Phosphorus Fractionations and Availability in Areas under Different Management Systems in the Cerrado

Author:

Torres José Luiz Rodrigues1ORCID,Costa Danyllo Denner de Almeida2,Pereira Marcos Gervasio3ORCID,Guardieiro Luiz Victorio França1,Loss Arcângelo4ORCID,Lourenzi Cledimar Rogério4ORCID,Gonzalez Antônio Paz5ORCID,Carvalho Mychelle1,Vieira Dinamar Márcia da Silva2

Affiliation:

1. Federal Institute of Triangulo Mineiro, Uberaba Campus, 4000 São João Batista Ribeiro St., Uberaba 38064-790, Minas Gerais, Brazil

2. Department of Agronomy, Agricultural Sciences Institute, Federal University of Uberlandia, Glória Campus, Uberlandia 38410-337, Minas Gerais, Brazil

3. Department of Soils, Federal Rural University of Rio de Janeiro, Seropédica Campus, Seropédica 23897-000, Rio de Janeiro, Brazil

4. Department of Rural Engineering, Center of Agricultural Sciences, Federal University of Santa Catarina, Florianópolis Campus, Florianópolis 88034-000, Santa Catarina, Brazil

5. Department of Soil Science, Facultad de Ciencias, Universidade da Coruña, 88034-000 Coruña, Spain

Abstract

The input of organic matter in the soil by the no-tillage system (NTS) increases as the system becomes established, raising the levels of organic phosphorus (P) and reducing the P soil adsorption. This study evaluated the availability of organic and inorganic P in areas under different management systems and stages of adoption in the Cerrado. The data were analyzed as a completely randomized design, corresponding to: (1) an NTS after 5 years of its implantation (NTS5); (2) an NTS after 17 years of its implantation (NTS17); (3) a conventional tillage system more than 20 years old (CTS); (4) Native Cerrado (NC). There were five repetitions for all treatments. Depths of 0–5 and 5–10 cm were evaluated for the available P (P-avail), remaining P (P-rem), organic P (oP), and inorganic P (iP) forms extracted with Sodium bicarbonate (NaHCO3) (P-avail), Sulfuric acid (H2SO4) (moderately labile), and Sodium hydroxide (NaOH) (moderately resistant). The P from the sequential extractions accumulated at a depth of 0–5 cm, mostly in the organic form in the NTS17 and NC areas, demonstrating the contribution of the NTS to the conversion of the P reserve in the soil. The CTS treatment greatly accumulated P, especially in the inorganic form, indicating the non-conservationist characteristic of this system. The oP and iP contents in the soil were not affected by age of the NTS, which was similar to the NC. Our results show that the continuous input of organic matter deposited on the soil surface in the NTS17 increased the levels of organic and inorganic P, consequently providing greater availability of P in the soil for cultivated crops.

Funder

National Council for Scientific and Technological Development

Luiz de Queiroz Foundation for Agricultural Studies

State Research Support Foundation of Minas Gerais

Publisher

MDPI AG

Subject

Agronomy and Crop Science

Reference51 articles.

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