SSSAJ Journal of Natural Resources and Life Sciences Education
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Published online 2 December 2005
Published in Soil Sci Soc Am J 70:163-171 (2006)
DOI: 10.2136/sssaj2005.0102
© 2005 Soil Science Society of America
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Nutrient Management & Soil & Plant Analysis

Phosphorus Loss in Runoff from Long-term Continuous Wheat Fertility Trials

H. Zhanga, J. L. Schrodera,*, R. L. Davisc, J. J. Wangd, M. E. Paytonb, W. E. Thomasone, Y. Tangf and W. R. Rauna

a Dep. of Plant and Soil Sciences
b Dep. of Statistics, Oklahoma State Univ., Stillwater, OK 74078
c Apex Environmental Inc., Lenexa, KS 66215
d Dep. of Agronomy and Environmental Management, Louisiana State Univ., Baton Rouge, LA 70803
e Dep. of Crop and Soil Environmental Sciences, Virginia Polytechnic Institute and State Univ., Blacksburg, VA 24061
f Yangzhou Univ., Jiangsu, China

* Corresponding author (jschrod{at}okstate.edu)

Some wheat (Triticum aestivum L.) farmers in the southern Great Plains routinely apply P fertilizer without soil testing. This practice may lead to P buildup in soils, hence, increased P runoff potential, making soil P management of concern in continuous wheat production. At present, there is also debate over the nature of P loss trends, particularly whether soil P release to runoff can be described generally, across a broad range of soils, or is soil-specific. Paired 1 m by 2 m runoff plots were established on three existing long-term continuous winter wheat fertility experiments. Two experiments have received annual fertilizer P application at different rates since 1970 (0–44 kg P ha–1), and the third received a one-time P application at much higher rates in 1977 (0–587 kg P ha–1). Rainfall-runoff experiments were conducted following the National P Research Project protocol. Simulated rain (75 mm h–1) produced 30 min of runoff from plots with different soil test P levels. Soil Mehlich-3 P (M3P) ranged from 11.5 to 130 mg kg–1 and water-soluble P (WSP) ranged from 0.70 to 15.7 mg kg–1. Runoff total P and dissolved reactive P (DRP) concentrations ranged from 0.47 to 1.5 and 0.03 to 0.70 mg L–1, respectively. Dissolved reactive P in runoff was significantly related to M3P, WSP, and ammonium oxalate P saturation index (PSIox) for combined soils as well as for individual soil series. Significant differences (p < 0.05) among the slopes of the regressions for the DRP-M3P, DRP-WSP, and DRP-PSIox relationships indicate that the relationships are soil specific. This study highlights the need for soil specific management to protect water quality.

Abbreviations: Alox, ammonium oxalate extractable Al • DRP, dissolved reactive P • Feox, ammonium oxalate extractable Fe • ICP–AES, inductively coupled plasma–atomic emission spectroscopy • M3P, Mehlich-3 P • NPRP, National Phosphorus Research Project • Pox, ammonium oxalate extractable P • PP, particulate P • PSIox, ammonium oxalate P saturation index • Smax, phosphorus adsorption maximum • STP, soil test P • TSS, total suspended solids • TP, total P • USEPA, United State Environmental Protection Agency • WSP, water soluble P







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