摘要
The adsorption characteristics of Pb on sediments of the Dianshan Lake in Shanghai was studied. The results show that (1) the relationship between the amount q of apparent equilibrium adsorption and the equilibrium concentration C conforms to the Freundlich isothermal adsorption equation; (2) the adsorption and desorption of Pb on sediments are not reversible, that is, adsorption/desorption of Pb exhibits hysteresis; (3) Pb adsorption behavior is initially fast, followed by a slow reaction, and the slow reaction conforms to a reversible first-order reaction; (4) by deducing the Pb adsorption kinetics, four kinetics parameters n,k 1,k 2,q (max) independent of C could be worked out; (5) the equilibrium parameter (K) and the free energy change (ΔG) could also be determined, and the negative values of free energy change (ΔG) indicate the spontaneous nature of the adsorption.
The adsorption characteristics of Pb on sediments of the Dianshan Lake in Shanghai was studied. The results show that (1) the relationship between the amount q of apparent equilibrium adsorption and the equilibrium concentration C conforms to the Freundlich isothermal adsorption equation; (2) the adsorption and desorption of Pb on sediments are not reversible, that is, adsorption/desorption of Pb exhibits hysteresis; (3) Pb adsorption behavior is initially fast, followed by a slow reaction, and the slow reaction conforms to a reversible first-order reaction; (4) by deducing the Pb adsorption kinetics, four kinetics parameters n,k 1,k 2,q (max) independent of C could be worked out; (5) the equilibrium parameter (K) and the free energy change (ΔG) could also be determined, and the negative values of free energy change (ΔG) indicate the spontaneous nature of the adsorption.
基金
ProjectsupportedbytheScienceFoundationofShanghaiMunic ipalCommissionofEducation (GrantNo .0 0QG14 0 0 3 )
