The fate of methiozolin under anaerobic conditions was
investigated
in clay loam with a high organic carbon content and sandy loam with
a low carbon content using [dihydroisoxazole ring-14C]
and [phenyl-14C] radiolabels. The sediment/water ratio
was 1:3 based on the dry weight:volume (w/v) ratio; the incubations
lasted up to 355 days after the treatment (DAT) and were performed
in the dark at 20.4 ± 0.7 °C. The overlying water flow-through
systems consisted of glass vessels containing sediment with traps
for [14C]carbon dioxide and [14C]volatiles.
The samples were collected and analyzed at 0, 3, 7, 14, 50, 100, 200,
and 355 DAT. The water and sediment samples were extracted with solvent
systems, centrifuged, concentrated, and analyzed by liquid scintillation
counting and a high-performance liquid chromatography (HPLC) system
equipped with a flow scintillation analyzer. Following extraction,
the sediments were air-dried, and the subsamples were combusted. [14C]Methiozolin was degraded in the water phase and partitioned
rapidly into the sediments, where it was further degraded to other
metabolites, which were identified by HPLC and liquid chromatography-
or gas chromatography-tandem mass spectrometry (MS/MS) with authentic
standards. The dissipation of methiozolin from the overlying water
was rapid (with half-lives of 1.1–1.8 and 3.6–4.9 days
in the clay loam and sandy loam, respectively). However, methiozolin
dissipation from the sediment phase and the whole system was much
slower than from the water phase (with half-lives of 122.0–220.0
and 110.0–130.0 days in the sediment phase of the clay loam
and sandy loam and 116.0–166.0 and 70.8–85.7 days in
the whole system of the clay loam and sandy loam, respectively).