The degradation of chlorsulfuron was studied in laboratory experiments
in three oxisols from south and south-east Brazil. Three soil profile
s were sampled by horizon, and classified according to USDA soil taxon
omy and the Brazilian system. Degradation assays were made to evaluate
the influence of temperature, humidity and liming on chlorsulfuron de
composition. Further experiments were set up to study enhanced biodegr
adation. Abiotic degradation was also studied in sterile soils, to eva
luate, by comparison with non-sterile soils, the role of microorganism
s in degradation. The degradation always followed first-order kinetics
and was generally faster in samples from A than B horizons. An increa
se in temperature (from 25 to 40 degrees C) increased chlorsulfuron de
gradation. Further, an increase in moisture content increased chlorsul
furon degradation in samples from the A horizons of all soils, whereas
for two out of three soils, degradation in samples from the B horizon
was greater at lower water content. The biotic contribution to degrad
ation was significant only for the soil with higher fertility. Soil li
ming significantly increased chlorsulfuron half-life in all samples. S
ignificant enhancement of degradation (decrease in half-life on reappl
ication) was observed only in soil from A horizons, where a higher mic
robial activity was likely.