“…cations by substituting the iron. ,− The content of Al(III) in natural goethite can be as high as 33% in molar ratios, while other elements are less than that. ,, By using Raman and Fourier transform infrared spectroscopy (FTIR) as well as microscopic techniques, the cation substitutions have been shown to alter the structure and surface reactivity of goethite to a certain extent, which further affects adsorption behavior of the heavy metals on it. , Among these cations, manganese is often substituted for Fe in many natural iron-bearing minerals, especially in goethite, due to its high affinity with Fe and almost equal radii of Fe ( r Fe3+ = r Mn3+ = 0.645 Å) . The incorporated Mn predominantly presents as Mn 3+ and/or Mn 4+ in an oxidizing environment. ,, Such incorporation normally alters the structure of goethite and its environmental performance. , Mn substitution observably enhances the oxidation of arsenite (As 3+ ) to arsenate (As 5+ ) by goethite, which suppresses the toxicity of arsenic in the environment . However, the valence of Mn on the goethite surface layer has not yet been accurately determined, which is crucial for understanding the surface reactivity.…”