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Raman and infrared spectra of carbonates of calcite structure
Author(s) -
Gunasekaran S.,
Anbalagan G.,
Pandi S.
Publication year - 2006
Publication title -
journal of raman spectroscopy
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.748
H-Index - 110
eISSN - 1097-4555
pISSN - 0377-0486
DOI - 10.1002/jrs.1518
Subject(s) - dolomite , calcite , raman spectroscopy , mineralogy , carbonate , carbonate minerals , mineral , geology , infrared , infrared spectroscopy , analytical chemistry (journal) , chemistry , environmental chemistry , physics , organic chemistry , optics
The Raman and mid‐range infrared spectra have been measured on natural limestone and dolomite minerals. The carbonate minerals show four prominent absorption bands in the regions 1450–1420, 890–870, 720–700 and 1000–1100 cm −1 . The positions of the wavenumbers are unique for each carbonate mineral and are thus diagnostic of their mineralogy. Calcite and dolomite groups are characterized by the Raman wavenumbers at 288 and 309 cm −1 and the infrared absorption bands at 712 and 728 cm −1 , respectively. The principal wavenumber at 1092 cm −1 in the limestone spectra is accompanied by two satellites with values of 1062 and 1075 cm −1 . The observed non‐split peaks ν 2 and ν 4 in the infrared spectra of limestone indicate the presence of calcite structure in all these samples. The principal reflections occurring at the d ‐spacings, 3.03482, 1.91658 and 1.87962 Å, confirm the presence of calcite structure in limestone minerals. The principal reflections occurring at the d ‐spacings, 3.037, 1.79179 and 2.19750 Å, confirm the existence of dolomite structure in the dolomite minerals. The calculated lattice parameters for the limestone minerals are: a = 4.9781 Å, c = 17.1188 Å and V = 367.392(Å) 3 and the corresponding values for the dolomite minerals are: a = 4.8247 Å, c = 15.9868 Å and V = 322.28 (Å) 3 . Copyright © 2006 John Wiley & Sons, Ltd.