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errocyanide, or yellow prussiate of potash (K_{4}FeC_{6}N_{6}), and potassium ferricyanide, or red prussiate of potash (K_{3}FeC_{6}N_{6}). These compounds are the potassium salts of the complex acids of the formulas H_{4}FeC_{6}N_{6} and H_{3}FeC_{6}N_{6}. ~Oxidation of ferrous salts.~ It has just been seen that when a ferrous salt is treated with an oxidizing agent in the presence of a free acid a ferric salt is formed: 2FeSO_{4} + H_{2}SO_{4} + O = Fe_{2}(SO_{4})_{3} + H_{2}O. In this reaction oxygen is used up, and the valence of the iron is changed from 2 to 3. The same equation may be written 2Fe^{++}, 2SO_{4}^{--} + 2H^{+}, SO_{4}^{--} + O = 2Fe^{+++}, 3SO_{4}^{--} + H_{2}O. Hydrogen ions have been oxidized to water, while the charge of each iron ion has been increased from 2 to 3. In a similar way the conversion of ferrous chloride into ferric chloride may be written Fe^{++}, 2Cl^{-} + Cl = Fe^{+++}, + 3Cl^{-}. Here again the valence of the iron and the charge on the iron ion has been increased from 2 to 3, though no oxygen has entered into the reaction. As a rule, however, changes of this kind are brought about by the use of an oxidizing agent, and are called oxidations. The term "oxidation" is applied to all reactions in which the valence of the metal of a compound is increased, or, in other words, to all reactions in which the charge of a cation is increased. ~Reduction of ferric salts.~ The changes which take place when a ferric salt is converted into a ferrous salt are the reverse of the ones just described. This is seen in the equation FeCl_{3} + H = FeCl_{2} + HCl In this reaction the valence of the iron has been changed from 3 to 2. The same equation may be written Fe^{+++}, 3Cl_{-} + H = Fe^{++}, + H^{+} + 3Cl_{-} It will be seen that the charge of the iron ions has been diminished from 3 to 2. Since these changes are the reverse of the oxidation changes just considered, they are called reduction reactions. The term "reduction" is applied to all processes in which the valence of the metal of a compound is diminished, or, in other words, to all processes in which the charge on the cations is diminished. NICKEL AND COBALT These elements occur sparingly in nature, usually combined with arsenic or with arsenic and sulphur. Both elements have been found in the free state in meteorites. Like iron they form two series of compounds, but the salts
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