On the validity of specific rate constants (kSA) in Fe0/H2O systems.
The validity of the specific reaction rate constants (k(SA)) in modelling contaminant removal in Fe(0)/H(2)O systems is questioned. It is shown that the current k(SA)-model does not consider the large reactive surface area provided by the in-situ formed oxide film, and thus the adsorptive interactions between contaminants and film materials. Furthermore, neither the dynamic nature of film formation nor the fact that the Fe(0) surface is shielded by the film is considered. Suggestions are made how the k(SA)-model could be further developed to meet its original goal.
Angewandte Geologie, Universität Göttingen, Göttingen, Germany. cnoubac@gwdg.de
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D000327:Adsorption; D005296:Ferrous Compounds / Q000302:isolation & purification*; D007700:Kinetics; D008956:Models, Chemical; D014867:Water / Q000737:chemistry*; D018508:Water Purification / Q000379:methods
D005296:Ferrous Compounds; D014867:Water; C034236:ferrous oxide