Department of Soil Science and Agricultural Chemistry, Rajendra Agricultural University, Pusa, Samastipur, Bihar, 848125.
The kinetics of reactions of Fe-FA1 (Comp.), Fe-FA2 (PM); Fe-FA3 (SS); Fe-FA4 (PR) and Fe-FA5 (BGs) with calcareous soil conformed to first order reaction. The rate constants (K) of displacement of Fe from Fe-FA1; Fe-FA2, Fe-FA3; Fe-FA4 and Fe-Fa5 were 0.0049, 0.0062, 0.0019, 0.0028, 0.0016 h−1, respectively in a calcareous soil. A plot of concentration of Fe-fulvate, Cu-fulvate, Zn-fulvate vs l-eks gave a linear relationship, indicating that Fefulvates reactions in a calcareous soil obey the pseudo-parallel first order kinetics. Agreement between the value of overall rate constant of Fe displacement from iron fulvate and summation of formation of Ca-fulvate (K2), Zn-fulvate (K3) and Cu-fulvate (K4) as predicted by the proposed kinetic model was excellent. The calculated diffusion coefficient of iron during its movement into the soil matrixfalls in/he order: Fe-FA2 > Fe-FA4 > Fe-FA1 > Fe-FA3 > Fe-FA5.
Iron-fulvates, calcareous soil, first-order reaction, kinetic model