Dynamics of Forms of Inorganic Phosphorus in Soil under Coffee Plants as a Function of Successive Annual Additions of the Nutrient

• Published in: Communications in Soil Science and Plant Analysis Vol. 42; no. 8; pp. 980 - 991
• Main Authors: Reis, Thiago Henrique Pereira, Neto, Antônio Eduardo Furtini, Guimarães, Paulo Tácito Gontijo, Curi, Nilton, Guerra, Antônio Fernando, Marques, João José
• Format: Journal Article
• Language: English
• Published: Philadelphia, PA Taylor & Francis Group 05.04.2011; Taylor & Francis; Taylor & Francis Ltd
• Subjects: Agronomy. Soil science and plant productions; Biological and medical sciences; Coffee; Fundamental and applied biological sciences. Psychology; Kaolinitic-oxidic soil; Mineralogy; phosphorus forms; soil chemistry; Soil science; Soil chemistry; Dynamic characteristic; Kaolinitic-oxidic soil; Coffea; Woody plant; phosphorus forms; Inorganic compound; Soils; Dicotyledones; Angiospermae; Rubiaceae; Nutrient; Spermatophyta; Kaolinite; Inorganic phosphorus
• ISSN: 0010-3624; 1532-2416; 1532-4133
• DOI: 10.1080/00103624.2011.558966

Phosphorus (P) dynamics and availability in soils are influenced by P fertilization. This paper aimed to evaluate inorganic P fractions bonded to calcium (Ca), iron (Fe), and aluminum (Al), associating them with soil mineralogy. The experiment was carried out using an acidic kaolinitic-oxidic soil, located in an irrigated area cultivated with coffee plants (Coffee arabica L.), submitted to successive annual fertilizations with triple superphosphate doses of 0, 50, 100 200, and 400 kg ha −1 phosphorus pentoxide (P 2 O 5 ) in randomized blocks with three replications. Phosphorus fractions were determined in soil samples collected at two depths, 0-10 and 10-20 cm, according to the methodology used by Chang and Jackson (1957 ). The inorganic P fractions presented the following sequence: P-Al > P-Fe > P-Ca. The dynamics of forms of inorganic P showed that P-Al is controlling the P bioavailability as a result of an acidic pH and a very simple and thermodynamically stable clay mineralogy, typical of very weathered and old tropical soils.