2006•Journal of the Indian Society of Soil ScienceOpen access

Effect of pH and lime on sulphate adsorption in some Alfisols of Orissa

Prosad Kumar Das, S.K. Sahu, Debasis Sarangi

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Abstract

Effect of pH and lime on sulphate adsorption was investigated in five Alfisols of Orissa. Sulphate adsorption decreased with increase in equilibrium pH of the SO42− solutions added. Distribution coefficient of SO42−-S decreased sharply with increase in equilibrium pH indicating that the SO42− adsorption in these soils was highly pH-dependent. Liming the soils by Woodruff's buffer method increased the pH in different soils ranging between 7.3 and 8.1 and caused a drastic reduction in SO42− adsorption varying from 60 to 93.5% in different soils. There were significant reductions in Freundlich K, Langmuir adsorption maxima, equilibrium buffering capacity and maximum buffering capacity of the soils after liming.

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Effect of pH and lime on sulphate adsorption was investigated in five Alfisols of Orissa. Sulphate adsorption decreased with increase in equilibrium pH of the SO42− solutions added. Distribution coefficient of SO42−-S decreased sharply with increase in equilibrium pH indicating that the SO42− adsorption in these soils was highly pH-dependent. Liming the soils by Woodruff's buffer method increased the pH in different soils ranging between 7.3 and 8.1 and caused a drastic reduction in SO42− adsorption varying from 60 to 93.5% in different soils. There were significant reductions in Freundlich K, Langmuir adsorption maxima, equilibrium buffering capacity and maximum buffering capacity of the soils after liming.

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Available abstract

Effect of pH and lime on sulphate adsorption was investigated in five Alfisols of Orissa. Sulphate adsorption decreased with increase in equilibrium pH of the SO42− solutions added. Distribution coefficient of SO42−-S decreased sharply with increase in equilibrium pH indicating that the SO42− adsorption in these soils was highly pH-dependent. Liming the soils by Woodruff's buffer method increased the pH in different soils ranging between 7.3 and 8.1 and caused a drastic reduction in SO42− adsorption varying from 60 to 93.5% in different soils. There were significant reductions in Freundlich K, Langmuir adsorption maxima, equilibrium buffering capacity and maximum buffering capacity of the soils after liming.

Key concepts: Adsorption, Lime, Soil water, Langmuir, Chemistry, Freundlich equation, Alfisol, Soil pH

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