Division of Soil Science, S.K. University of Agricultural Sciences and Technology of Kashmir, Shalimar, Srinagar, 191 121, Jammu and Kashmir
*Corresponding author (Email: mushtaqb4u@gmail.com)
Soils of low altitude zone contained lower values of quantity parameters (KL, KX, K0), PBCK and potassium potential than soils of mid and high altitude zones. However, there was no regular pattern in intensity parameters of the soil viz., AReK and -ΔG. Multiple and step down regression analysis revealed positive influence of silt and pH on K adsorbed on non-specific site, negative influence of silt on PBCK and positive on AReK. Among soil attributes, most of the variation was accounted for by silt and pH on KL, K0 and PBCK; silt and EC on K potential; pH, EC and OC on -ΔG. Positive relationship of AReK with K0 and negative with -ΔG indicated that higher intensity was associated with higher quantity and lower energy of K removal. Positive relationship between PBCK and -ΔG indicated that soils low in K supply rate were associated with strongly bound-K.
Q/I parameters, rice soils, lesser Himalayas