Quinoid groups of humic acids from various sources (soil, peat, brown and oxidized coals) can undergo reversible redox transformations, this being a fundamental property of this class of natural compounds. Kinetic oxidation curves for reduced humic acids indicate the presence of various types of quinoid groups. The specificity of a previously suggested technique for determining quinones in humic acids has been corroborated. Exhaustive carbonyl reduction by sodium borohydride combined with reductometric methods for determining quinones in alkaline media make possible a better estimation of the ketone content in humic acids. When humic acids are reduced in an acid solution of tin chloride, rigorous conditions (4 h, 120°C, strong acid media) lead to an irreversible conversion of part of the quinone carbonyls and, as a result, the reaction proceeds nonstoichiometrically.