Clay Research
  • Year: 2006
  • Volume: 25
  • Issue: 1

A study on sorption and desorption kinetics of potassium in some selected surface soils of West Bengal

  • Author:
  • Sourov Chatterjee, S. K. Sanyal
  • Total Page Count: 22
  • Page Number: 23 to 44

Department of Agricultural Chemistry and Soil Science, Bidhan Chandra Krishi Viswavidyalaya, Mohanpur, Nadia, West Bengal - 741252

*Present address: Director of Research, Bidhan Chandra Krishi Viswavidyalaya, Kalyani, Nadia, West Bengal - 741 235

Abstract

Five surface soils of different agro-climatic zones of West Bengal with varying potassium supplying power and different clay mineralogical make-up were characterized in terms of relevant physico-chemical properties and various forms of soil K. The K sorption and desorption kinetics in these soils were examined by using the batch technique. The K sorption and desorption kinetic data in the present soils at two temperatures, were fitted to several kinetic models. The K adsorption and desorption rate coefficient (ka and kd, respectively) were computed from the respective first-order kinetic equations. The ka values were the highest and the lowest for the Kalyani and the Abas soils, respectively. The kd values, on the other hand, were the highest and the lowest for the Abas and the Polba soils, respectively. These ka and kd values were well related with the nature and the content of the clay minerals of the given soils. The activation energy for K desorption (Ed) was higher than the corresponding activation energy for K adsorption (Ea) in case of the Kalyani and the Karbala soils, and the reverse was true for the Abas, Polba and Digha soils. The standard free energy change of K adsorption at mean temperature (ΔG0mean), standard enthalpy change of K adsorption at mean temperature (ΔH0mean), standard entropy change of K adsorption at mean temperature (ΔS0mean) were determined from the first-order sorption-desorption kinetic data and were correlated with the relevant soil properties. A comparison among different kinetic equations with the aid of the standard error of estimate (S.E.) and the coefficient of determination (R2) values indicated that the parabolic diffusion and the power-function equations described the adsorption and desorption kinetics of K of the soils equally well as did the first-order kinetic equations. The constants of different kinetic equations were computed and interrelated. The Elovich and the zero-order kinetic equations were less successful in the present study.