
nitrogen content
rain
soybeans
temporal variation
Total-N in runoff
vegetation cover
water quality
Zea mays
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Summary:Despite improvements in the use of soil conservation practices, crop rotation and managed fertilizer applications, large losses of nitrogen (N) in runoff continue to occur from row-cropped watersheds. Increasing requirements for implementing water quality standards in the United States, has increased pressure for the development of research-based guidelines to reduce N losses from agricultural runoff. The objectives of this study were to examine the effects of management, watershed characteristics, and precipitation on TN and nitrate-N (NO 3 −-N) loss over time by comparing losses on three adjacent watersheds with claypan soils. The three adjacent north-facing, corn–soybean rotational watersheds in northeastern Missouri were instrumented with H-flumes, water samplers, and flow-monitoring devices in 1991. Runoff samples from each individual rainfall event between 1991 and 1997 were analyzed for TN and NO 3 −-N concentrations. The 7-year mean annual TN losses on the three watersheds ranged from 13 to 19 kg ha −1 with a mean of 16 kg ha −1. Nitrate-N losses ranged from 8 to 14 kg ha −1 with a mean of 11 kg ha −1. During the study, 67% of the TN was lost as NO 3 −-N with a range from 22% in 1997 to 76% in 1996. The mean annual TN losses for corn and soybean years during the study were 30.7 and 5.7 kg ha −1, respectively. Significantly higher loss (57%) of N from watersheds occurred during the period between fall harvest and spring planting when crops were not present (referred to as the “fallow” period in this paper; 86.8 kg ha −1) compared to N losses during the cropping period (64.5 kg ha −1). In 1994, 96% of the annual TN loss and 98% of the annual NO 3 −-N loss occurred during the fallow period. In contrast, the lowest fallow period losses of TN (19%) and NO 3 −-N (14%) occurred in 1993. The watershed-mean TN and NO 3 −-N losses in 1993 alone accounted for 44 and 46% of the total losses observed over the 7-year period because during that year the study area received 142% of the normal precipitation. When the study area received 51% of the annual precipitation before planting in 1996, the TN and NO 3 −-N losses accounted for 34 and 38% of the 7-year loss, respectively. Nitrogen fertilizer that was applied in 1993 and 1996 may also have contributed to the observed large losses. The results of this study suggest that the maintenance of a suitable vegetative cover throughout the year could reduce runoff and lower TN and NO 3 −-N loss from agricultural watershe
ISSN:0167-8809
1873-2305
DOI:10.1016/j.agee.2006.03.002