摘要
The kinetic characteristics of P adsorption and desorption by organo-mineral colloidal complexes (OMC)were studied using acid, calcareous and neutral purple paddy soils taken from Chongqing and Sichuan, China.The results showed that the P adsorption capacity of the organo-mineral colloidal complexes differed with the soil types, being higher for the acid and calcareous purple soils than for the neutral purple soils. Partial removal of the organic matter increased the adsorption capacity of the colloidal complexes. A very significant positive correlation was found between the amounts of P desorbed from OMC and the P saturation degrees.The P adsorption reaction was quick at the early stage and slowed later. The raise of temperature increased P adsorption capacity and P adsorption rate of the colloidal complexes. The adsorption processes could be described by the Elovich equation.
The kinetic characteristics of P adsorption and desorption by organo-mineralcolloidal complexes (OMC) were studied using acid, calcareous and neutral purple paddy soils takenfrom Chongqing and Sichuan, China. The results showed that the P adsorption capacity of theorgano-mineral colloidal complexes differed with the soil types, being higher for the acid andcalcareous purple soils than for the neutral purple soils. Partial removal of the organic; matterincreased the adsorption capacity of the colloidal complexes. A very significant positivecorrelation was found between the amounts of P desorbed from OMC and the P saturation degrees. The Padsorption reaction was quick at the early stage and slowed later. The raise of temperatureincreased P adsorption capacity and P adsorption rate of the colloidal complexes. The adsorptionprocesses could be described by the Elovich equation.
基金
the Applied Science Foundation of the Science and Technology Commission of Chongqing,China.
