Long‐Term Sorption and Desorption of Sulfadiazine in Soil: Experiments and Modeling

Antibiotics, such as sulfadiazine (SDZ), may enter arable soil by spreading of manure of medicated husbandry or directly by the excrement of grazing animals. Knowledge of the fate of antibiotics in soils is crucial for assessing the environmental risk of these compounds, including possible transport to ground water. Kinetic sorption of 14 C‐labeled SDZ (4‐amino‐N‐pyrimidin‐2‐yl‐benzenesulfonamide) was investigated using the batch technique. The batch sorption–desorption experiments were conducted at various concentration levels (0.044–13 mg L −1 initial solute concentration) and time scales (0.75–272 d). Sorption of 14 C‐SDZ in the investigated silty loam was time dependent and strongly nonlinear in the solution phase concentration. The time to reach an apparent sorption equilibrium was about 20 d. However, desorption was very slow, and 41 d were insufficient to reach the desorption equilibrium. An inverse modeling technique was used to identify relevant sorption processes of 14 C‐SDZ during the batch experiments. Among the investigated two‐ and three‐domain sorption models, adsorption and desorption of 14 C‐SDZ were best described with a new model defining two sorption domains and four parameters. Whereas sorption in the first sorption domain was nonlinear and instantaneous, solute uptake in the second sorption domain was rate limited following first‐order kinetics. Desorption followed the same rate law until an equilibrium distribution was reached. After that, desorption was assumed to be impossible due to partly irreversible sorption. Although the proposed model needs further validation, it contributes to the discussion on complex sorption processes of organic chemicals in soils.