Published online 12 October 2005
Published in J Environ Qual 34:2024-2035 (2005)
DOI: 10.2134/jeq2004.0445
© 2005 American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
Field-Scale Evaluation of Phosphorus Leaching in Acid Sandy Soils Receiving Swine Waste
Nathan O. Nelsona,*,
John E. Parsonsb and
Robert L. Mikkelsenc
a USDA-ARS Northwest Irrigation and Soils Research Laboratory, 3793 N. 3600 E., Kimberly, ID 83341-5076
b Department of Biological and Agricultural Engineering, Box 7625, North Carolina State University, Raleigh, NC 27695-7625
c Department of Soil Science, Box 7619, North Carolina State Univ., Raleigh, NC 27695-7619

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Fig. 1. (a) Location of pits where soil solution samplers were installed in Autryville and Blanton soils on a 20-yr-old swine farm in Sampson County, NC, and (b) schematic of soil solution samplers as installed at each site in Fig. 1a (time-domain reflectometry [TDR] probes were only installed at Blanton Site I and Autryville Site II).
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Fig. 2. (a) Mehlich 3extractable phosphorus (M3-P) and water-extractable phosphorus (Pw) concentrations with depth in the Autryville and Blanton soils (95% confidence limits [CL] represent ±43 and ±3 mg kg1 M3-P and Pw, respectively) and (b) total phosphorus (TP) and oxalate-extractable phosphorus (Pox) concentrations with depth in the Autryville and Blanton soils (95% confidence limits [CL] represent ±74 and ±56 mg kg1 TP and Pox, respectively).
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Fig. 3. (a) Oxalate-extractable aluminum (Alox) and iron (Feox) and (b) degree of phosphorus saturation (DPS) with depth in the Autryville and Blanton soils (95% confidence limits [CL] represent ±88 and ±30 mg kg1 Alox and Feox, respectively, and ±8% DPS).
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Fig. 4. Monthly precipitation and irrigation during the study compared to the 30-yr average precipitation.
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Fig. 5. Dissolved reactive phosphorus (DRP) concentrations in soil solution collected at (a) 45 cm in the Autryville soil and at 45 and 90 cm in the Blanton soil and (b) 90 and 135 cm in the Autryville soil and at 135 cm in the Blanton soil.
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Fig. 6. Dissolved reactive phosphorus (DRP) concentrations in soil solution at 45 cm in the Autryville soil with corresponding drainage rates from the overlying soil layer (020 cm; bars) and waste applications.
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Fig. 7. Relationship between the (a) average soil solution dissolved reactive phosphorus (DRP) concentration and soil degree of phosphorus saturation (DPS) and (b) water-extractable phosphorus (Pw) concentration and DPS for Autryville and Blanton soils fit with corresponding split-line models.
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Copyright © 2005 by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America.