A field study was conducted to determine the fate of atrazine (6-chloro-N-2
-ethyl-N-4-isopropyl-1,3,5-triazine-2,4-diamine) within the root zone (0 to
90 cm) of a sandy soil cropped with sorghum [Sorghum bicolor (L.) Moench]
in Gainesville, Florida. Atrazine was uniformly applied at a rate of 1.12 k
g a.i. ha(-1) to a sorghum crop ender moderate irrigation, optimum irrigati
on, and no irrigation (rainfed), 2 d after crop emergence. Bromide as a tra
cer for water movement was applied to the soil as NaBr at a rate of 45 kg B
r- ha(-1), 3 d before atrazine application, Soil water content, atrazine, a
nd Br- concentrations were determined as a function of time using soil samp
les taken from the root zone. Atrazine sorption coefficients and degradatio
n rates were determined by depth for the entire root zone in the laboratory
. Atrazine was strongly adsorbed within the upper 30 cm of soil and most of
the atrazine recovered from the soil during the growing season was in that
depth. The estimated half-life for atrazine was 32 d in topsoil to 83 d in
subsoil, Atrazine concentration within the root zone decreased from 0.44 k
g a.i. ha(-1) 2 days after application (DAA) to 0.1 kg a.i. ha(-1) 26 DAA.
Negligible amounts of atrazine (approximate to5 mug kg(-1)) were detected b
elow the 60-cm soil depth by 64 DAA, Most of the decrease in atrazine conce
ntration in the root zone over time was attributed to degradation. In contr
ast, all applied bromide had leached past the 60-cm soil depth during the s
ame time interval.