SPAFMSR



Buzgar N., Apopei A. I., Buzatu A. (2009) - Romanian Database of Raman Spectroscopy (http://rdrs.uaic.ro)
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Formula: |
Cu2(CO3)(OH)2 |
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Crystal Data: |
Crystal System: Monoclinic - Prismatic |
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Point Group: 2/m |
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Cell Data: |
Space Group: P21/a, a = 9.502, b = 11.974, c = 3.24, Z = 4 |
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Density (calc.) = 4.03 and V = 364.35 Å3 |
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Element color: Cu, C, O, H |
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Sample no. 5393 from the "Mineralogy and Petrography Museum Grigore Cobălcescu" of "Alexandru Ioan Cuza" University, Iaşi. Origin: Eisenzeche - Germany. Click image to enlarge |
Malachite has two characteristic very strong bands at 435 and 1495 cm-1.
As in the case of azurite, the bands at the lowest region of the spectrum of malachite can be attributed to the lattice modes. In this region the spectrum shows an intense band at 434 cm-1, and the others at: 215, 269, 354, 536 and 596 cm-1.
The characteristic bands for CO3 group are observed at: 1059 and 1097 cm-1 for the ν1 symmetric stretching modes (of two different CO3 groups - doubly degenerate mode); 820 cm-1 attributed to ν2 asymmetric bending (Frost et al., 2002); 1368, 1462 and 1495 cm-1 assigned to ν3 asymmetric stretching mode; and for ν4 symmetric bending mode (doubly degenerate mode) at 722 and 755 cm-1. For the hydroxyl-stretching region, the spectrum shows bands at 3310 and 3382 cm-1. The vibration mode of hydroxyl group (O-H bending mode) appear at 1639 cm-1.
Differences between the spectra of malachite and azurite may be explained by the molecular structure of azurite being based upon a distorted square planar arrangement compared with a distorted octahedral arrangement about the copper in malachite (Frost et. al., 2002).
Buzgar et al., 20091 | Frost et al., 2002 | Mattei et al., 2008 | Assignment |
215, 269, 354, 434, 536, 596 |
130, 142, 151, 166, 176, 205, 217, 267, 294, 320, 349, 389, 429, 514, 531, 563, 596 |
157, 171, 182, 204, 224, 272, 352, 435, 513, 537, 601 |
T(Cu,CO3) |
722, 755 | 718, 750 | 723, 753 | ν4 symmetric CO3 deformation |
820 | 807, 817 | ν2 asymmetric CO3 deformation | |
1059, 1097 | 1098 | 1058, 1101 | ν1 symmetric CO3 stretching |
1368, 1462, 1495 | 1365, 1423, 1493, 1514 | 1370, 1463, 1497 | ν3 asymmetric CO3 stretching |
1639 | O-H bending mode | ||
3310, 3382 | 3349, 3380 | 3380 | O-H stretching mode |
• The Mineralogy Database [link]
• Crystal data (.cif file) from the American Mineralogist Crystal Structure Database [link]
• 1BUZGAR N., APOPEI A. I. (2009) - The Raman study on certain carbonates. Analele Stiintifice ale Universitatii “Al. I. Cuza” - Iasi, Tome 55, issue 2, 97-112 [link]
• FROST R. L., MARTENS W. N., RINTOUL L., MAHMUTAGIC E., KLOPROGGE J. T. (2002) - Raman spectroscopic study of azurite and malachite at 298 and 77 K. Journal of Raman Spectroscopy, 33, p. 252-259 [link]
• MATTEI E., VIVO G., SANTIS A., GAETANI C., PELOSI C., SANTAMARIA U. (2008) - Raman spectroscopic analysis of azurite blackening. Journal of Raman Spectroscopy, 39, p. 302-306 [link]