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Degradation and Field Persistence of Imazethapyr
153
Citations
7
References
1990
Year
EngineeringDegradation ReactionOrganic ChemistryOrganic GeochemistryEnvironmental ChemistryChemical EngineeringField PersistenceMicrobial EcologyToxicologyEnvironmental MicrobiologySoil MicrobiologySoil MoisturePhotosynthesisBiogeochemistryCo 2EcotoxicologyEnvironmental FateEnvironmental EngineeringSoil ChemistryMedicineMicrobiological Degradation
The volatilization, photolysis, microbial degradation, and field persistence of imazethapyr were studied using formulated and 14 C-labeled imazethapyr. Volatilization losses from soil were less than 2%. Photodecomposition losses of up to 8% occurred from soil and up to 52% from a glass slide with no soil. Significantly greater photodecomposition occurred with chain-labeled than ring-labeled 14 C-imazethapyr. The amount of 14 CO 2 evolution from soil treated with either ring- or chain-labeled 14 C-imazethapyr was not significantly different. The total 14 CO 2 evolved from the soils ranged from 2.4 to 3.6% of the total 14 C-imazethapyr applied to the soil. However, degradation of imazethapyr from the same soils, as determined by high-pressure liquid chromatography, indicated that 62 to 82% of the applied 14 C-imazethapyr had been degraded. The degradation rate increased as soil moisture was increased from −100 to −33 kPa. Imazethapyr was more persistent in soil with the higher clay and organic matter content.
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