Abstract

AbstractAzurite [Cu2+3(CO3)2(OH)2] and malachite [Cu2+2(CO3)(OH)2] are both monoclinic hydroxy carbonates of copper. The Raman spectra of these two minerals were collected at both 298 and 77 K together with the single crystal Raman spectra of azurite at 298 K. The spectra of both azurite and malachite contain modes of three separate vibrational groups: OH, CO3 and Cu O. Accordingly, for azurite the bands at 3453 and 3427 cm−1 have been assigned as the O H stretching mode with the O H bending modes found at 1035 and 952 cm−1. Malachite displays two hydroxyl stretching bands at 3474 and 3404 cm−1 at 298 K which shift to 3470 and 3400 cm−1 at 77 K while O H out‐of‐plane bending modes are found at 1045 and 875 cm−1. For the carbonate group, bands are observed at 1090 cm−1 (ν1), 837 and 817 cm−1 (ν2), 1490 and 1415 cm−1 (ν3) and 769 and 747 cm−1 (ν4). The effect of collecting the spectra at 77 K results in considerable band narrowing. The Raman spectra of the single crystals of azurite show the orientation dependence of the vibrational modes. A mechanism for ν2 splitting is proposed whereby vertical carbonate ions couple to form an in‐phase and out‐of‐phase bending modes. Combination of these vibrational modes such as ν1 + ν3, ν1 + ν3, ν1 + ν4 and 2ν2 are found at 2530, 2414, 1860, and 1670 cm−1, respectively. IR bands for the Cu O stretching modes are observed at 495 and 400 cm−1, while Cu O bending modes occur at 455 and 345 cm−1. Bands at 305 and 240 cm−1 are assigned to the O Cu OH bending modes. The Raman out‐of‐plane bending modes are found at 194 and 170 cm−1. For the carbonate group, infrared bands are observed at 1095 cm−1 (ν1), 834 and 816 cm−1(ν2), 1430 and 1419 cm−1 (ν3) and 764 and 739 cm−1 (ν4). Combination of the CO3 vibrational modes ν1 + ν4 is observed at 1860 cm−1. IR bands for Cu O stretching modes are observed at 580, 570 and 505 cm−1. Copyright © 2002 John Wiley & Sons, Ltd.

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