“…In particular, mainly iron hydroxide carbonate (chukanovite, Fe 2 CO 3 (OH) 2 ) is formed in the presence of carbonate on the iron surface (Ruhl et al, 2011) and influences significantly the reactivity (Jeen et al, 2006;Lee and Wilkin, 2010;Ruhl et al, 2012). High concentrations of inorganic carbon increase not only the dehalogenation rates of chlorinated groundwater contaminants but also the inhibition of reactive sites in the long-term (Parbs et al, 2007).…”