Plants have developed different mechanisms to absorb and solubilize phosphorus (P) in the soil, especially in environments with low P availability. This study evaluated the effects of different winter cover crops on soil P availability in a clayey subtropical (Hapludox) soil receiving soluble P fertilizer and a rock phosphate applied to the summer crop, under no-tillage. The experiment was carried out over 3 yrs (2009)(2010)(2011) with five different cover crop species: common vetch, fodder radish, ryegrass, black oat, white clover and fallow as control. The soil was sampled after the third year of cover crop cultivation and analysed for inorganic and organic P forms according to the well-established Hedley fractionation procedure. Phosphate fertilizers promoted accumulation of both labile and nonlabile P pools in soil in the near surface layer, especially under rock phosphate. Fertilizer applications were not able to change P fractions in deeper layers, emphasizing that the Brazilian clayey soils are a sink of P from fertilizer and its mobility is almost nil. Although the cover crops recycled a great amount of P in tissue, in a short-term evaluation (3 yrs) they only changed the content of moderately labile P in soil, indicating that long-term studies are needed for more conclusive results.
Phosphorus is one of the most limiting nutrients for plants in weathered tropical soils. To overcome this constraint, the use of humic‐complexed phosphate fertilizer may be considered as one alternative, which would reduce P fixation and increase its bioavailability. This study aimed to determine the crop yield response and soil P lability changes after five crop cycles under humic‐complexed and non‐humic‐complexed superphosphate cumulative applications. The field experiment was conducted for 4 yr (2010–2013) in Tibagi, Brazil, in a Typic Hapludox, arranged in a randomized block design with two P sources; single superphosphate (SSP) and complexed single superphosphate (CSSP); and five cumulative dosages (0, 48, 96, 144, and 192 kg P ha−1), divided over five consecutive crops: maize (Zea mays L.), wheat (Triticum aestivum L.), soybean [Glycine max (L.) Merr.], white oat (Avena sativa L.), and soybean. Grain yield was determined for each crop and soil samples were collected after the fifth harvest for Hedley P fractionation. Our results demonstrated that cumulative grain yield increased in line with the P dosage, however, higher agronomic efficiency was also observed at intermediate P dosages, when CSSP was used. Labile soil P was more influenced by the application of CSSP than SSP. Moreover, higher cumulative P dosages also increased labile and non‐labile P, mainly in the 0‐ to 5‐cm layer, indicating an intensive P pool reallocation in the surface soil layer. The study demonstrated that humic‐complexed phosphate fertilizer can enhance soil P availability and improve crop grain yield in commercial field conditions.Core Ideas
Phosphate fertilizers efficiency in cropping system.
Residual effects of phosphate sources in tropical weathered soils.
Organic complexed fertilizers can be more efficient in plant P supply.
Soil labile P is affected by clay content and its adsorption capacity.
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