Department of Soil Science, CCS Haryana Agricultural University, Hisar, 125 004, Haryana
*Corresponding author (Email: tchand@hau.ernet.in)
Laboratory investigation was carried out to study the effect of CaCO3 and clay on phosphate sorption by calcareous soils. Three surface soil samples (0–0.15m) representing; Typic Camborthid, Typic Haplustepts and varying in CaCO3 and clay were collected. The samples of each soil were equilibrated for 48 hrs at 25±2°C with aqueous solution of NaH2PO4 containing (0–465 µg P mL−1) in a 1:20 soil: solution ratio. The amount of phosphate sorbed (x/m), per cent of added phosphate sorbed (XAd) and distribution coefficient (Kd) increased with increasing CaCO3 content of the soils. The x/m increased whereas, XAd and Kd decreased with increasing concentrations of P in solution phase. The phosphate sorption was satisfactorily (r2=0.98 to 0.99, P=0.01) described by Freundlich equation. The Freundlich ‘k’ and ‘n’ increased with increasing CaCO3 content of soils. Removal of CaCO3 from soil decreased the x/m, XAd, Kd, ‘k’ and ‘n’. The magnitude of decrease in P sorption parameters varied with CaCO3 content of the soils. In different soils, CaCO3 contributed 11.3 to 59.7% and clay 17.9 to 53.8% to the total P sorption at different solution P concentrations. However, the effect of clay content of soils and solution P concentration on contribution of clay to phosphate sorption was not consistent.
CaCO3, clay, phosphate sorption, Freundlich equation, calcareous soils