“…The propensity for transition metals, including Zn, to reside in multiple coordination environments makes aqueous, sorbed and mineral speciation complex and identification in unknown specimens challenging. Such variations in the Zn coordination environment have been documented at several mineral surfaces, including silica (Nelson et al, 2017(Nelson et al, , 2018Roberts et al, 2003), kaolinite (Guinoiseau et al, 2016;Nachtegaal & Sparks, 2004), alumina (Trainor et al, 2000;Roberts et al, 2003), montmorillonite (Lee et al, 2004), birnessite (Qin et al, 2018;Manceau et al, 2002), hematite (Ha et al, 2009), goethite (Nachtegaal & Sparks, 2004;Hamilton et al, 2016) and ferrihydrite (Waychunas et al, 2002). The precise bonding environment of Zn on mineral surfaces has implications for mobility and toxicity because different sorbed species may be differentially labile, such as octahedral versus tetrahedral Zn complexes on birnessite (Qin et al, 2018) and inner-sphere versus outer-sphere Zn complexes on hematite (Ha et al, 2009).…”