Most studies on elemental sulfur (Es) oxidation have focused on small Es particles mixed through soil, even though commercial Es fertilizers are usually in granular form. Although it has been recognized that cogranulation of Es decreases its oxidation rate, no attempt has been made to quantify this effect. We developed a conceptual model that predicts the "effective diameter" (the diameter of Es particles mixed through soil that would oxidize at the same rate as the granulated Es) by taking into account the effect of granulation on the effective surface area available to the Es in the granule cavity after the soluble macronutrient compound in the fertilizer has diffused away. To validate the model, the oxidation rate was determined for Es-fortified monoammonium phosphate fertilizer with varying Es content (20-250 g kg −1 ), Es particle diameter (25 or 60 mm), and granule diameter (1.8 or 3.4 mm). The time to reach 50% oxidation varied from 17 d for small granules at the lowest Es content to 210 d for the large granules with the highest Es content. In agreement with the model predictions, reducing Es particle size did not affect the oxidation rate except at the lowest Es rate, whereas reducing granule size increased the oxidation rate. Predicted and observed oxidation rates were in good agreement, indicating that the model describes the effect of granulation with reasonable accuracy. This model may assist in improving formulation of Es-containing fertilizers and guiding fertilizer recommendations.Abbreviations: ES, elemental sulfur; MAP, monoammonium phosphate; TSP, triple superphosphate. E lemental sulfur (ES) is a common S fertilizer source. Elemental S is insoluble in water and hence is not susceptible to leaching and also has the benefit of lower transport/handling costs because it is the most concentrated form of S. However, ES only becomes available to plants when it is oxidized to sulfate (Boswell and Friesen, 1993). Knowledge of the factors that affect ES oxidation is hence required to develop fertilizer recommendations for ES-containing fertilizers.The oxidation of ES particles is affected by biological, fertilizer, and soil-related factors (Germida and Janzen, 1993). Because ES oxidation is a biologically mediated process, it is strongly influenced by temperature. Janzen and Bettany (1987a) assessed ES oxidation in six soils in Saskatchewan, Canada, at temperatures ranging between 3 and 30°C and found Q 10 values (factor increase per 10°C increase) ranging from 3.2 to 4.3. Oxidation of ES is a surficial process, and the rate of oxidation is therefore proportional to the specific surface area of the ES particles. Soil properties also affect the oxidation rate, likely through their effect on the composition and abundance of the microbial community. For instance, Zhao et al. (2015) found that the surface-based oxidation rate of ES in 10 Australian soils ranged between 5 and 52 mg cm −2 d −1 and was positively correlated with the pH and organic matter content of the soil.