L. Cox et al., ADSORPTION AND DESORPTION OF THE HERBICIDE THIAZAFLURON AS A FUNCTIONOF SOIL PROPERTIES, International journal of environmental analytical chemistry, 58(1-4), 1995, pp. 305-314
The effect of soil composition on the adsorption and desorption of the
herbicide thiazafluron methyl-1-(5-trifluoromethyl-1,2,3-thiadiazol-2
-yl) urea] by 20 soil samples of 13 selected soil profiles of southern
Spain has been studied. The adsorption curves conformed the Freundlic
h equation and the values of the constants, Kf and nf, ranged from 0.1
3 to 4.64 and from 0.14 to 1.30, respectively. The simple and multiple
regression analysis between Kf and soil properties revealed soil clay
content, illite content and CEC as fundamental factors determining th
iazafluron adsorption by soils. Unlike other substituted ureas, non si
gnificant correlation was found with soil organic matter. Desorption o
f thiazafluron was hysteretic in all cases, showing nfd values much lo
wer than those for adsorption. Desorption kinetic indicated that this
hysteresis is essentially due to irreversible adsorption, although som
e degradation seems also to occur. The Freundlich desorption Kfd value
s were closely related to the same factors as Kf: clay and illite cont
ents and also montmorillonite content, suggesting that most of the hys
teresis was due to thiazafluron irreversibly bound to soil clay minera
l components.