FT-RAMAN AND INFRARED SPECTROSCOPIC STUDY OF ARAGONITE-STRONTIANITE (CAXSR1-XCO3) SOLID-SOLUTION

Citation
Jm. Alia et al., FT-RAMAN AND INFRARED SPECTROSCOPIC STUDY OF ARAGONITE-STRONTIANITE (CAXSR1-XCO3) SOLID-SOLUTION, SPECT ACT A, 53(13), 1997, pp. 2347-2362
Citations number
39
Journal title
SPECTROCHIMICA ACTA PART A-MOLECULAR AND BIOMOLECULAR SPECTROSCOPY
ISSN journal
13861425 → ACNP
Volume
53
Issue
13
Year of publication
1997
Pages
2347 - 2362
Database
ISI
SICI code
1386-1425(1997)53:13<2347:FAISSO>2.0.ZU;2-R
Abstract
Synthetic aragonite-strontianite solid-solution samples have been stud ied using dispersive IR and FT-Raman spectroscopy. In addition to the end-members, nine samples over a range of composition from Ca0.9Sr0.1C O3 to Ca0.1Sr0.9CO3 were analysed. Carbonate anion internal modes are examined in detail by means of band-shape analysis and component fitti ng procedures. Positional disorder induced by the random cationic subs titution results in strong increase of the halfwidth in several vibrat ional bands. Results obtained for the doubly degenerate modes (antisym metric stretching and bending, nu(3) and nu(4)) reveal the presence of three components both in the TR antisymmetric stretching band as well as in the Raman antisymmetric bending band. These observations are in terpreted in terms of an overtone 2 nu(4) in possible Fermi resonance with the corresponding nu(3) fundamental in the IR spectra, and the pr esence of Davidov (factor group) splitting in the FT-Raman nu(4) band. Lattice modes in the FT-Raman spectra demonstrate weaker cohesion bet ween the cation/carbonate/cation layers in aragonite (synth) than in s trontianite (synth). (C) 1997 Elsevier Science B.V.