SPAFMSR


Buzgar N., Apopei A. I., Buzatu A. (2009) - Romanian Database of Raman Spectroscopy (http://rdrs.uaic.ro)
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Formula: |
Cu3(CO3)2(OH)2 |
|
Crystal Data: |
Crystal System: Monoclinic - Prismatic |
|
| Point Group: 2/m | ||
Cell Data: |
Space Group: P21/a, a = 5.008, c = 10.336, Z = 2 |
|
Density (calc.) = 3.79 and V = 302.25 Å3 |
||
| Element color: Cu, C, O, H | ||
Sample no. 5397 from the "Mineralogy and Petrography Museum Grigore Cobălcescu" of "Alexandru Ioan Cuza" University, Iaşi. Origin: Namibia. Click image to enlarge |
The azurite spectrum is characterized by several lines that cover the spectral range 200-1600 cm-1. The bands observed up to 600 cm-1 are assigned to the translations of (Cu, CO3), those observed up to 1600 cm-1 are assigned to CO3 complex (Frost et al., 2002). The Raman spectrum of our azurite does not show the O-H stretching band at about 3400 cm-1.
Azurite has a characteristic intense band at 404 cm-1. The symmetric stretching band of carbonate ion is observed at 1097 cm-1, this band is assigned to the ν1 symmetric stretching vibration. The band attributed to the carbonate (ν3) asymmetric stretching vibration is observed at 1425 cm-1 and 1459 cm-1. One band is observed in the Raman spectrum of azurite at 766 cm-1 and is assigned to the ν4 mode. The band of 835 cm-1 was assigned to the ν2 asymmetric bending vibration. A number of bands with different intensities are observed in the lowest spectral shift of the Raman spectrum of azurite (250, 285, 339, 404 and 544 cm-1). These Raman lines are assigned to the lattice modes. The O-H out-of-plane bending mode of azurite was reported at 939 cm-1. We have not found any information available for Raman line of 1579 cm-1. It is probably due to the O-H bending mode, in agreement with Nakamoto (1997).
| Buzgar et al., 20091 | Frost et al., 2002 | Mattei et al., 2008 | Assignment |
| 250, 285, 339, 404, 544 |
112, 131, 139, 144, 154, 165, 171, 179, 194, 215, 237, 248, 265, 281, 332, 387, 400, 414, 540 |
157, 174, 182, 240, 250, 267, 282, 332, 387, 402, 542 |
T(Cu,CO3) |
| 766 | 739, 764 | 744, 768 | ν4 symmetric CO3 deformation |
| 835 | 815, 835 | 840 | ν2 asymmetric CO3 deformation |
| 939 | 952 | 937 | O-H out-of-plane |
| 1097 | 1095 | 1099 | ν1 symmetric CO3 stretching |
| 1425 1459 |
1421 1431 |
1422, 1433, 1462 |
ν3 asymmetric CO3 stretching |
| 1579 | O-H bending mode | ||
| NO | 3424, 3446 | 3431 | 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]