The aim of this work was to study the influence of low molecular weight organic acid concentration (0 to 1600 μmol C L−1) and type (oxalic, citric (CI), salicylic) and of solution pH (3.2 to 4.7) on the kinetics of SO4sorption by the B horizon of two Spodosols (HER and CON) from the Lower Laurentians, Quebec. Using a miscible displacement technique, the soil materials were leached at a flow rate of 0.2 ml min−1for 6 h at 25°C. The slope parameter (1/β) of the Elovich equation was used as an apparent SO4sorption rate. The presence of organic ligands in solution reduced SO4sorption by the HER B and the CON B horizons from 543 to 365 μmol SO4kg−1and from 1053 to 642 μmol SO4kg−1, respectively. For both soils, 1/β values were always higher (97 to 51 μmol kg−1In min−1(HER) and 256 to 135 μmol kg−1In min−1(CON)) in systems that were free of organic acids; however, the relationships between the properties of the acids and their relative SO4sorption inhibition capacity was not clear. The extent of SO4sorption inhibition increased considerably as CI concentration was augmented from 100 to 1600 μmol C L−1. The efficiency of CI in reducing SO4sorption by the HER B horizon was pH dependent, with SO4sorption during the experiment decreasing by 23% at pH 3.2 and by 355% (desorption) at pH 4.7. The presence of CI led to the desorption of native exchangeable SO4when the pH was above 4.2 or when the total C concentration was high (1600 μnol C L−1). The data thus reveal that temporal changes in C cycling can affect SO4mobility in acidic forest soils with potential implications on the transport of nutrient cations if the total anionic equivalent charge of the soil solution is increased.