Ak. Sarmah et al., Leaching and degradation of triasulfuron, metsulfuron-methyl, and chlorsulfuron in alkaline soil profiles under field conditions, AUST J SOIL, 38(3), 2000, pp. 617-631
A field study was conducted on an alkaline cropping soil (plot size 4 m by
1 m), representative of cereal growing regions in southern Australia, to ex
amine the degradation and leaching behaviour of triasulfuron, metsulfuron-m
ethyl, and chlorsulfuron (150 g a.i./ha), along with a non-reactive tracer
(KBr, 50 kg/ha), under 2 water treatments ('rainfall' and 'rainfall + irrig
ation'). The results showed that the distributions of water content, Br-, a
nd the 3 herbicides were influenced by the amount of rainfall/irrigation re
ceived, and the biological activity as well as the physico-chemical propert
ies of the soil within the profile. The largest concentrations of Br- were
detected in the 10-20 cm depth under both treatments. No additional peak of
Br- was observed in the plots which received only rainfall; however, there
was another peak at 100 cm depth after a cumulative rainfall and irrigatio
n of 158 mm. The spatial distribution of Br- in the plots was attributed to
preferential flow through cracks or the presence of 'mobile' and 'immobile
' water, which gave rise to bimodal distribution in the profile. Metsulfuro
n-methyl showed the greatest mobility, followed by chlorsulfuron and triasu
lfuron under both the treatments, with metsulfuron-methyl being detected at
120 cm depth under rainfall + irrigation. A bimodal distribution was also
observed for the 3 herbicides, but the location of peaks was dependent on t
he solute. Rates of degradation of the herbicides could be described reason
ably well with first-order reaction kinetics (r(2) = 0.72-0.91). The half-l
ives for triasulfuron, metsulfuron-methyl, and chlorsulfuron were 44, 45, a
nd 32 days, respectively, under rainfall (69 mm), and 46, 59, and 48 days u
nder rainfall + irrigation (158 mm).