Reassessment of the Raman CO2 densimeter

被引:74
|
作者
Lamadrid, H. M. [1 ,2 ]
Moore, L. R. [1 ]
Moncada, D. [3 ,4 ]
Rimstidt, J. D. [1 ]
Burruss, R. C. [5 ]
Bodnar, R. J. [1 ]
机构
[1] Virginia Tech, Dept Geosci, Blacksburg, VA 24061 USA
[2] Univ Toronto, Dept Earth Sci, Toronto, ON M5S 3B1, Canada
[3] Univ Chile, Dept Geol, Plaza Ercilla 803, Santiago, Chile
[4] Univ Chile, Andean Geothermal Ctr Excellence CEGA, Plaza Ercilla 803, Santiago, Chile
[5] US Geol Survey, Natl Ctr, Reston, VA 20192 USA
基金
美国国家科学基金会;
关键词
H2O-CO2 FLUID INCLUSIONS; CARBON-DIOXIDE; ULTRAMAFIC ROCKS; MELT INCLUSIONS; VAPOR BUBBLES; HIGH-PRESSURE; TEMPERATURE; EQUATION; DENSITY; BEHAVIOR;
D O I
10.1016/j.chemgeo.2016.12.034
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Raman spectroscopy has proven to be an effective tool to confirm the presence and abundance of CO2 in fluid and melt inclusions. The Raman method for quantifying CO2 abundance is based on the observation that the distance between the two Raman bands comprising the Fermi diad varies systematically with 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 are mainly the result of using different Raman instruments and settings, different collection parameters, and different analytical methods. 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 degrees 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 similar to 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.(C) 2016 Elsevier B.V. All rights reserved.
引用
收藏
页码:210 / 222
页数:13
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