Gooddy, D.C.; Harrison, I.; Allen, D.; Carlick, C.; Chilton, P.J.. 2002 A field study to determine the fate of diuron and its metabolites in calcareous sediments. British Geological Survey, 26pp. (IR/02/022) (Unpublished)
Abstract
An experimental plot has been established on a calcareous soil in southern England to investigate
the fate and transport of diuron (N`-[3,4-dichlorophenyl]-N,N-dimethylurea), a commonly used
phenylurea herbicide. In early January 2001 an agricultural grade of diuron was applied to the
soil surface at a rate of 6.7 kg/ha along with a potassium bromide conservative tracer applied at
200 kg/ha. Hand augured samples were taken at regular intervals over the next 50 days, and then
again after 338 days, with samples collected down to 54 cm. Porewaters were extracted from the
soil cores by using high speed centrifugation and the supernatant fluids were retained for
analysis by HPLC for diuron and three of its metabolites, N`-[3,4-dichlorophenyl]-N,Nmethylurea
(DCPMU), N`-3,4-dichlorophenylurea (DCPU) and 3,4-dichloroaniline (DCA). The
centrifuged soil was retained and then extracted with methanol prior to HPLC analysis for the
same suite of phenylureas. A mass balance approach showed large variations in diuron
distribution but on average accounted for 104% of the diuron applied. Concentrations of diuron
and its metabolites were roughly five times higher in the soil than in the soil porewaters. After 50
days metabolites comprised 10% of the total diuron present in the porewater and 20% of the total
diuron sorbed to the soil matrix. After 36 days a large pulse of diuron and DCPMU appeared in
the porewaters and soil matrix at a depth of 54 cm, travelling an average of 0.15 cm/d faster than
Br. A preferential route for diuron transport is suggested. There is evidence to suggest that
degradation occurs at depth as well as at the soil surface. Metabolites generally appear to move
more slowly than the parent compound. All metabolites were encountered but interpreting
transport and degradation processes simultaneously proved beyond the capability of the study.
Diuron was detected once in a shallow (5 m) observation well situated on the experimental plot.
High concentrations of diuron and metabolites were still present in the soil and soil solutions
after 50 days. After 338 days diuron was absent from the porewaters but still resided in the solid
phase. The metabolite DCPU became the dominant compound in the soil solution whereas
DCPMU was dominant in the sorbed phase. Both compounds remained as a source of potential
groundwater contamination.
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