The ability of three atrazine-degrading bacteria, Pseudomonas sp. strain AD
P, a Pseudaminobacter sp., and a Nocardioides sp., to degrade and mineraliz
e this herbicide in a loam soil was evaluated in laboratory microcosms. The
se bacteria all hydrolytically dechlorinate atrazine, and degrade atrazine
in pure culture with comparable specific activities. The Pseudaminobacter a
nd Nocardioides can utilize atrazine as sole carbon and nitrogen source, wh
ereas the Pseudomonas can utilize the compound only as a nitrogen source. T
he Pseudomonas and Pseudaminobacter mineralize the compound; the end produc
t of atrazine metabolism by the Nocardioides is N-ethylammelide. At inoculu
m densities of 10(5) cells/g soil, only the Pseudaminobacter and Nocardioid
es accelerated atrazine dissipation. The Pseudaminobacter mineralized atraz
ine rapidly and without a lag, whereas atrazine was mineralized in the Noca
rdioides-inoculated soil but only after a lag of several days. The Pseudami
nobacter remained viable longer than did the Pseudomonas in soil. PCR analy
sis of recovered bacteria indicated that the genes atzA (atrazine chlorohyd
rolase) and atzB (hydroxyatrazine ethylaminohydrolase) were less stable in
the Pseudaminobacter than the Pseudomonas. In summary, this study has revea
led important differences in the ability of atrazine-hydrolyzing bacteria t
o degrade this compound in soil, and suggests that the ability to utilize a
trazine as a carbon source is important to establish "enhanced degradation"
by ecologically meaningful inoculum densities.