Publication
Names
  • T. N. Brusentsova
  • R. E. Peale
  • D. Maukonen
  • G. E. Harlow
  • J. S. Boesenberg
  • D. Ebel
Title
Far infrared spectroscopy of carbonate minerals
Abstract
This study presents far infrared spectra in the range 650–70 cm–1 of 18 common and rare carbonate minerals. Mineral samples of known provenance are selected and physically characterized to determine the purity of the crystalline phase and their composition. The fine ground mineral powders are embedded in polyethylene pellets, and their transmittance spectra are collected with a Fourier spectrometer. The far infrared spectra of different carbonate minerals from the same structural group have well-defined similarities. Observed shifts generally manifest the mass effect of the constituent metal cations. Remarkable spectral differences occur for different carbonates in the far IR region and may serve as fingerprints for mineral identification and are more useful identifiers of carbonate species than those in any other infrared range. For some of the minerals studied here, like kutnohorite, artinite, gaylussite, and trona, no far infrared spectra to that extend (up to 70 cm–1) have been found in literature.
Keywords
Qualitative analysis, Infrared spectroscopy, IR spectra, transmittance spectra, absorption, far-IR, data analysis, band position, band vibration mode, powder, pellets, mineral, carbonate, calcite, magnesite, rhodochrosite, siderite, smithsonite, aragonite, strontianite, witherite, cerussite, huntite, dolomite, ankerite, kutnohorite, hydrozincite, hydromagnesite, artinite, gaylussite, trona, Ca, Mg, Fe, Mn, Zn, Sr, Ba, Pb, Na, CO3, Earth
Content
spectral data, band list data, sample
Year
2010
Journal
American Mineralogist
Volume
95
Number
10
Pages
1515 - 1522
Pages number
8
Document type
article
Publication state
published