“…Synchrotron‐based μ‐XRD analyses of these same POIs confirmed the presence of willemite and hemimorphite, which are both Zn silicate minerals. Other studies using EXAFS discovered that Zn primarily exists as willemite, hemimorphite, gahnite, franklinite, and sphalerite, and incorporated into the interlayers of phyllosilicate minerals (i.e., LDH phases) in smelter‐contaminated environments (Isaure et al, 2005; Manceau et al, 2000; Nachtegaal et al, 2005; Roberts et al, 2002; Sarret et al, 2004; Scheinost et al, 2002; Williams et al, 2011). The minerals willemite, hemimorphite, franklinite, and gahnite are all high‐temperature Zn minerals that were likely formed during the smelting process, which causes them to be highly crystalline and easily identified by XRD (Manceau et al, 2000; Nachtegaal et al, 2005; Roberts et al, 2002; Williams et al, 2011).…”