Iron complexes water exchange reactions

The above mechanistic interpretation is in contrast with the one appearing in the coordination chemistry of NO on the very labile Fe(III) porphyrins and hemoproteins, which show water substitution-controlled kinetics at the iron(III) center (22,25). The latter Fe(III) moieties are, however, high-spin systems, whilst the cyano-complexes are low-spin. There is strong experimental evidence to support the dissociative mechanism with the Fe(III)-porphyrins, because the rates are of the same order as the water-exchange reactions measured in these systems (22d). Besides, the Fe(III) centers are less oxidizing than [Fein(CN)5H20]2- (21,25). 

In contrast to the acid—base behavior of iron(III) porphyrin species, Fe (Pz) exists as an equilibrium mixture of monoaqua and diaqua complexes in acidic medium (46). The five-coordinate monoaqua iron(III) porphyrazine, [Fe (Pz)(H20)], which is the main species at low pH, is stabilized in the unusual intermediate spin state, S = 3/2. This behavior results from the fact that the porphyrazine ring is much smaller than that of the porphyrin and the iron(III) center has to be displaced out of the plane. At higher pH (pH = 10), a low-spin, six-coordinate aquahydroxido complex, [Fe (Pz)(H20)(0H)], is formed whereas a further increase in pH (pH = 13) results in the formation of the low-spin, dihydroxido complex, [Fe (Pz)(OH)2], for which no water exchange reaction could be observed (46). 

Sutin N., Rowley J. K. and Dodson W. (1961). Chloride complexes of iron (III) ions and the kinetics of chloride-catalyzed exchange reactions between iron (II) and iron (III) in light and heavy water. J. Phys. Chem., 65 1248-1252. 

A review of iron(III) in aqueous solution covers hydrolysis and polymerization, the formation and dissociation of binuclear species, and kinetics and mechanisms of water exchange and complex formation. " Kinetic and equilibrium data for hydrolytic reactions of iron(III) have been conveniently assembled. Reviews of hydrolysis of Fe aq, and subsequent precipitation of hydrated oxide-hydroxide species, cover a very wide range of media, from geochemistry to biology to human metabolism. Added anions or pH variation can affect which form... 

We can now make sensible guesses as to the order of rate constant for water replacement from coordination complexes of the metals tabulated. (With the formation of fused rings these relationships may no longer apply. Consider, for example, the slow reactions of metal ions with porphyrine derivatives (20) or with tetrasulfonated phthalocyanine, where the rate determining step in the incorporation of metal ion is the dissociation of the pyrrole N-H bond (164).) The reason for many earlier (mostly qualitative) observations on the behavior of complex ions can now be understood. The relative reaction rates of cations with the anion of thenoyltrifluoroacetone (113) and metal-aqua water exchange data from NMR studies (69) are much as expected. The rapid exchange of CN " with Hg(CN)4 2 or Zn(CN)4-2 or the very slow Hg(CN)+, Hg+2 isotopic exchange can be understood, when the dissociative rate constants are estimated. Reactions of the type M+a + L b = ML+(a "b) can be justifiably assumed rapid in the proposed mechanisms for the redox reactions of iron(III) with iodide (47) or thiosulfate (93) ions or when copper(II) reacts with cyanide ions (9). Finally relations between kinetic and thermodynamic parameters are shown by a variety of complex ions since the dissociation rate constant dominates the thermodynamic stability constant of the complex (127). A recently observed linear relation between the rate constant for dissociation of nickel complexes with a variety of pyridine bases and the acidity constant of the base arises from the constancy of the formation rate constant for these complexes (87). 

Tris(2,4-pentanedionato)iron(III) [14024-18-1], Fe(C H202)3 or Fe(acac)3, forms mby red rhombic crystals that melt at 184°C. This high spin complex is obtained by reaction of iron(III) hydroxide and excess ligand. It is only slightly soluble in water, but is soluble in alcohol, acetone, chloroform, or benzene. The stmcture has a near-octahedral arrangement of the six oxygen atoms. Related complexes can be formed with other P-diketones by either direct synthesis or exchange of the diketone into Fe(acac)3. The complex is used as a catalyst in oxidation and polymerization reactions. 

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