Release of non-exchangeable potassium in some acidic Terai soils of himalayan floodplain Singh N.K., Banik G.C.*, Mukhopadhyay D., Patra A.1 Department of Soil Science and Agricultural Chemistry, Faculty of Agriculture, Uttar Banga Krishi Viswavidyalaya, Pundibari, Cooch Behar, 736165, West Bengal 1Present address: Department of Soil Science and Agricultural Chemistry, Institute of Agricultural Sciences, Banaras Hindu University, Varanasi, 221005, Uttar Pradesh *Corresponding author Email: gcbanik79@yahoo.co.in
Online published on 23 March, 2021. Abstract Non-exchangeable potassium (K) reserve and its release pattern is an important issue to optimize the Kfertilization for crops in long-term. The non-exchangeable K release in terms of Step-K and Constant rate-K was measured by repeated extraction of soil with boiling 1 N HNO3 in surface (0-20 cm) and sub-surface (20-40 cm) soil of six different blocks of Cooch Behar district situated in Himalayan floodplain of northern part of West Bengal. The non-exchangeable K content was found adequate in surface soils. Step-K and Constant rate-K were dependent on organic carbon, CEC and soil texture. The cumulative release of nonexchangeable K showed semi-logarithmic behaviour with increasing number of extractions with a highly significant correlation coefficient and suggested the progressive decrease in release of non-exchangeable K with sequential extraction. The threshold-K level for release of intermediate K and Gapon constant (KG) of surface soils were found to vary with the change of background electrolyte concentration for all soils and suggests the tenacity with which K is specifically held in the wedge zones of the clays present in these soils. Top Keywords Activity ratio, Constant rate-K, Step-K, Specifically held K, Threshold value. Top |