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Volmer cation-exchanged

Metal dissolution usually follows the Butler-Volmer equation (Eqs. (1-26) and (1-28)) independent from which surface position the transfer of the metal cation may occur. The relation for the exchange current density may contain the concentration of a catalyzing or complexing anion. The catalysis of iron dissolution by OH" ions is a typical example which has been studied in detail (Bonhoeffer and Heusler, 1956). Its mechanism includes a sequence of partial reactions of an electrode process and its in-... [Pg.43]

While the presence of MV2+ on the zeolite external surface, or ion exchange of MV2+ with solution-phase cations such as H+ might be invoked to explain these anomalously high quenching rates, we consider these explanations unlikely. The Stem-Volmer plots for zeolites L and Y are linear down to very low MV2+ loading, where we would expect little or no MV2+ to be present at external sites. Ion-exchange with solution-phase H+ should give detectable concentrations of MV2+ and/or Ru(bpy)32+ in solution, and none... [Pg.337]


See other pages where Volmer cation-exchanged is mentioned: [Pg.150]    [Pg.281]    [Pg.331]    [Pg.116]    [Pg.179]    [Pg.100]    [Pg.206]    [Pg.198]    [Pg.246]   
See also in sourсe #XX -- [ Pg.249 ]




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Exchangeable cations

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