“…Furthermore, in soil with CaCO 3 , Ca 2þ ions reduce adsorption and increase solubility of Cd 2þ (Lagerwerff and Brower, 1972). In the case of As, because it is co-precipitated fundamentally with Fe oxyhydroxides, and the quantity precipitated decreases as pH increases (Jones et al, 1997;Tyler and Olson, 2001;Simón et al, 2005), high solubility and low precipitation and/ or adsorption of As would be expected in Area B, characterized by a basic pH and a relatively low Fe concentration (similar concentration as in Area C). The low Fe concentration in Area B would be attributable to the low concentration on sulphur-mining wastes (mean ¼ 62 g kg À1 ), far lower than in other types of mining wastes, such as sulphide (mean ¼ 359 mg kg À1 ; Alastuey et al, 1999).…”