“…The role of OM in the retention of Cu in archaeological soils is threefold; ionic interactions between OM and metals and complexation reactions may enhance retention (Singh, 1971;Covelo et al, 2004;Vega et al, 2006); insoluble high molecular weight organic acids can strongly bind Cu (Senesi et al, 1986;Kumpiene et al, 2007) and stabilize Cu through soil acidification (Chirenje and Ma, 1999); and low molecular weight humic-and fulvic acids (HA and FA) can form highly soluble Cu complexes (Hsu and Lo, 2000;Ashworth and Alloway, 2004) and remove Cu from soils. Despite the fact that the latter are likely eluviated from soils, stabilization of HA-Cu and FA-Cu complexes by adsorption onto clay minerals has also been reported (Arias et al, 2002;Hizal and Apak, 2006). Zinc retention shows trends similar to Cu, apart from the fact that Zn is relatively mobile in soils and easily exchanged by other trace metals (Cao et al, 2004).…”