Nitrogen and phosphorus in surface runoff and sediment from a wheat-pea rotation in northeastern Oregon

Runoff and erosion from cultivated fields are suggested as major sources of nitrogen (N) and phosphorus (P) entering lakes and streams. Loss of these nutrients can be impacted by soil and crop management practices. There is relatively little information on nutrients leaving agricultural fields in th...

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Bibliographic Details
Published in:Journal of environmental quality 1998-09, Vol.27 (5), p.1170-1177
Main Authors: Douglas, C.L. Jr. (USDA, ARS, Pendleton, OR.), King, K.A, Zuzel, J.F
Format: Article
Language:English
Subjects:
ABONOS
Agronomy. Soil science and plant productions
ARIDOCULTURE
AZOTE
Biological and medical sciences
CULTIVO EN TIERRAS ARIDAS
DRY FARMING
ENGRAIS
ESCORRENTIA
FERTILIZERS
FOSFORO
Fundamental and applied biological sciences. Psychology
LOSSES FROM SOIL
NITROGEN
NITROGENO
OREGON
PERDIDAS DESDE SUELOS
PERTE DES LES SOLS
PHOSPHORE
PHOSPHORUS
Pisum sativum
RUISSELLEMENT
RUNOFF
Soil and water pollution
Soil science
Surface runoff
Triticum aestivum
USA, Oregon, Northeast
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Summary:Runoff and erosion from cultivated fields are suggested as major sources of nitrogen (N) and phosphorus (P) entering lakes and streams. Loss of these nutrients can be impacted by soil and crop management practices. There is relatively little information on nutrients leaving agricultural fields in the dryland areas of the Pacific Northwest, especially as impacted by different crops and crop rotations. Nutrients in surface runoff and soil leaving a series of plots in northeast Oregon were evaluated for 5 yr. Objectives were to evaluate the effects of a wheat-pea (Triticum aestivium L.-Pisum sativum L.) rotation on N and P in surface runoff and eroded soil. Cumulative N and P lost in runoff were less than 3 and 0.2 kg ha-1, respectively. Total N lost from continuous fallow (CF) plots, even though they were never fertilized, ranged from 20 to 100 kg ha-1 yr-1. This was much more N than was lost from winter wheat (WW) (5-70 kg ha-1 yr-1) and spring pea (SP) (25-40 kg ha-1 yr-1), because there was much more sediment loss from CF than from WW or SP plots. The same scenario occurred with P as with N, with loss from CF of 8 to 48 kg ha-1 yr-1, WW of 2 to 28 kg ha-1 yr-1, and from SP of 8 to 16 kg ha-1 yr-1. All fertilizer was surface-applied and 25 to 76% of the fertilizer applied was lost in 5 yr, depending on the time of fertilizer application and the type of crop growing. Nutrient loss from these fields can be controlled by controlling soil erosion
ISSN:0047-2425
1537-2537
DOI:10.2134/jeq1998.00472425002700050023x