Humic acid-phosphate fertilizer interaction and extractable phosphorus in soils of contrasting texture

Extractable phosphorus (P) in soil depends on soil test employed, reactivity of fertilizer and interaction of P added to the soil properties, including organic matter. The aim of this paper was to assess the contents of P extracted from Red Latosol (LVd) and Quartzarenic Neosol (RQ) samples, incubat...

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Published inCiência agronômica Vol. 49; no. 1; pp. 32 - 42
Main Authors Rosa, Sara Dantas, Silva, Carlos Alberto, Maluf, Henrique José Guimarães Moreira
Format Journal Article
LanguageEnglish
Portuguese
Published Fortaleza Universidade Federal do Ceará, Centro de Ciências Agrárias 01.01.2018
Universidade Federal do Ceará
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Abstract Extractable phosphorus (P) in soil depends on soil test employed, reactivity of fertilizer and interaction of P added to the soil properties, including organic matter. The aim of this paper was to assess the contents of P extracted from Red Latosol (LVd) and Quartzarenic Neosol (RQ) samples, incubated with 0; 5; 10; 50 or 100 mg kg-1 C-humic acid (C-HA) and 400 mg kg-1 of P, via Araxá phosphate rock (AP), Bayóvar reactive phosphate rock (BP) or single superphosphate (SS). Thus, it was adopted a five (C-HA concentrations) x three (P sources) factorial arrangement, using a randomized block design with three replications. The mixtures of soil, C-HA concentrations and P sources were incubated for 60 days; in sequence, the soil P was extracted by solutions of Bray-1, Mehlich-1 and Mehlich-3 and mixed ion exchange resin. In the LVd and RQ samples, the addition of C-HA reduced extractable phosphorus when the source was AP and BP. The levels of extractable P increased with the application of C-HA in RQ when the source was SS; the average concentration of 50 mg kg-1 C-AH provided the maximum extractable P by Bray-1, Mehlich-3 and mixed resin. The pH is the chemical attribute that most influence the extractable P content of the soil.
AbstractList Extractable phosphorus (P) in soil depends on soil test employed, reactivity of fertilizer and interaction of P added to the soil properties, including organic matter. The aim of this paper was to assess the contents of P extracted from Red Latosol (LVd) and Quartzarenic Neosol (RQ) samples, incubated with 0; 5; 10; 50 or 100 mg kg-1 C-humic acid (C-HA) and 400 mg kg-1 of P, via Araxá phosphate rock (AP), Bayóvar reactive phosphate rock (BP) or single superphosphate (SS). Thus, it was adopted a five (C-HA concentrations) x three (P sources) factorial arrangement, using a randomized block design with three replications. The mixtures of soil, C-HA concentrations and P sources were incubated for 60 days; in sequence, the soil P was extracted by solutions of Bray-1, Mehlich-1 and Mehlich-3 and mixed ion exchange resin. In the LVd and RQ samples, the addition of C-HA reduced extractable phosphorus when the source was AP and BP. The levels of extractable P increased with the application of C-HA in RQ when the source was SS; the average concentration of 50 mg kg-1 C-AH provided the maximum extractable P by Bray-1, Mehlich-3 and mixed resin. The pH is the chemical attribute that most influence the extractable P content of the soil.
ABSTRACT Extractable phosphorus (P) in soil depends on soil test employed, reactivity of fertilizer and interaction of P added to the soil properties, including organic matter. The aim of this paper was to assess the contents of P extracted from Red Latosol (LVd) and Quartzarenic Neosol (RQ) samples, incubated with 0; 5; 10; 50 or 100 mg kg-1 C-humic acid (C-HA) and 400 mg kg-1 of P, via Araxá phosphate rock (AP), Bayóvar reactive phosphate rock (BP) or single superphosphate (SS). Thus, it was adopted a five (C-HA concentrations) x three (P sources) factorial arrangement, using a randomized block design with three replications. The mixtures of soil, C-HA concentrations and P sources were incubated for 60 days; in sequence, the soil P was extracted by solutions of Bray-1, Mehlich-1 and Mehlich-3 and mixed ion exchange resin. In the LVd and RQ samples, the addition of C-HA reduced extractable phosphorus when the source was AP and BP. The levels of extractable P increased with the application of C-HA in RQ when the source was SS; the average concentration of 50 mg kg-1 C-AH provided the maximum extractable P by Bray-1, Mehlich-3 and mixed resin. The pH is the chemical attribute that most influence the extractable P content of the soil.
Author Rosa, Sara Dantas
Silva, Carlos Alberto
Maluf, Henrique José Guimarães Moreira
AuthorAffiliation Universidade Federal de Lavras
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  givenname: Sara Dantas
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  givenname: Carlos Alberto
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  surname: Maluf
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Issue 1
Keywords Extractors of soil P
Soil pH
Phosphate rocks
pH do solo
Substâncias húmicas
Fosfatos naturais
Humic substances
Extratores de P do solo
Language English
Portuguese
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PublicationTitle Ciência agronômica
PublicationTitleAlternate Rev. Ciênc. Agron
PublicationYear 2018
Publisher Universidade Federal do Ceará, Centro de Ciências Agrárias
Universidade Federal do Ceará
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Snippet Extractable phosphorus (P) in soil depends on soil test employed, reactivity of fertilizer and interaction of P added to the soil properties, including organic...
ABSTRACT Extractable phosphorus (P) in soil depends on soil test employed, reactivity of fertilizer and interaction of P added to the soil properties,...
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SubjectTerms Agrochemicals
AGRONOMY
Extratores de P do solo
Fertilizers
Fosfatos naturais
Humic acids
Ion exchange resins
Organic matter
Organic soils
pH do solo
pH effects
Phosphates
Phosphorus
Soil mixtures
Soil properties
Substâncias húmicas
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Title Humic acid-phosphate fertilizer interaction and extractable phosphorus in soils of contrasting texture
URI https://www.proquest.com/docview/1982847805/abstract/
http://www.scielo.br/scielo.php?script=sci_arttext&pid=S1806-66902018000100032&lng=en&tlng=en
https://doaj.org/article/bf23c24cce7b4529be4eec58e8fb2a34
Volume 49
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