Department of Soil Science, Himachal Pradesh Agricultural University, Patampur, Himachal Pradesh, 176062
In a study on phosphate diffusion from 32P labelled KH2PO4 in sixteen Himalayan mid-hill soils, it was found that the P diffusion coefficient (PBC) varied from 10.5xl0-8 to 68 85 x 10−8 cm2/sec with an average value of 24.63 x 10−8 cm2/sec. The soil factors that significantly influenced the diffusion coefficient in a bivariate correlation analysis were surface area, clay content, Al-P and free iron. In multiple regression analysis, the variation in PDC due to surface area, Al-P and free iron could be explained to the extent of 66.9% with 45.4% being the share of surf ace area alone. Thus, surface area, Al-P and free iron were found to be the important factors influencing phosphate diffusion in mid-hill soils of Himalayan region in north-west India, the first one being the most important among the three.
Phosphate diffusion, soil factors, surface area, Himalayan soils