Article ID Journal Published Year Pages File Type
5783068 Chemical Geology 2017 56 Pages PDF
Abstract
Twelve experiments were 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.
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Geochemistry and Petrology
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