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ABSTRACT
Testing of a simplified soil phosphorus model is described. Changes in organic P content of the surface soil due to cultivation are simulated relatively accurately for periods of up to 40 years at several locations in the Great Plains. Simulated changes in organic P contents of the subsoil are smaller than those of the topsoil. Concentrations of soil test P are accurately simulated over periods of up to 20 years with and without fertilizer P applications in several soils. Simulated responses of maize (Zea mays L.) and wheat (Triticum aestivum L.) to soil test P concentrations are similar to those found in three published studies. Fertilizer P required to maintain adequate P fertility is accurately simulated for maize and wheat at several locations in the U.S.
1 Contribution from USDA-ARS, and Oklahoma State Univ.
2 Plant Physiologist, USDA-ARS, Grassland, Soil and Water Research Lab., P.O. Box 748, Temple, TX 76503; Soil Scientist, USDA-ARS and Oklahoma State Univ.; Water Quality and Watershed Research Lab., P.O. Box 1430, Durant, OK 74702; Hydraulic Engineer, USDA-ARS, Grassland, Soil and Water Research Lab., P.O. Box 748, Temple, TX 76503.
Received for publication October 26, 1983. Accepted for publication February 17, 1984.
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K.-W. Juang, D.-C. Liou, and D.-Y. Lee Site-Specific Phosphorus Application Based on the Kriging Fertilizer-Phosphorus Availability Index of Soils J. Environ. Qual., July 1, 2002; 31(4): 1248 - 1255. [Abstract] [Full Text] [PDF] |
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