A BSTRA CT Plant residue and soil depth ejfects on metrihuzin degradation were investigated. Dundee silt loam soil collected at depth increments of0-10 em (SUR) and 10-35 cin (SUB) was treated with labeled Samples were assayed at several time points up to 140 days after treatment. Soybean residue nws added to half of the SUR samples (RES), with remaining SUR unamended (NORES). None of the SUB samples were amended with soybean residue. Metribuzin mineralization to I4CO2 proceeded more slowly in RES and SUB than in NORES and SUR, respectively. Extractable components in SUR samples included polar metabolites, plus deaminated metrihuzin ( D A ) in the RES, and parent metrihuzin in the NORES. Deaminated diketometribuzin (DADK) and metribuzin comprised major I4C components extractedfroni SUB, while in SUR, faster degradation of metabolites resulted in metrirubin as the primary identifiable compound. Unextractable 14C increased until day 35 for both RES and NORES, after which it remained constant for NORES, hut declined for RES. A corresponding rise in RES polar 14C suggested that as soybean residue decomposed, I4C bound in the residue MIUS released as extractable polar material. Soil with soybean residue accumulation r n q alter metabolite degradation patterns, but does not impede initial metribuzin degradation. Depth diffL'renceS in metribuzin degradation were attributed to reductions in microbial activity with increasing soil depth.