Abstract

The phosphorus supply to crops in tropical soils is deficient due to its somewhat insoluble nature in soil, and addition of P fertilizers has been necessary to achieve high yields. The objective of this study was to examine the mechanisms through which a cover crop (Congo grass - Brachiaria ruziziensis) in rotation with soybean can enhance soil and fertilizer P availability using long-term field trials and laboratory chemical fractionation approaches. The experimental field had been cropped to soybean in rotation with several species under no-till for six years. An application rate of no P or 240 kg ha-1 of P2O5 had been applied as triple superphosphate or as Arad rock phosphate. In April 2009, once more 0.0 or 80.0 kg ha-1 of P2O5 was applied to the same plots when Congo grass was planted. In November 2009, after Congo grass desiccation, soil samples were taken from the 0-5 and 5-10 cm depth layer and soil P was fractionated. Soil-available P increased to the depth of 10 cm through growing Congo grass when P fertilizers were applied. The C:P ratio was also increased by the cover crop. Congo grass cultivation increased P content in the soil humic fraction to the depth of 10 cm. Congo grass increases soil P availability by preventing fertilizer from being adsorbed and by increasing soil organic P.

Highlights

  • The low efficiency of phosphorus use by crops in tropical soils is mostly due to soil P-fixation through adsorption or precipitation reactions

  • Crop residues applied together with rock phosphate resulted in increased soil P availability, increased cereal P uptake, and higher yields than application of rock phosphate alone (Waigwa et al, 2003)

  • The objective of this study was to evaluate the effectiveness of Congo grass (B. ruziziensis) grown as a cover crop in enhancing soil P availability and its relationship to C behavior using long-term field trials and laboratory chemical fractionation approaches

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Summary

Introduction

The low efficiency of phosphorus use by crops in tropical soils is mostly due to soil P-fixation through adsorption or precipitation reactions. One potential approach is to adopt cropping systems that may increase the level of plant-available P in soil. From 30 to 50 % of total soil P is organic P, appearing mainly as phytates, nucleic acids (and their derivatives), and phospholipids. Some of this organic P is contained in or originates from crop residues. Crop residues applied together with rock phosphate resulted in increased soil P availability, increased cereal P uptake, and higher yields than application of rock phosphate alone (Waigwa et al, 2003). Essington & Howard (2000) reported that plots under no-till had significantly higher values of organic P than those under conventional tillage

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