Adsorption, incubation and soil-column experiments with bentazone [3-i
sopropyl-1H-2,1,3-benzothiadiazin-4(3H)-one 2,2-dioxide] were carried
out in ten different soils from the marches surrounding the Donana Nat
ional Park (Huelva, SW Spain). Adsorption isotherms for the different
soils showed a good fit with the Freundlich equation. Bentazone was po
orly adsorbed in all the soils studied, with no significant relationsh
ip between the K-f values and soil characteristics. A significant corr
elation was obtained between the soil organic matter content and the d
istribution constant values (K-d) calculated at an equilibrium concent
ration of 200 mu g cm(-3). The low adsorption and non-degradation of b
entazone on these soils suggest that the herbicide readily percolates
through soils to reach the surface and ground waters. The mobility of
bentazone through three soil columns was also studied. The mass balanc
es carried out showed that bentazone was totally eluted from the soil
columns. The theoretical model applied to explain bentazone leaching u
nder our experimental conditions seems to be suitable for soil columns
with a uniform water-flow rate.