2000•Journal of the Indian Society of Soil ScienceOpen access

Non-exchangeable Potassium Reserves and their Release Pattern in Some Alfisols and Inceptisols of West Bengal

Arabinda Dhar, S.K. Sanyal

Open full text 6 citations

Abstract

A study was conducted to characterise the non-exchangeable K reserves in three Alfisols and two Inceptisols of West Bengal. The reserves of step-K and constant rate K were evaluated by repeated extraction of soils with boiling molar nitric acid. The reserves of step-K content were, in general, related to the content of the clay fraction of the soils. The cumulative release of non-exchangeable K by repeated extraction with boiling 1 M HNO3 followed a semi-logarithmic behaviour with increasing number of extractions, suggesting that the release of non-exchangeable K decreased with successive number of extractions. The threshold levels of K in soil solution below which the release of K from the initially non-exchangeable K reserve starts were also evaluated for the given soils in terms of the K-activity ratio, K-concentration and exchangeable K in 0.01 M and 0.002 M CaCl2 solution. These threshold values registered change with the change of background electrolyte concentration. Specifically held K, determined as exchangeable K below which the Gapon constant (KG) showed a sharp rise, varied from soil to soil in almost the same manner as noted for threshold K levels in these soils. These trends have been related to the properties of the soils, especially their clay make-up.

About this research paper

What this paper is about

A study was conducted to characterise the non-exchangeable K reserves in three Alfisols and two Inceptisols of West Bengal. The reserves of step-K and constant rate K were evaluated by repeated extraction of soils with boiling molar nitric acid. The reserves of step-K content were, in general, related to the content of the clay fraction of the soils. The cumulative release of non-exchangeable K by repeated extraction with boiling 1 M HNO3 followed a semi-logarithmic behaviour with increasing number of extractions, suggesting that the release of non-exchangeable K decreased with successive number of extractions. The threshold levels of K in soil solution below which the release of K from the initially non-exchangeable K reserve starts were also evaluated for the given soils in terms of the K-activity ratio, K-concentration and exchangeable K in 0.01 M and 0.002 M CaCl2 solution. These threshold values registered change with the change of background electrolyte concentration. Specifically held K, determined as exchangeable K below which the Gapon constant (KG) showed a sharp rise, varied from soil to soil in almost the same manner as noted for threshold K levels in these soils. These trends have been related to the properties of the soils, especially their clay make-up.

Why it matters

OpenAlex reports 6 citations for this work. Citation counts describe recorded attention and do not establish research quality.

Key contribution

A contribution statement is not available in the OpenAlex record.

Method / approach

Method details are not available in the OpenAlex metadata.

Main findings

Findings are not separately available in the OpenAlex metadata.

Limitations

Limitations are not available in the OpenAlex metadata.

Applications

Application details are not available in the OpenAlex metadata.

Available abstract

A study was conducted to characterise the non-exchangeable K reserves in three Alfisols and two Inceptisols of West Bengal. The reserves of step-K and constant rate K were evaluated by repeated extraction of soils with boiling molar nitric acid. The reserves of step-K content were, in general, related to the content of the clay fraction of the soils. The cumulative release of non-exchangeable K by repeated extraction with boiling 1 M HNO3 followed a semi-logarithmic behaviour with increasing number of extractions, suggesting that the release of non-exchangeable K decreased with successive number of extractions. The threshold levels of K in soil solution below which the release of K from the initially non-exchangeable K reserve starts were also evaluated for the given soils in terms of the K-activity ratio, K-concentration and exchangeable K in 0.01 M and 0.002 M CaCl2 solution. These threshold values registered change with the change of background electrolyte concentration. Specifically held K, determined as exchangeable K below which the Gapon constant (KG) showed a sharp rise, varied from soil to soil in almost the same manner as noted for threshold K levels in these soils. These trends have been related to the properties of the soils, especially their clay make-up.

Key concepts: Inceptisol, Soil water, West bengal, Chemistry, Potassium, Extraction (chemistry), Cation-exchange capacity, Alfisol

Related papers

Back to paper searchBrowse research topicsOriginal source
Non-exchangeable Potassium Reserves and their Release Pattern in Some Alfisols and Inceptisols of West Bengal — Research Paper | ScholarLens