International Journal of Bioresource Science
  • Year: 2017
  • Volume: 4
  • Issue: 1

Distribution of different forms of potassium in some coastal soils of West Bengal

  • Author:
  • Ranajit Panda1, Sanmay Kumar Patra1, Somsubhra Chakraborty2, D.P. Ray3,, Parimal Panda4, Bappa Paramanik5
  • Total Page Count: 12
  • Page Number: 35 to 46

1Bidhan Chandra Krishi Viswavidyalaya, Mohanpur, Nadia, W.B., India

2Agricultural and Food Engineering Department, IIT Kharagpur, Kharagpur, West Bengal, India

3ICAR-National Institute of Research on Jute and Allied Fibre Technology, Kolkata, India

4Uttar Banga Krishi Viswavidyalaya, Cooch Behar, West Bengal, India

5Dakshin Dinajpur Krishi Vigan Kendra, Dakshin, Dinajpur, West Bengal, India

*Corresponding author: drdebprasadray@gmail.com

Online published on 22 June, 2017.

Abstract

The research work with a view to evaluate the status, availability, fixation, releasing and supplying behaviour of potassium for a meaningful K-fertilizer management strategy for sustainable crop production in the coastal soils of West Bengal. Forty surface (0–15 cm) soil samples representing the coastal soils of West Bengal were used for assessing the important physical and physicochemical properties and distribution of different forms of potassium. Total K and lattice K content of the soils were high ranging between 1.0 to 2.74 and 0.93 to 2.60%, respectively. Non-exchangeable, available, exchangeable and water soluble K contents of the soils varied from 534 to 1050, 68.81 to 284.77, 58.65 to 232.50 and 10.16 to 52.27 mg/kg contributing 3.84 to 6.32, 0.53 to 1.23, 0.45 to 1.02 and 0.08 to 0.22% towards total K, respectively. The overall soils were high in available, non-exchangeable and mineral K status. Based on the district wise average values of the different forms of K, the soils were in the order: Medinipur East > North 24 Parganas> South 24 Parganas. Different forms of soil K had highly significant positive correlation with pH and EC. Non-exchangeable K was significantly and positively correlated with organic carbon and CEC. Available K, exchangeable K and water soluble K had significant negative correlation with sand. All the forms of soil potassium were interrelated, indicating the existence of a dynamic equilibrium among them.

Keywords

Structural or mineral K, Available K, Exch. K, Non-exch. K& Water soluble K