The fate of
14C-labeled sulfadiazine (
14C-SDZ) residues was studied in time-course experiments for 218 days of incubation using two soils (A
p horizon of loamy sand, orthic luvisol; A
p horizon of silt loam, cambisol) amended with fresh and aged (6 months)
14C-manure [40 g kg
?1 of soil; 6.36 mg of sulfadiazine (SDZ) equivalents per kg of soil], which was derived from two shoats treated with
14C-SDZ. Mineralization of
14C-SDZ residues was below 2% after 218 days depending little on soil type. Portions of extractable
14C (ethanol-water, 9:1, v/v) decreased with time to 4–13% after 218 days of incubation with fresh and aged
14C-manure and both soils. Non-extractable residues were the main route of the fate of the
14C-SDZ residues (above 90% of total recovered
14C after 218 days). These residues were high immediately after amendment depending on soil type and aging of the
14C-manure, and were stable and not remobilized throughout 218 days of incubation. Bioavailable portions (extraction using CaCl
2 solution) also decreased with increasing incubation period (5–7% after 218 days). Due to thin-layer chromatography (TLC), 500 μg of
14C-SDZ per kg soil were found in the ethanol-water extracts immediately after amendment with fresh
14C-manure, and about 50 μg kg
?1 after 218 days. Bioavailable
14C-SDZ portions present in the CaCl
2 extracts were about 350 μg kg
?1 with amendment. Higher concentrations were initially detected with aged
14C-manure (ethanol-water extracts: 1,920 μg kg
?1; CaCl
2 extracts: 1,020 μg kg
?1), probably due to release of
14C-SDZ from bound forms during storage. Consistent results were obtained by extraction of the
14C-manure-soil samples with ethyl acetate; portions of N-acetylated SDZ were additionally determined. All soluble
14C-SDZ residues contained in
14C-manure contributed to the formation of non-extractable residues; a tendency for persistence or accumulation was not observed. SDZ's non-extractable soil residues were associated with the soluble HCl, fulvic acids and humic acids fractions, and the insoluble humin fraction. The majority of the non-extractable residues appeared to be due to stable covalent binding to soil organic matter.
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