Humic acid (HA) participates in a variety of electron transfer reactions, but its fundamental redox properties, such as formal electrode potential and oxidation capacity, are not well characterized. Specific functionalities in HA, such as semiquinone free radicals, have been hypothesized to participate in redox reactions; however, few supportive data exist. To address these issues, three standard humic acids (Suwannee River, soil, and peat) were titrated at pH 5 and 7 with I2 as an oxidant under an inert Ar atmosphere at 25°C. The formal electrode potential of the three HA samples at pH 5 was 0.778±0.017 V, decreasing with pH by −20.0±3.2 mV per pH unit. The oxidation capacity of HA (moles of HA charge per unit mass transferred to a strong oxidant) ranged from 1.09 to 6.5 molc kg−1 at pH 5 and from 3.3 to 11.5 molc kg−1 at pH 7. The increasing order of oxidation capacity for the humic acids was: soil HA