“…(a) spectra for gray/buff samples from 0.35 to 2.5 µm showing several features due to H 2 O, OH, NH 4 , and sulfate in these samples, (b) spectra from 1.3-2.5 µm including also NH 4 -bearing minerals. Vertical lines mark features due to minerals or species in these samples: dotted lines at 1.41 and 1.91 µm due to bound H 2 O in clays (Bishop et al, 1994) or zeolite (e.g., clinoptilolite, USGS spectral library, Clark et al, 1990), dashed lines at 1.45-1.48 and 1.94-1.97 µm due to H 2 O in hydrated sulfates such as hexahydrite (e.g., Bishop et al, 2009) or tschermigite (speclib.jpl.nasa.gov/library; Meerdink et al, 2019), solid lines at 1.56, 2.01 and 2.11 µm due to NH 4 + in minerals (e.g., Bishop et al, 2002;Berg et al, 2016), yellow solid lines at 1.47 and 2.26 µm due to Fe-OH in jarosite (Bishop and Murad, 2005), broken lines at 2.17 and 2.21 µm due to Al-OH in alunite (Bishop and Murad, 2005) and montmorillonite (e.g., Bishop et al, 2008), respectively. This is the peer-reviewed, final accepted version for American Mineralogist, published by the Mineralogical Society of America.…”