2004
DOI: 10.1590/s0100-06832004000600003
|View full text |Cite
|
Sign up to set email alerts
|

Adsorção de fósforo, superfície específica e atributos mineralógicos em solos desenvolvidos de rochas vulcânicas do Alto Paranaíba (MG)

Abstract: M. M. CORRÊA (4) , E. I. FERNANDES FILHO (3) & M. M. IBRAIMO (4) RESUMOMuitos solos tropicais com grau avançado de intemperismo, apesar de apresentarem teores totais de P relativamente elevados, mostram-se deficientes em P disponível, pela baixa solubilidade das principais formas de P encontradas. Neste trabalho, estudou-se o processo de adsorção de P em solos desenvolvidos de rochas vulcânicas básicas e ultrabásicas do Alto Paranaíba em Minas Gerais, algumas das quais ricas em apatita, estabelecendo-se relaçõ… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
3
2

Citation Types

1
4
0
2

Year Published

2010
2010
2021
2021

Publication Types

Select...
7
1

Relationship

0
8

Authors

Journals

citations
Cited by 36 publications
(7 citation statements)
references
References 24 publications
(26 reference statements)
1
4
0
2
Order By: Relevance
“…The precipitation of SRP by Luvisol, Planosol, and Scheelite tailing refuted the hypothesis that the greatest SRP adsorption would be that of the natural adsorbent material with a higher clay content, indicating that the mineralogy of this clay fraction in addition to the content of exchangeable bases in the soil is more important than clay fraction content, as was reported by other studies (Rolim-Neto et al, 2004;Corrêa et al, 2011).…”
Section: Discussionsupporting
confidence: 79%
See 1 more Smart Citation
“…The precipitation of SRP by Luvisol, Planosol, and Scheelite tailing refuted the hypothesis that the greatest SRP adsorption would be that of the natural adsorbent material with a higher clay content, indicating that the mineralogy of this clay fraction in addition to the content of exchangeable bases in the soil is more important than clay fraction content, as was reported by other studies (Rolim-Neto et al, 2004;Corrêa et al, 2011).…”
Section: Discussionsupporting
confidence: 79%
“…The presence of gibbsite in this fraction may contribute to the high efficiency of the tailings in SRP sorption. Gibbsite strongly retains phosphate (Rolim-Neto et al, 2004;Eriksson et al, 2016), so knowledge of the mineralogy of clay fraction is essential to understand the potential for SRP sorption by the natural adsorbent materials, even more than quantity. In semiarid regions, gibbsite plays a greater role in the maximum phosphorus sorption capacity of soils than iron oxides (Agbenin & Tiessen, 1994).…”
Section: Discussionmentioning
confidence: 99%
“…In another study, it was observed that the amount of available phosphorus in soil decreases gradually as a function of the number of grown crops and the removal of this nutrient by plants [ 20 ]. Besides the uptake by plants, it is argued that a decrease in available phosphorus in soil may be related to the low solubility of phosphorus compounds in soil and the formation of nonlabile compounds in the soil after application of the waste [ 21 ].…”
Section: Discussionmentioning
confidence: 99%
“…Among the models, there is a preference for the Langmuir isotherm, because it allows to obtain the maximum soil phosphorus adsorption capacity (PAC) and the constant "k", related to the energy of this element binding to the soil (Novais & Smyth, 1999). As it turns, the PAC is strongly associated with the clay content and the type of mineral present in the soil (Rolim Neto et al, 2004;Simões Neto et al, 2009;Corrêa, Nascimento, & Tavares, 2011).…”
Section: Introductionmentioning
confidence: 92%
“…In tropical soils, clay minerals govern the sorption and adsorption mechanism of P, both supplying this nutrient to the plant and competing for P applied in phosphate fertilizers (Rolim Neto, Schaefer, Costa, Corrêa, Fernandes Filho, & Ibraimo, 2004). Several investigations have shown that goethite (Gt = α-FeOOH) and gibbsite (Gb = γ-Al(OH) 3 ) rich soils provide higher P-fixing power than hematite-governed soils (Hm = α-Fe 2 O 3 ) and, secondarily, kaolinite (Kt) (Broggi, Oliveira, F. J. Freire, M. B. G. S. Freire, & Nascimento, 2011;Barbieri et al, 2014).…”
Section: Introductionmentioning
confidence: 99%