Phosphorus Concentrations and Loads in Runoff Water under Crop Production

Transport of phosphorus (P) through surface runoff from agriculture is suspected to contribute to the eutrophication of surface waters in South Florida and elsewhere. There is minimal quantitative information on the concentrations and loads of various P forms in surface runoff water on a field‐scale...

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Veröffentlicht in:Soil Science Society of America journal 2006-09, Vol.70 (5), p.1807-1816
Hauptverfasser: He, Z. L., Zhang, M. K., Stoffella, P. J., Yang, X. E., Banks, D. J.
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container_issue 5
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Zhang, M. K.
Stoffella, P. J.
Yang, X. E.
Banks, D. J.
description Transport of phosphorus (P) through surface runoff from agriculture is suspected to contribute to the eutrophication of surface waters in South Florida and elsewhere. There is minimal quantitative information on the concentrations and loads of various P forms in surface runoff water on a field‐scale. The objective of this study was to evaluate the annual loads of various P forms in runoff water from citrus and vegetable crop production systems in sandy soil regions in Florida and their relations to soil P status, fertilizer P input, and environmental conditions. Eleven field sites (four on vegetable farms and seven in citrus groves) were selected for this monitoring study over a 2‐yr period. The concentrations of total P (TP) in the runoff water samples varied widely from 0.01 to 22.74 mg L−1, with approximately half of the samples having the TP over 1 mg L−1 Eighty‐three percent of the samples had orthophosphate (PO4–P) higher than 0.02 mg L−1 The mean proportion of total dissolved P (TDP) in the TP was higher than that of the total particulate P (TPP). The TDP constituted the major proportion of P in runoff water from most of the sites. The PO4–P accounted for approximately 64% of the TDP. The annual median concentrations of various P forms in the runoff water varied spatially and temporally and were correlated with total and labile P in the soils (water‐P, Olsen‐P, Mehlich 1‐P, and Mehlich 3‐P) as well as fertilizer P rate. The vegetable farms had higher concentrations of P in the runoff water than citrus groves due to their more severe soil erosion and higher fertilizer P input, which resulted in higher soil P accumulation and availability. The annual loads of TP, TDP, and PO4–P varied among the field sites and between the 2 yr. The TP loads were significantly correlated with soil labile P estimated by the four extraction procedures, but the Olsen‐P was best related to runoff P. Runoff P concentrations and the annual discharge rate accounted for 55 to 64% of the variance in the annual P loads. These results indicate that P transport through surface runoff from agriculture is affected by soil P status and water management, and merits attention in the development of best management practices.
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The concentrations of total P (TP) in the runoff water samples varied widely from 0.01 to 22.74 mg L−1, with approximately half of the samples having the TP over 1 mg L−1 Eighty‐three percent of the samples had orthophosphate (PO4–P) higher than 0.02 mg L−1 The mean proportion of total dissolved P (TDP) in the TP was higher than that of the total particulate P (TPP). The TDP constituted the major proportion of P in runoff water from most of the sites. The PO4–P accounted for approximately 64% of the TDP. The annual median concentrations of various P forms in the runoff water varied spatially and temporally and were correlated with total and labile P in the soils (water‐P, Olsen‐P, Mehlich 1‐P, and Mehlich 3‐P) as well as fertilizer P rate. The vegetable farms had higher concentrations of P in the runoff water than citrus groves due to their more severe soil erosion and higher fertilizer P input, which resulted in higher soil P accumulation and availability. The annual loads of TP, TDP, and PO4–P varied among the field sites and between the 2 yr. The TP loads were significantly correlated with soil labile P estimated by the four extraction procedures, but the Olsen‐P was best related to runoff P. Runoff P concentrations and the annual discharge rate accounted for 55 to 64% of the variance in the annual P loads. 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Eleven field sites (four on vegetable farms and seven in citrus groves) were selected for this monitoring study over a 2‐yr period. The concentrations of total P (TP) in the runoff water samples varied widely from 0.01 to 22.74 mg L−1, with approximately half of the samples having the TP over 1 mg L−1 Eighty‐three percent of the samples had orthophosphate (PO4–P) higher than 0.02 mg L−1 The mean proportion of total dissolved P (TDP) in the TP was higher than that of the total particulate P (TPP). The TDP constituted the major proportion of P in runoff water from most of the sites. The PO4–P accounted for approximately 64% of the TDP. The annual median concentrations of various P forms in the runoff water varied spatially and temporally and were correlated with total and labile P in the soils (water‐P, Olsen‐P, Mehlich 1‐P, and Mehlich 3‐P) as well as fertilizer P rate. 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Eleven field sites (four on vegetable farms and seven in citrus groves) were selected for this monitoring study over a 2‐yr period. The concentrations of total P (TP) in the runoff water samples varied widely from 0.01 to 22.74 mg L−1, with approximately half of the samples having the TP over 1 mg L−1 Eighty‐three percent of the samples had orthophosphate (PO4–P) higher than 0.02 mg L−1 The mean proportion of total dissolved P (TDP) in the TP was higher than that of the total particulate P (TPP). The TDP constituted the major proportion of P in runoff water from most of the sites. The PO4–P accounted for approximately 64% of the TDP. The annual median concentrations of various P forms in the runoff water varied spatially and temporally and were correlated with total and labile P in the soils (water‐P, Olsen‐P, Mehlich 1‐P, and Mehlich 3‐P) as well as fertilizer P rate. 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title Phosphorus Concentrations and Loads in Runoff Water under Crop Production
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