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Characterization of inorganic and biogenic magnesian calcites by Fourier Transform infrared spectroscopy

✍ Scribed by Michael E. Böttcher; Peer-Lennart Gehlken; D.Fraser Steele


Book ID
104296724
Publisher
Elsevier Science
Year
1997
Tongue
English
Weight
450 KB
Volume
101-103
Category
Article
ISSN
0167-2738

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✦ Synopsis


The effect of cationic substitution on the mid-infrared absorption spectra of synthetic, and natural inorganic and biogenic MgCO,-CaCO, solid solutions (Mg calcites; space group Rk; O-23 mol% MgCO,) is investigated, and the results are compared to disordered proto-dolomite (Ca,,,Mg, ,COs; space group Rk), ordered dolomite (Ca,,,Mg,,CO,; space group Rg), huntite (Ca,,,Mg 0.,$O,; space group R32), and magnesite (MgCO,; space group Rk). The measurements show that significant frequency shifts of the vibrational bands of the carbonate ion group occur as a function of chemical composition. The Mg2+ content of all Mg calcites correlates linearly with the position of the sharp u4 mode according to: v4 (cm-') = 39.40XM, + 712.20 (r = 0.97).


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