Transformation of pesticides is dependent on soil environmental condit
ions and knowledge of this is necessary to improve subsurface fate and
transport pesticide models. Laboratory experiments were performed usi
ng C-14 ring and isopropyl side-chain labeled atrazine -chloro-4-ethyl
amino-6-isopropyl-amino-s-triazine) applied to three Iowa soils incuba
ted in batch reactors under different environmental conditions. Minera
lization of both the ring and isopropyl side chain carbons was proport
ional to the organic matter content of the soils and oxygen content. A
trazine ring carbon mineralization also increased with soil water cont
ent. Oxygen limitation in soils reduced the bio-transformation rate of
atrazine, and mineralization was much slower under denitrifying condi
tions. Empirical models were developed to represent the mineralization
rate of atrazine ring carbon and isopropyl side-chain carbon for vary
ing soil organic matter, soil water content, temperature, and oxygen p
artial pressure.