Effects of temperature and water content on degradation of isoproturon in three soil profiles
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 p...
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Published in | Chemosphere (Oxford) Vol. 64; no. 7; pp. 1053 - 1061 |
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Main Authors | , , , |
Format | Journal Article |
Language | English |
Published |
Oxford
Elsevier Ltd
01.08.2006
Elsevier |
Subjects | |
Online Access | Get full text |
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Summary: | 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. |
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Bibliography: | http://dx.doi.org/10.1016/j.chemosphere.2005.12.004 ObjectType-Article-2 SourceType-Scholarly Journals-1 ObjectType-Feature-1 content type line 23 ObjectType-Article-1 ObjectType-Feature-2 |
ISSN: | 0045-6535 1879-1298 |
DOI: | 10.1016/j.chemosphere.2005.12.004 |