Reassessment of the Raman CO2 densimeter
Author
Abstract
Raman spectroscopy has proven to be an effective tool to confirm the presence and abundance of CO2 in fluid and
melt inclusions. The Ramanmethod for quantifying CO2 abundance is based on the observation that the distance
between the two Raman bands comprising the Fermi diad varies systematicallywith CO2 density. In recent years,
several Raman densimeters have been developed by different research groups to determine the density of CO2 in
fluid and melt inclusions. The different densimeters that have been proposed predict different densities for the
same Fermi diad splitting, leading to large differences in estimated CO2 contents for inclusions, depending on
which densimeter is used to interpret the Raman data. In this study, we examine potential causes for variations
in the various densimeters and show that these differences aremainly the result of using different Raman instruments
and settings, different collection parameters, and different analytical methods.
Twelve experimentswere conducted to test the variability associated with changing instrumental and analytical
conditions, as well as to understand the differences between the various densimeters, using three different
Raman instruments, with different laser sources and dispersion gratings. In all of the experiments, the splitting
of the Fermi diad of CO2 and CO2 density at pressures from the liquid-vapor curve (6.0 MPa to 0.06 MPa) at ambient
temperature (~22 °C) was calibrated using a high-pressure optical cell. The results show a consistent behavior
whereby all analytical configurations show parallel trends in terms of the variation in Fermi diad
splitting as a function of CO2 density. The slopes of the lines representing the variation in Fermi diad splitting
as a function of CO2 density, as well as low density (pressure) data from other densimeters (Kawakami et al.,
2003; Yamamoto and Kagi, 2006; Song et al., 2009; Fall et al., 2011; Wang et al., 2011) are remarkably similar,
with a variation of about ~10% and a standard deviation of 3%. The differences observed in all densimeters, including
previously published densimeters and the 12 experiments from this study, are most likely a function of variations
in instrumentation, laser excitation wavelength, gratings, and analytical protocols used during the
experimental calibration of the splitting of the Fermi diad. Based on results of this study, we recommend against
using any published densimeter to interpret Raman data collected using an instrument other than that on which
the calibration is based, and suggest that researchers develop a calibration that is applicable and specific to their
instrument and data collection protocol.
Indexation
Artículo de publicación SCOPUS
Identifier
URI: https://repositorio.uchile.cl/handle/2250/168794
DOI: 10.1016/j.chemgeo.2016.12.034
ISSN: 00092541
Quote Item
Chemical Geology 450 (2017) 210–222
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