The decomposition of H 2 O 2 , catalyzed by the Co 2 ® complex of 4,4′,4″,4″′-tetrasulfophthalocyanine (Co II PTS), was investigated in the pH range 3.8 through 10 by measuring the initial rate, v 0 =d(O 2 )/dt, of the increasing formation of O 2 (25°; I=0.1). In this pH range v 0 is proportional to the initial concentration of H 2 O 2 (determined at pH 5.0 and 9.2). Due to the dimerization (log KD=5.47 ±0.09 at natural ionic strength and about 7.63 ±0.16 in 0.1 M NaClO 4 ; 25°) and polymerization of Co II PTS the catalyst and its reaction order are difficult to establish: Based on the experimental evidence it is suggested that v 0 is proportional to the concentration of monomer Co II PTS. Additionally, there is evidence that the experimentally determined v 0 contains the contributions of a pH-independent and a pH-dependent reaction course. These results are analog to those obtained earlier with Fe III PTS as catalyst. A mechanism for the catalyzed disproportionation of H 2 O 2 by CoIIPTS is proposed. The catalase-like activity of Co III PTS (OH) is smaller than that of Co II PTS and the pH-dependence is different.
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