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a Dep. of Agronomy, Iowa State Univ., Ames, IA 50011
b Formerly a graduate student, now at Pioneer Hi-Bred, Inc., 910 6th Street, Colo, IA 50056
* Corresponding author (apmallar{at}iastate.edu)
Farmers and nutrient management regulatory agencies are requesting better knowledge of P fertilization impacts on soil-test P (STP) and crop yield. This study evaluated STP and grain yield of corn (Zea mays L.) and soybean [Glycine max (L.) Merr.] as affected by long-term P fertilization in three trials evaluated from the 1970s until 2002 near Boone, Kanawha, and Nashua in central, northern, and northeast Iowa. Soils were Aquic Hapludolls and Typic Endoaquolls at Boone, Typic Endoaquolls at Kanawha, and Typic Hapludolls at Nashua. At Boone and Kanawha, treatments were the combinations of three initial STP levels (1796 mg P kg1, Bray-P1) and four annual rates (033 kg P ha1). At Nashua, initial STP was 28 mg P kg1 and treatments were 0, 22, and 44 kg P ha1. Ten to twenty years of cropping were needed on soils testing 43 to 96 mg P kg1 to observe yield response to P. Annual P rates that maintained near optimum STP (1620 mg P kg1) were 17, 14, and 13 kg P ha1 yr1 at Boone, Kanawha, and Nashua, respectively. Phosphorus required to increase STP 1 mg P kg1 yr1 were 23, 28, and 17 kg P ha1 yr1 at Boone, Kanawha, and Nashua, respectively. Critical STP concentrations (CC) identified across sites and years were 15 to 21 mg P kg1 for corn and 12 to 18 mg P kg1 for soybean. Observed grain yield and STP responses are useful to develop effective P management plans for cornsoybean rotations under approximately similar conditions to those in this study.
Abbreviations: CC, critical soil-test P concentration STP, soil-test P
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