| Abstract: | In the reaction between equimolar amounts of horseradish peroxidase and chlorite, the native enzyme is oxidized directly to Compound II (Hewson, W.D., and Hager, L.P. (1979) J. Biol. Chem. 254, 3175-3181). At acidic pH but not at alkaline values, this initial reaction is followed by oxidation of Compound II to Compound I. The highly pH-dependent chemistry of Compound II can be readily demonstrated by the reduction of Compound I, with ferrocyanide at acidic, neutral, and alkaline pH values. Titration at low pH yields very little Compound II, whereas at high pH, the yield is quantitative. Similarly, the reaction of horseradish peroxidase and chlorite at low pH yields Compound I while only Compound II is formed at high pH. At intermediate pH values both the ferrocyanide reduction and the chlorite reaction produce intermediate yields of Compound II. This behavior is explained in terms of acidic and basic forms of Compound II. The acidic form is reactive and unstable relative to the basic form. Compound II can be readily oxidized to Compound I by either chloride or chlorine dioxide in acidic solution. The oxidation does not occur in alkaline solution, nor will hydrogen peroxide cause the oxidation of Compound II, even at low pH. |
