Abstract

Use of cover crops in an integrated agricultural system can reduce demand of inorganic phosphorus (P) fertilizers, where the subsequent crops can take up P accumulated in cover crops biomass after the decomposition. In this research we hypothesized that some cover crops can take up P from less labile fractions and recycle it back to the soil through plant residues resulting in better P use efficiency of the system; cover crops are capable of P uptake from subsurface layers which leads to the accumulation of this P on the surface after the decomposition of their residues; and cover crop species respond differently to distinct inorganic P sources. To examine these hypotheses, a field experiment was conducted over nine successive years in South Brazil. The experimental treatments were established as a split-plot randomized block design, in a 3 × 6 factorial scheme, considering three P treatments [no-P, single superphosphate (SSP), and rock phosphate (RP)] as main plot and six cover crop treatments (common vetch, white lupin, fodder radish, ryegrass, black oat, and a fallow) as subplots. Soil samples were collected from the depths of 0–5, 5–10, and 10–15 cm and analyzed by Hedley P fractionation. In P-unfertilized cropping system, the amounts of labile and mod-labile P fractions were not modified by cover crops related to fallow. When inorganic P fertilizers were applied, the amount of labile and mod-labile P pools under fallow were higher than under cover crops in 5–10 cm depth. Black oat and common vetch cycled more labile P under SSP and RP, respectively. Common vetch and ryegrass resulted in the highest accumulation of organic P on the surface under SSP and RP, respectively. Black oat was capable to change P extracted by 1.0 M HCl to more labile forms. Fodder radish showed the highest P uptake in comparison with other cover crops. The higher P balance efficiency of the system was achieved under SSP in comparison with RP application but it seems that cover crops are more effective at improving the efficiency under RP compared to SSP.

Highlights

  • Phosphorus is the least mobile plant nutrient and a key limiting factor for crop development in agricultural systems (Hinsinger, 2001) and terrestrial ecosystems (Frossard et al, 1995)

  • When inorganic P fertilizers were applied, the amount of labile and mod-labile P pools under fallow were higher than under cover crops in the second soil layer evaluated (5–10 cm), showing that cover crops were able to take up P from less labile P fractions in subsurface layers and accumulate it on the surface after the decomposition of their residues (Table 2)

  • Cover crops evaluated in our study were able to take up P from less labile P fractions in subsurface layers and accumulate it on the surface after the decomposition of their residues

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Summary

Introduction

Phosphorus is the least mobile plant nutrient and a key limiting factor for crop development in agricultural systems (Hinsinger, 2001) and terrestrial ecosystems (Frossard et al, 1995). Some plants like white lupin (Lupinus albus), pigeon pea (Cajanus cajan), rye (Secale cereale), and wheat (Triticum aestivum) are capable of using these less labile P fractions through different acquisition strategies and accumulate it in their aboveground plant parts (Braum and Helmke, 1995; Kamh et al, 1999; Raghothama, 1999; Wasaki et al, 2008, 2009) These crops can be used as cover crops in an integrated agricultural system (Vanlauwe et al, 2000; Horst et al, 2001), where the subsequent crops can take up P accumulated in their biomass after the decomposition, resulting in reduced demand of inorganic P fertilizers. Residues with high C:N ratio, high lignin and low cellulose contents like the species of the Poaceae family including black oat (Avena strigosa) and rye decompose slower and release smaller amounts of P (Ferreira et al, 2014), while residues with low C:N ratio, low lignin and high cellulose contents like the species of Brassicaceae family, including oilseed radish (Raphanus sativus) decompose faster and release higher amounts of P to the soil (Doneda et al, 2012)

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