ADSORPTION AND RELEASE OF TYLOSIN BY CLAYS AND SOILS

The uptake and release of tylosin by Wyoming bentonite, Ca++ montmorillonite, illite (Fithian Illinois) and kaolin (china clay) was studied. The adsorption capacities of bentonite and montmorillonite for tylosin were found to be 190 and 65 μg mg-1 respectively, while the adsorption capacities of illite and kaolinite were found to be 22 and 6.5 μg mg-1. 7.6 and 7.4% respectively of the tylosin adsorbed by bentonite and montmorillonite, and 30 and 25% respectively of the tylosin adsorbed by illite and kaolinite, was released in phosphate buffer. The presence of tylosin in two different soils amended with tylosin fermentation waste was also studied, and the effect of temperature on tylosin release was examined in one of the soils. The concentration of tylosin in the soil water was found to be related more to the concentration of tylosin fermentation waste than to the incubation temperature. The amounts of tylosin present in the initial leachates of the two soils, a modified John Innes compost and a limestone waste, were found to be in excess of the minimum inhibitory concentrations for susceptible bacteria. It is hypothesised that in these particular soils if the tylosin is not broken down by microbial action it could affect susceptible populations of bacteria. © 1979 Martinus Nijhoff, The Hague/Kluwer Academic Publishers.