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J Inorg Biochem ; 11(3): 205-12, 1979 Nov.
Article in English | MEDLINE | ID: mdl-512658

ABSTRACT

The reduction by dithionite ion (in excess) of methemerythrin-anion adducts, Hr+X-, to deoxyhemerythrin, Hr degree, has been examined at 25 degrees and pH 6.3 and 8.2. The results accord with the scheme: S2O42- in equilibrium 2SO2- rapid Hr+X- in equilibrium Hr++X- k-1, k1 Hr++SO2- leads to PRODUCT k2 with X- = Br-, HCO2-, CNO-, and F-, k2[SO2-] greater than k1[X-], and the pseudo first-order rate constant, kobs (= k-1), is independent of [X-] and [S2O42-]. Only with X- = NCS- is k2[SO2-] approximately k1[X-] and kobs = a[S2O42-]1/2 (b[NCS-] + [S2OR2-]1/2)-1. Values at pH 6.3 of k-1 (sec-1) and k1 (M-1 sec-1), obtained by anation and anion displacement reactions, are 2.3 x 10(-3), 1.6 x 10(-2) (Br-); 1.5 x 10(-3), 1.2 x 10(-2) (HCO2-); 1.3 x 10(-4), 0.52 (CNO-) and approximately 2 x 10(-4), 3.3 x 10(-3) (CN-, pH 7.0). Values of k-1 from reduction and displacement methods are in good agreement with each other. The value of k2 (1.6 x 10(5) M-1 sec-1, pH 6.3) in somewhat smaller than that for reduction of the met form of hemoproteins. There is only a small effect of pH on rates. Direct reduction of Hr+CN- does not occur, in contrast with Mb+CN-.


Subject(s)
Dithionite , Hemerythrin , Metalloproteins , Sulfites , Animals , Anions , Ferric Compounds , Kinetics , Nematoda , Oxidation-Reduction , Protein Binding
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