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Laboratory experiments about the dissipation, adsorption and translocation in four paddy topsoils were conducted in this paper. From the results it can be concluded as follows: the dissipation rate of clomazone differed greatly in different paddy soil derived from different parent materials. The half-lives for clomazone degradation in paddy soils ranged from 5.7 to 22.0 d. The order of clomazone dissipation rate was reddish yellow paddy soil > alluvial sandy paddy soil > yellow clayey paddy soil > purple sandy paddy soil. Clomazone sorption quantity was significantly correlated with organic carbon(R2=0.62) and clay content(R2=0.67) in the tested paddy soils. Positive correlation was found between apparent K d value and cation exchange content(CEC). The consequences for the adsorption of different soils were purple sandy paddy soil>yellow clayey paddy soil>reddish yellow paddy soil>alluvial sandy paddy soil. Under the simulated rainfall of 200 mm through four different unsaturated soil lysimeters over 24 h, clomazone was readily to be leached into lower surface soil and there was about 2.6%—4.2% of applied clomazone leached out of 20 cm cultivated soil layer. Translocation experiments showed that the order of clomazone leaching ability was: alluvial sandy paddy soil > reddish yellow paddy soil > yellow clayey paddy soil > purple sandy paddy soil. Simple regression results manifested that factors like CEC, organic carbon, clay, and adsorption rate constant had been negatively correlated with the percentage of clomazone loss from soil lysimeters.
Laboratory experiments about the dissipation, adsorption and translocation in four paddy topsoils were conducted in this paper. From the results it can be concluded in: the dissipation rate of clomazone differed greatly in different paddy soil derived from different parent materials. The half-lives for clomazone degradation in paddy soils ranged from 5.7 to 22.0 d. The order of clomazone dissipation rate was reddish yellow paddy soil> alluvial sandy paddy soil> yellow clayey paddy soil> purple sandy paddy soil. Clomazone sorption quantity was significantly correlated with organic carbon ( R2 = 0.62) and clay content (R2 = 0.67) in the tested paddy soils. Positive correlation was found between apparent K d value and cation exchange content (CEC). The consequences for the adsorption of different soils were purple sandy paddy soil> yellow clayey paddy soil> reddish yellow paddy soil> alluvial sandy paddy soil. Under the simulated rainfall of 200 mm through four different unsaturated soils lysimeters over 24 h, clomazone was readily to be leached into lower surface soil and there was about 2.6% -4.2% of applied clomazone leached out of 20 cm cultivated soil layer. Translocation experiments showed that the order of clomazone leaching ability was: alluvial sandy paddy soil> reddish yellow paddy soil> yellow clayey paddy soil> purple sandy paddy soil. Simple regression results manifested that factors like CEC, organic carbon, clay, and adsorption rate constant had been negatively correlated with the percentage of clomazone loss from soil lysimeters.