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Adsorption of Acid Phosphatase on Minerals and Soil Colloids in Presence of Citrate and Phosphate 被引量:2

Adsorption of Acid Phosphatase on Minerals and Soil Colloids in Presence of Citrate and Phosphate
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摘要 The aim of this work was to study the influence of phosphate and citrate, which are common inorganic and organic anions in soils, on the adsorption of acid phosphatase by kaolin, goethite and the colloids separated from yellow-brown soil (YBS) and latosol (LS) in central-south China. The YBS colloid has the major clay mineral composition of 1.4 nm mineral, illite and kaolinite while the LS colloid mainly contains kaolinite and oxides. The adsorption isotherm of acid phosphatase on the examined soil colloids and minerals fitted to the Langmuir model. The amount of enzyme adsorbed in the absence of ligands was in the order of YBS colloid > LS colloid > kaolin ≈ goethite. In the presence of phosphate or citrate, the amounts of the enzyme adsorbed followed the sequence YBS colloid > kaolin > LS colloid > goethite. The presence of ligands also decreased the binding energy between the enzyme and soil colloids or minerals. With the increase of ligand concentration from 10 mmol L-1 to 400 m mol L-1, different behaviors for the adsorption of enzyme were found in the colloid and mineral systems studied. A sharp decrease in enzyme adsorption was observed on goethite while gradual decreases of enzyme adsorption were recorded in the two soil colloid systems. However, no any decrease was found for the amount of enzyme adsorbed on kaolin at higher ligand concentrations. When phosphate or citrate was introduced to the system before the addition of enzyme, the ligands usually enhanced the adsorption of enzyme. The results obtained in this study suggested the important role of kaolinite mineral in the adsorption of enzyme molecules in acidic soils in the presence of various ligands. The aim of this work was to study the influence of phosphate and citrate,which are common inorganic and organic anions in soils,on the adsorption of acid phosphatase by kaolin,goethite and the colloids separated from yellow-brown soil(YBS)and latosol(LS)in central-south China.The YBS colloid has the major clay mincral composition of 1.4 nm mincral,illite and kaolinite while the LS colloid mainly contains kaolinite and oxides.The adsorption isotherm of acid phosphatase on the examined soil colloids and minerals fitted to the Langmuir model.The amount of enzyme adsorbed in the absence of ligands was in the order of YBS colloid>LS colloid>kaolin≈goethite.In the presence of phosphate or citrate,the amounts of the enzyme adsorbed followed the sequence YBS colloid>kaolin>LS colloid>goethite.The presence of ligands also decreased the binding energy between the enzyme and soil colloids or minerals.With the increase of ligand concentration from 10mmol L^-1 to 400 m mol L^-1,different behaviors for the adsorption of cnzyme were found in the colloid and mineral systems studied.A sharp decrease in enzyme adsorption was observed on goethite while gradual decreases of enzyme adsorption were recorded in the two soil colloid systems.However,no any decrease was found for the amount of enzyme adsorbed on kaolin at higher ligand concentrations.When phosphate or citrate was introduced to the system before the addition of enzyme,the ligands usually enhanced the adsorption of enzyme.The results obtained in this study suggested the important role of kaolinite mineral in the adsorption of enzyme molecules in acidic soils in the presence of various ligands.
出处 《Pedosphere》 SCIE CAS CSCD 2002年第4期339-348,共10页 土壤圈(英文版)
基金 Project supported by the National Natural Science Foundation of China (No. 49601011) by the International Foundation for Science (IFS, No. C/2527-1).
关键词 acid phosphatase ADSORPTION GOETHITE KAOLIN soil colloid 磷酸盐 柠檬酸盐 土壤 酸性磷酸酶 胶体
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