Phosphate Associated Cadmium Immobilization Mechanism Depending on the Original Concentration of Cd in Soil
Hyun Ho Lee, Chang Oh Hong
Abstract
Hyun Ho Lee, Chang Oh Hong
Abstract
Adsorption and precipitation of cadmium (Cd) could be dependent on rate of P addition and Cd level in soil. Therefore, the objective of this study was to examine how addition rate of P affect mechanisms of Cd immobilization such as adsorption and precipitation in different levels of Cd in soil. Arable soils were spiked with inorganic Cd (CdCl₂) to give a total Cd concentration of 10, 100, and 1,000 mg Cd kg -1 . Monopotassium phosphate (KH₂PO₄, MPP) was selected as phosphate material and mixed with the pretreated arable soil at the rates of 0, 800, 1,600 and 3,200 mg P kg-1. The mixture soils were incubated at 25°C for 8 weeks in dark condition. Soil pH decreased with increasing MPP addition rate in all levels of Cd but negative charge of soil increased, thereby reducing 1 M NH₄OAc extractable Cd. Soil solutions were undersaturated with respect to CdCO₃ and Cd₃(PO₄)₂ with all P addition rate in soil with low Cd level (≤ 100 mg Cd kg-1) but supersaturated in soil with high Cd level (1,000 mg Cd kg-1). From the above results, Cd solubility was controlled by precipitation of Cd minerals such as CdCO₃ and Cd₃(PO₄)₂ in soil with high Cd level but by Cd adsorption induced by increase in negative charge of soil with low level of Cd.
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Adsorption and precipitation of cadmium (Cd) could be dependent on rate of P addition and Cd level in soil. Therefore, the objective of this study was to examine how addition rate of P affect mechanisms of Cd immobilization such as adsorption and precipitation in different levels of Cd in soil. Arable soils were spiked with inorganic Cd (CdCl₂) to give a total Cd concentration of 10, 100, and 1,000 mg Cd kg -1 . Monopotassium phosphate (KH₂PO₄, MPP) was selected as phosphate material and mixed with the pretreated arable soil at the rates of 0, 800, 1,600 and 3,200 mg P kg-1. The mixture soils were incubated at 25°C for 8 weeks in dark condition. Soil pH decreased with increasing MPP addition rate in all levels of Cd but negative charge of soil increased, thereby reducing 1 M NH₄OAc extractable Cd. Soil solutions were undersaturated with respect to CdCO₃ and Cd₃(PO₄)₂ with all P addition rate in soil with low Cd level (≤ 100 mg Cd kg-1) but supersaturated in soil with high Cd level (1,000 mg Cd kg-1). From the above results, Cd solubility was controlled by precipitation of Cd minerals such as CdCO₃ and Cd₃(PO₄)₂ in soil with high Cd level but by Cd adsorption induced by increase in negative charge of soil with low level of Cd.
Key concepts: Phosphate, Cadmium, Chemistry, Mechanism (biology), Environmental chemistry, Biochemistry, Philosophy, Organic chemistry