Abstract
The degradation of caffeine by ozone was investigated in this article. In the laboratory experimental scale, the effect of pH, caffeine initial concentration, power UV light and reaction time were studied by experimental design. The use of response surface methodology (RSM) allowed to adjust the optimal regions of the parameters leading to the response factor (% mineralization). In addition, a single polynomial expression for modeling the reaction was obtained. Results clearly demonstrated that caffeine is quickly degraded, but not mineralized as quickly. The results indicated that the caffeine mineralization rate increased with pH and reaction time. Power UV light showed little effect on mineralization efficiency.