Formed by evaporation of a solution of K2SO4 + CaSO4 solution at room temperature. Hydrous sulfate Spectrum originally published in: Crowley, J.K., 1991, Visible and Near-Infrared (0.4 - 2.5µm) Reflectance Spectra of Playa Evaporite Minerals: Journal of Geophysical Research, vol 96, no.B10, p. 16,231-16,240. IMAGE_OF_SAMPLE:
XRD Analysis
Pure syngenite. (Crowley, 1991)
X Units
cm⁻¹
Y Units
Absorbance
Data Points
1,801
Download
Attribution
USGS Spectral Library Version 7, U.S. Geological Survey