Abstract

The transformation of phosphorus in a rice-wheat cropping sequence was studied on alluvial, black, red and laterite soils of India. Phosphorus applied to rice increased Al-P and Fe-P in all soils, R-P in alluvial, black and laterite, and Fe-P and Ca-P in laterite soil only, while it increased native Fe-P in black and red soils. Phosphorus applied to rice and recovered as Al-P was higher after wheat than after rice in alluvial, red and laterite soils. In alluvial and laterite soils, the sum of total inorganic phosphorus fractions in no-P treatment was almost the same after the harvest of rice or wheat, while in black and red soils it was lower after wheat than after rice.

Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call