The pathway with the name Folpet
 has the following structure: 
Result: 
C1=CC(=C(C=C1)C(=O)O)C(=O)N
 no rule associatedC1=CC(=C(C=C1)C(=O)O)C(=O)O
C1=CC2=C(C=C1)C(=O)N(C2=O)SC(Cl)(Cl)Cl
 no rule associatedC1=CC2=C(C=C1)C(=O)NC2=O
C1=CC2=C(C=C1)C(=O)NC2=O
 no rule associatedC1=CC(=C(C=C1)C(=O)O)C(=O)N

Description: Folpet underwent rapid degradation in soil at temperatures of 20 and 25?C under laboratory aerobic conditions with a DT50 of 0.2 to 4.3 days. The significant metabolites phthalimide, phthalamic acid and phthalic acid were observed, but levels of these compounds rapidly declined. For the degradation of folpet under aerobic conditions at lower temperatures a corresponding DT50 value at 10?C was measured to be 3.8 days in a silt loam soil (corresponding value at 20?C was 0.8 days). In the study of Crowe 2001, radioactivity associated with the non-extractable soil fraction (bound residue) is ultimately degraded to CO2 and experimental evidence for this is provided, for example, by the clay loam soil. In this soil, the bound residue fraction represented the only significant pool of radioactivity in the soil after 4 days and therefore this fraction must be considered the source of radioactivity from which the increasing levels of carbon dioxide observed between 4 and 30 days were generated. Aniline is not formed as a metabolite of folpet in soil under aerobic conditions and therefore the effect on soil humic acids need not be considered.
Your Options:
Update the Pathway Information: POST with (required) pathwayName and (optional) pathwayDescription.
Delete the Pathway: DELETE.
Show nodes: GET on https://envipath.org/package/d817c31c-d879-44c8-913d-2963d42f8203/pathway/7af2ee17-4b38-49ab-a243-92b4b44cb3ed/node
Show edges: GET on https://envipath.org/package/d817c31c-d879-44c8-913d-2963d42f8203/pathway/7af2ee17-4b38-49ab-a243-92b4b44cb3ed/edge