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Meridianiite_IR_Spectra.jpg (799 × 426 pixels, file size: 65 KB, MIME type: image/jpeg)

Summary

Description
English: Infrared absorption of meridianiite. Trace A was obtained below 0 °C, trace B was recorded after the sample was warmed and had incongruently melted to epsomite and solution, and trace C was recorded from a mixture containing epsomite (MgSO4·7H2O) with paraffin oil and a small amount of water prepared to simulate the product of the transition from MgSO4·11H2O to MgSO4·7H2O + 4H2O. As the sample was warmed, changes were observed in both the water band centered near 3400 cm–1, and the sulfate band centered at 1100 cm–1. In both regions, the new bands of trace B resemble those observed in the spectrum of MgSO4·7H2O with a small amount of water added (trace C).
Date
Source Meridianiite: A new mineral species observed on Earth and predicted to exist on Mars
Author R.C. PETERSON, W. NELSON, B. MADU, AND H.F. SHURVELL

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Date/TimeThumbnailDimensionsUserComment
current04:15, 11 February 2010Thumbnail for version as of 04:15, 11 February 2010799 × 426 (65 KB)Ian Foster{{Information |Description={{en|1=Infrared absorption of meridianiite. Trace A was obtained below 0 °C, trace B was recorded after the sample was warmed and had incongruently melted to epsomite and solution, and trace C was recorded from a mixture contai

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