2015
DOI: 10.3329/sja.v13i1.24176
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Phosphorus sorption characteristics of some representative soils of south India

Abstract: Studies were conducted to investigate P sorption characteristics of representative soils from ten locations of alfisol and ultisol of India using Langmuir and Freundlich equations. The P sorption maxima (b) of soils derived from Langmuir equation in alfisol varied from 520.6 to 574.7 µg g -1 and ultisol varied from 561.6 to 678.1 µg g -1.The maximum phosphorus buffering capacity (MPBC) in alfisol ranged from 80.7 to 180.2 ml µg -1 and ultisol ranged from 162.1 to 284.4 ml µg ) was significantly correlated with… Show more

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Cited by 9 publications
(7 citation statements)
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“…is is consistent with Rashmi et al [31], who showed that the P sorbed and equilibrium P concentrations increased with increasing P addition. e results indicate that both the Freundlich and Langmuir P sorption models were well fitted as evidenced by higher R 2 and lower SE values.…”
Section: Discussionsupporting
confidence: 92%
“…is is consistent with Rashmi et al [31], who showed that the P sorbed and equilibrium P concentrations increased with increasing P addition. e results indicate that both the Freundlich and Langmuir P sorption models were well fitted as evidenced by higher R 2 and lower SE values.…”
Section: Discussionsupporting
confidence: 92%
“…At low concentration, the relationship was linear, whereas it deviated from linearity at high concentrations. The linearity between equilibrium P concentrations versus rate of P sorbed was due to large intermolecular distance between P ions resulting in negligible mutual repulsion, whereas the deviation from linearity indicates the decrease in the binding affinity of soil to P with increasing surface saturation with P (Rashmi et al., 2015).…”
Section: Resultsmentioning
confidence: 99%
“…At low concentration, the relationship was linear, whereas it deviated from linearity at high concentrations. The linearity between equilibrium P concentrations versus rate of P sorbed was due to large intermolecular distance between P ions resulting in negligible mutual repulsion, whereas the deviation from linearity indicates the decrease in the binding affinity of soil to P with increasing surface saturation with P(Rashmi et al, 2015).The P sorption data were adequately fitted with the model according to the Freundlich and Langmuir equations for the three soils of the study sites. The data showed satisfactory agreements with both Freundlich (R 2 > 0.90) and Langmuir (R 2 > 0.95) equations.…”
mentioning
confidence: 95%
“…The availability of P element for plants is often limited since the majority of the elements are insoluble form. Rashmi et al (2015) stated that Langmuir and Freundlich's model was acceptable to describe phosphate ion absorption on soil colloid surface where the presence of clay. Al and Fe elements guided the capacity of ion absorption by soil colloid.…”
Section: Discussionmentioning
confidence: 99%