Comparison of methods for extracting available phosphorus from soils of the semi-arid

Autores/as

  • Maria Deuzilene Oliveira do Nascimento Medeiros https://orcid.org/0000-0003-4475-3218
  • Fábio Henrique Tavares de Oliveira
  • Welka Preston
  • Maria Regilene de Freitas Costa Paiva
  • Helena Maria de Morais Neta Góis

Palabras clave:

Alkaline soils. Mehlich-1. Olsen. Ion-exchange resin.

Resumen

Mehlich-1 is the most used method in Brazil for extracting available phosphorus (P) from the soil. Given the heterogeneity
of soils in the semi-arid region of the Northeast, and the need for an analytical protocol for P extraction, the Mehlich-1, Olsen and ionexchange resin methods were compared in samples of ten representative soils taken from the semi-arid region between the valley of the
River Piranhas-Açu (Rio Grande do Norte) and the valley of the River Jaguaribe (Ceará), where the soil pH ranges from 4.1 to 8.0. The
soil samples received four doses of P based on the phosphate buffering capacity (PBC) of the soils, and were incubated for 30
days. The treatments were divided into randomised blocks, in a 10 × 4 factorial arrangement, represented by ten soils and four doses of
phosphorus, each with three replications. Each experimental unit comprised one plastic pot containing 3.0 dm³ of soil, where two maize
plants were grown for 31 days in a greenhouse. The P extracted by each method was correlated with the P accumulated in the aerial part
of the plants. The mixed-resin and Olsen methods showed the best correlation with the P accumulated in the plants, irrespective of the
pH or PBC of the soil. Neutralisation of the acidity of Mehlich-1 was signifi cant in alkaline soils with high levels of CaCO3
equivalent.
Mehlich-1 was suitable for strongly acidic soils with a low PBC, however, the use of this extractor in pH neutral to alkaline soils with a
high Ca2+ content can overestimate P availability when the soils are rich in P-Ca, or underestimate the availability in soils rich in CaCO3
.

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Publicado

2021-08-03

Número

Sección

Ciencia del suelo