2014
DOI: 10.1590/s0100-06832014000500018
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Alterações químicas e avaliação de P disponível na região adjacente aos grânulos de superfosfato triplo e diamônio fosfato em solos ácidos

Abstract: RESUMOO P tem baixa mobilidade no solo resultando em altas concentrações nas regiões adjacentes aos grânulos de fertilizantes fosfatados. Isso pode interferir na disponibilidade de P e na composição química do solo nesses locais. O objetivo deste estudo foi avaliar a composição química do solo e a mobilidade de P nas adjacências de regiões fertilizadas com fosfatos de amônio ou de cálcio, em solos ácidos. Este trabalho foi realizado em 2009, com amostras de dois solos catarinenses. Os tratamentos consistiram d… Show more

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Cited by 3 publications
(3 citation statements)
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“…Acidification is also an indirect consequence of the increase in the concentration of sulfate in the soil solution (Rosado et al, 2014). Oliveira et al (2014) found decrease in the pH of electronegative soils up to 10 cm from the location of potassium chloride (KCl) granules; this decrease in pH was mainly attributed to increase in the density of electric charges at the surface of the electronegative colloids of the soils, due to the increase in electrolytic concentration, releasing ions of an acidic nature to the soil solution.…”
Section: Resultsmentioning
confidence: 99%
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“…Acidification is also an indirect consequence of the increase in the concentration of sulfate in the soil solution (Rosado et al, 2014). Oliveira et al (2014) found decrease in the pH of electronegative soils up to 10 cm from the location of potassium chloride (KCl) granules; this decrease in pH was mainly attributed to increase in the density of electric charges at the surface of the electronegative colloids of the soils, due to the increase in electrolytic concentration, releasing ions of an acidic nature to the soil solution.…”
Section: Resultsmentioning
confidence: 99%
“…Ali et al (2014) showed that rates of application of single superphosphate (from zero to 150 kg ha -1 P 2 O 5 ) in soil with pH(H 2 O) of 7.73 brought about a reduction of 0.17 units of pH for every 100 kg P 2 O 5 applied. The reduction in soil pH was attributed to release of H + ions derived from the chemical equilibrium reaction between the two main soluble forms of phosphate (H 2 PO 4 -+ H 2 O= HPO 4 2-+ H + ), whose acid dissociation constant is 6.2 × 10 -8 , which results in a pK a (potential of the dissociation constant) of 7.21 (Oliveira et al, 2014). In our study, soil pH was greater than 7.21 ( Figure 3); thus, the equilibrium reaction brings about predominance of HPO 4 2and the release of H + ions in the soil solution after fertilization with single superphosphate.…”
Section: Resultsmentioning
confidence: 99%
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