The chemistry of extremely acid Oa horizons does not conform to traditional pH, Al, and base saturation relationships. Results from two separate studies of northeastern U.S. forested soils were used to investigate relationships between pH in water or dilute salt solutions and other soil characteristics. In Oa horizons with pH below 4, soil pH in dilute CaCl₂ solution was correlated with exchangeable H⁺ measured either by titration (r = −0.88, P = 0.0001, n = 142) or by electrode (r = −0.89, P = 0.0001, n = 45). Exchangeable H⁺ expressed as a percentage of the cation-exchange capacity (CEC) was linear with pH and showed similar slopes for data from both studies. For all samples, pHw = 4.21 − 1.80 × H⁺/CEC (R² = 0.69, n = 194). The reciprocal of the H⁺/CEC ratio is base saturation with Al added to the bases. Because of the low pH, exchangeable Al does not appear to behave as an acid. Exchangeable H⁺ remains an operationally defined quantity because of the difficulty in separating exchange and hydrolysis reactions. In a variety of neutral-salt extractants, concentrations of H⁺ were correlated with 0.1 M BaCl₂-exchangeable H⁺ (r > 0.91, P = 0.0001, n = 26) regardless of the strength of the extract. Nine successive extractions with 0.33 mM CaCl₂ removed more H⁺ than was removed by single batch extractions with either 1 M KCl or 0.1 M BaCl₂ (average H⁺ of 70, 43, and 49 mmol kg⁻¹, respectively for 26 samples). The data showed little difference in the chemical behavior of Oa horizons from a variety of geographical sites and vegetation types.