The pathway with the name Bensulfuron methyl
 has the following structure: 
Result: 
COC1=NC(=NC(=C1)OC)NC(=O)NS(=O)(=O)CC2=C(C=CC=C2)C(=O)OC
 no rule associatedCOC1=CC(=NC(=N1)NC(=O)NS(=O)(=O)CC2=C(C=CC=C2)C(=O)OC)O
COC(=O)C1=C(C=CC=C1)CS(=O)(=O)N
 no rule associatedC1=CC2=C(C=C1)C(=O)NS(=O)(=O)C2
COC1=NC(=NC(=C1)OC)NC(=O)NS(=O)(=O)CC2=C(C=CC=C2)C(=O)O
 no rule associatedC1=CC(=C(C=C1)C(=O)O)CS(=O)(=O)N
COC(=O)C1=C(C=CC=C1)CS(=O)(=O)N
 no rule associatedC1=CC(=C(C=C1)C(=O)O)CS(=O)(=O)N
COC1=NC(=NC(=C1)OC)NC(=O)NS(=O)(=O)CC2=C(C=CC=C2)C(=O)OC
 no rule associatedCOC1=NC(=NC(=C1)OC)NC(=O)NS(=O)(=O)CC2=C(C=CC=C2)C(=O)O
COC1=NC(=NC(=C1)OC)NC(=O)NS(=O)(=O)CC2=C(C=CC=C2)C(=O)OC
 no rule associatedCOC1=NC(=NC(=C1)OC)N
COC(=O)C1=C(C=CC=C1)CS(=O)(=O)N

Description: Degradation of [14C]bensulfuron methyl was rapid; besides 14CO2, IN-R9419, IN-J0290, and IN-D1R84 were the only degradation products found at levels greater than 10% of the applied radioactivity. Degradates present between 5-10% AR were IN-N5297 and IN-F7880. IN-B6895 was identified as a minor degradate less than 2%. The formation of 14CO2, which accompanied the disappearance of bensulfuron methyl, IN-R9419, and the formation (and decline) of the other degradates was indicative that soil microbes played a significant part in the ultimate mineralisation of bensulfuron methyl. In other soil degradation studies, no 14CO2 was observed to form from [14C]bensulfuron methyl if soils were sterilised prior to treatment (Friedman, 1984; Yordy, 1987). The results obtained in this study indicate that bensulfuron methyl should readily degrade in a microbially viable soil, with eventual mineralisation to CO2.
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