摘要
The phenylurea herbicide isoproturon, 3-(4-isopropylphenyl)-1,1-dimethylurea (IPU), is widely used to control pre- and post-emergence of grass and broad-leaved weeds in cereal crops. Its degradation in soils is a key process for assessing its leaching risk to groundwater resources. The degradation properties of various samples from surface and subsurface soil (down to 1 m depth) of a heterogeneous agricultural field were studied using 14C-IPU. Laboratory incubations were carried out at 22 and 10 °C and at water contents 90 % and 50 % of the estimated water holding capacity (eWHC) corresponding to water potentials between −56 kPa and −660 MPa. Degradation was found to be more sensitive to water content variations than to temperature variations in the ranges that we used. For surface layers, at 10 and 22 °C, the degradation half-life increased by a factor 10 and 15, respectively, when water content decreased from 90 % to 50 % eWHC. Under optimal degradation conditions (i.e. 22 °C and 90 % eWHC), 3-(4-isopropylphenyl)-1-methylurea (MDIPU) was the main metabolite in surface samples. At subsurface depths, IPU half-lives were larger than 100 d, IPU was the main compound after 92 d of incubation and the main metabolite was an unidentified polar metabolite. These results suggest a metabolic pathway involving hydroxylations for subsurface materials. IPU degradation was largely affected by water availability in both surface and subsurface horizons. Clay content seemed to play a major role in degradation processes in subsurface soil by determining through sorption IPU availability in soil solution and/or by limiting water availability for microorganisms.