Interaction between uranium and humic acid (Ⅱ): complexation, precipitation and migration behavior of U(Ⅵ) in the presence of humic substances

The complexation, precipitation, and migration behavior of uranium in the presence of humic acid (HA) or fulvic acid (FA) were investigated by cation exchange, ultrafiltration and dynamic experiment, respectively. The results showed that (i) complex equilibrium between the uranium and humic substances was achieved at approximately 72 h, (ii) the coordination number varied from 1:1 to 1:2 ( U(Ⅵ) : humic acid) as pH increased from 3 to 6; and (iii) , while the complex stability constant decreased when temperature increased, but increased with pH value. We found that the precipitation of uranyl could only be observed in presence of HA, and the precipitation was influenced by conditions, such as pH, uranium concentration, temperature, and the HA concentration. The maximum precipitation proportion up to 60% could be achieved in the condition of 40 mg/L HA solution at pH 6. We further observed that the migration behavior of uranium in soil in the presence of humic acid (HA) or fulvic acid (FA) was different from that in the presence of inorganic colloid, and the effect of humic substances (HS) was limited.

The complexation, precipitation, and migration behavior of uranium in the presence of humic acid （HA） or fulvic acid （FA） were investigated by cation exchange, ultrafiltration and dynamic experiment, respectively. The results showed that （i） complex equilibrium between the uranium and humic substances was achieved at approximately 72 h, （ii） the coordination number varied from l：l to 1：2 （U（VI） ： humic acid） as pH increased from 3 to 6; and （iii） , while the complex stability constant decreased when temperature increased, but increased with pH value. We found that the precipitation of uranyl could only be observed in presence of HA, and the precipitation was influenced by conditions, such as pH, uranium concentration, temperature, and the HA concentration. The maximum precipitation proportion up to 60% could be achieved in the condition of 40 mg/L HA solution at pH 6. We further observed that the migration behavior of uranium in soil in the presence of humic acid （HA） or fulvic acid （FA） was different from that in the presence of inorganic colloid, and the effect of humic substances （HS） was limited,