Adsorption and Release Behaviors of Phosphate on Sediments in the Upper and Middle Reaches of Yellow River
Beigang Li, Na Gao, Qin Ma
Abstract
Beigang Li, Na Gao, Qin Ma
Abstract
A total of 8 sediment samples collected from the upper and middle reaches of the Yellow River were studied for adsorption and release kinetics,adsorption isotherms,adsorption-desorption equilibrium phosphate concentration,differences among the sediments in adsorption and influences of P forms on P adsorption characteristics in sediments.Results show that both the processes of adsorption and release of phosphate in the sediments completed mainly within the initial 8 h,and the highest adsorption and desorption rates were observed within the first 0.5 h and the reactions basically reached equilibrium in 24 h;P adsorption isotherms accorded with both the linear equation and the Freundlich equation as well as the Langmuir equation(4).Calculation using the Langmuir equation(4),indicate that the maximum P adsorption capacity of the sediments varied from 0.095 to 0.272 mg·g-1,showing significant positive correlations of the capacity with total P(TP),exchangeable loosely-bound phosphorus(Ex-P),and organic matter in the sediments;the sediments have a P adsorption-desorption equilibrium point during adsorbing P in the overlying water,and its corresponding adsorption-desorption equilibrium mass concentration was in the range of 0.009-0.031 mg·L-1,higher than the P concentration in the overlying water,indicating a trend of sediments releasing P to the overlying water.
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A total of 8 sediment samples collected from the upper and middle reaches of the Yellow River were studied for adsorption and release kinetics,adsorption isotherms,adsorption-desorption equilibrium phosphate concentration,differences among the sediments in adsorption and influences of P forms on P adsorption characteristics in sediments.Results show that both the processes of adsorption and release of phosphate in the sediments completed mainly within the initial 8 h,and the highest adsorption and desorption rates were observed within the first 0.5 h and the reactions basically reached equilibrium in 24 h;P adsorption isotherms accorded with both the linear equation and the Freundlich equation as well as the Langmuir equation(4).Calculation using the Langmuir equation(4),indicate that the maximum P adsorption capacity of the sediments varied from 0.095 to 0.272 mg·g-1,showing significant positive correlations of the capacity with total P(TP),exchangeable loosely-bound phosphorus(Ex-P),and organic matter in the sediments;the sediments have a P adsorption-desorption equilibrium point during adsorbing P in the overlying water,and its corresponding adsorption-desorption equilibrium mass concentration was in the range of 0.009-0.031 mg·L-1,higher than the P concentration in the overlying water,indicating a trend of sediments releasing P to the overlying water.
Key concepts: Adsorption, Desorption, Freundlich equation, Chemistry, Phosphate, Langmuir, Sediment, Langmuir equation